TS3.5 | Advances in earthquake geology and seismic hazard assessment
Advances in earthquake geology and seismic hazard assessment
Co-organized by NH4
Convener: Francesco Iezzi | Co-conveners: Jenni Robertson, Alessandro Valentini, Francesco Visini, Oona Scotti
Orals
| Mon, 15 Apr, 14:00–15:45 (CEST)
 
Room K1
Posters on site
| Attendance Tue, 16 Apr, 10:45–12:30 (CEST) | Display Tue, 16 Apr, 08:30–12:30
 
Hall X2
Orals |
Mon, 14:00
Tue, 10:45
Geological investigations on faults and the earthquakes they produce continue to advance our understanding of earthquake geology and of the associated seismic hazard.

The application of modern approaches has been shown to provide unprecedented and comprehensive pictures of the mechanics and dynamics of active faults over multiple temporal and spatial scales. Studying recent earthquakes can yield valuable information to characterize the earthquake source parameters and the coseismic behaviour of faults. Paleoseismological investigations extend the seismic record of active faults, providing information on past earthquakes and their recurrence intervals. Studies of the structural geology and tectonic geomorphology of active faults can help us defining their long-term behaviour. Geodesy may be used to complement studies that focus on decadal to multi-millennial timescales. Moreover, multidisciplinary approaches have demonstrated the interaction of faults within fault systems.

Incorporating the knowledge gained from active faults into suitable fault models for probabilistic seismic hazard assessments (PSHA) presents challenges, both in terms of ground motion and fault displacement hazard analysis (FDHA). Hence, this session aims to provide an open forum for recent studies concerning active faults, crustal deformation, PSHA, and FDHA.

In this Fault2SHA session, we welcome contributions describing and discussing different approaches to study active faults and to perform SHA. We are particularly interested in studies applying innovative and multidisciplinary approaches from observations on single earthquakes to geologic timescales. These methods may include, but are not limited to, structural analyses, paleoseismological trenching, high-resolution coring, geologic and morphotectonic studies, Quaternary dating, geophysical imaging, geodetic studies, and stress modelling. We encourage contributors to present studies that consider how fault data can be incorporated into models for seismic hazard assessment.

Orals: Mon, 15 Apr | Room K1

Chairpersons: Francesco Iezzi, Jenni Robertson, Alessandro Valentini
14:00–14:05
14:05–14:25
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EGU24-11726
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solicited
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On-site presentation
Luca Dal Zilio and the FEAR team

Understanding earthquake initiation, propagation, and arrest is critical for mitigating seismic risks, yet these processes remain among the most complex natural phenomena to decipher. The ERC-Synergy project FEAR (Fault Activation and Earthquake Ruptures), conducted within the Bedretto Underground Laboratory for Geosciences and Geoenergy (BedrettoLab), offers a pioneering approach to investigate these intricate mechanics. Here, we highlight the unique challenges and opportunities presented by the FEAR project, with a particular focus on computational earthquake physics and its potential to enhance our understanding of fluid-induced seismic events on broadband seismic arrays. Located ~1.5 kilometers beneath the Swiss Alps, BedrettoLab provides an unparalleled setting for a detailed study of earthquake mechanics. The FEAR project utilizes this exceptional environment to induce and monitor small-scale seismic events. By employing hydraulic stimulation on selected faults near the BedrettoLab tunnel, the project aims to initiate and observe earthquakes of approximately magnitude ~1.0. These refined methods provide a controlled setting to study the intricate details of earthquake processes closely, offering a chance to push the boundaries of current understanding of earthquake physics.

Central to the FEAR project is the development and testing of hydro-mechanical computational methods capable of replicating various injection protocols. These methods systematically test a range of constitutive laws that govern the evolution of fault friction, integrating insights from laboratory experiments with fully inertial elastodynamic modeling of earthquake processes. This approach allows us to investigate the poroelastic response of the rock mass, examining how seismic and aseismic slip interact in space and time, and assessing the dynamic evolution of pore-fluid pressure due to processes such as shear-induced dilatancy and compaction. Furthermore, we employ 3D dynamic rupture simulations to explore conditions controlling either self-arresting or run-away rupture. These simulations provide critical insights into wave spectrum and attenuation near BedrettoLab, enabling us to predict the peak ground velocity (PGV) of anticipated magnitude ~1 earthquakes. This innovative modeling approach represents a significant opportunity to advance our understanding of fault mechanics and the influence of fluid interactions.

In conclusion, the FEAR project within BedrettoLab provides a unique and controlled environment to study the mechanics of earthquakes. The challenges posed by this research are matched by the significant opportunities it offers for advancing our understanding of seismic phenomena. By focusing on innovative modeling techniques and integrating multidisciplinary data, this project aims to shed light on the complex dynamics of fault activation and rupture, ultimately contributing to more accurate seismic hazard assessments and safer geoenergy practices.

How to cite: Dal Zilio, L. and the FEAR team: Modeling Earthquake Dynamics and Fault Poromechanics in the BedrettoLab FEAR Project: Opportunities & Challenges, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-11726, https://doi.org/10.5194/egusphere-egu24-11726, 2024.

14:25–14:35
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EGU24-14251
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On-site presentation
Ioannis Koukouvelas, Athanassios Ganas, Vasiliki Zygouri, and Christina Tsimi

Geomorphologic analysis and data from paleoseismological sites across segmented active faults help the evaluation of past and future seismic faulting. The study of paleo-earthquakes on the Pidima-Anthia Fault provides an opportunity to unravel the seismic behaviour of the Eastern Messinia Fault Zone (EMFZ) that defines the western border of the N-S trending Taygetos Mtn range in Peloponnese (southern Greece). This fault zone is segmented and includes a complex system of primarily normal fault- segments dipping westwards, with a traceable length from 6-10 km. We applied geomorphological and palaeoseismological analysis across the Pidima-Anthia Fault segment. The palaeoseismological trench data provide evidence for five M >6.4 earthquakes and indicate an apparent slip rate of 0.23 mm/a. Geomorphologically, the modelling of a footwall series of triangular facets, attest to a slip-rate estimation in the order of 0.28-0.44 mm/a. These data highlight that the slip rate of the fault is remarkably stable for the Quaternary period but particularly over the last 17 ka period, as well as that this duration is enough for a morphogenic active fault to create seismic landscapes. The Holocene earthquake history of the Pidima-Anthia Fault allows its comparison with six other known active normal faults of southern Greece. The overall data indicate a pattern of earthquake clustering in the southern Greece faults ("Wallace-type" behaviour). In particular, the Pidima-Anthia Fault's seismic history resembles with time predictable earthquakes and clustering during the Holocene. However, the Pidima-Anthia Fault during the current period (i.e., post 1 Ka AD) does not display cluster time-predictable behaviour, and a strong earthquake can happen at any time.

How to cite: Koukouvelas, I., Ganas, A., Zygouri, V., and Tsimi, C.: Palaeoseismology and tectonic geomorphology for detecting the seismic behaviour of the Pidima-Anthia Fault, south Greece, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-14251, https://doi.org/10.5194/egusphere-egu24-14251, 2024.

14:35–14:45
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EGU24-9870
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On-site presentation
Gerald P. Roberts, Claudia Sgambato, Ioannis Papanikolaou, Zoe Mildon, Joakim Beck, Alessandro Michetti, Joanna Faure Walker, Sam Mitchell, Marco Meschis, Richard Shanks, Richard Phillips, Ken McCaffrey, Eutizio Vittori, Francesco Iezzi, Jennifer Robertson, Francesco Visini, and Maz Iqbal

We present an in situ 36Cl dataset recording the exhumation of 27 active normal fault planes by earthquake slip for the central Apennines, Italy. We do this to constrain the characteristics of earthquake clustering and anticlustering across the entire extending orogen, and in an attempt to constrain the reasons why clustering and anticlustering occurs. We show that duration and magnitude of clustering and anticlustering, and their characteristics, can be explained by a model where the transfer of differential stress between faults and their underlying shear-zones, and between neighbouring fault/shear-zone structures, produces changes in strain-rates on underlying viscous shear zones which drive periods of rapid or reduced slip-rate on their overlying faults. We suggest that stress increase on an underlying shear zone produced by coseismic slip on its overlying fault could be the mechanism that initiates an earthquake cluster. We suggest that stress reductions on shear-zones from coseismic slip located across strike could be the mechanism that initiates an earthquake anticluster. The durations of anticlusters are controlled by the summed stress decreases through time on shear zones, because although these shear zones are slipping relatively slowly, eventually they will load their overlying fault to failure initiating a new cluster, with anticlusters induced across strike. Thus, there is dynamic feedback both up and down dip between faults and their underlying shear zones and crucially across strike between neighbouring fault/shear-zone structures. If the dynamics producing clustering and anticlustering can be constrained, it may be that observations of these phenomena should be included in probabilistic seismic hazard assessments (PSHA) and also interpretations of regional deformation rates and crustal rheologies based on geodetic data. Multi-millennial clustering and anticlustering should become a subject for discussion in these scientific communities.

How to cite: Roberts, G. P., Sgambato, C., Papanikolaou, I., Mildon, Z., Beck, J., Michetti, A., Faure Walker, J., Mitchell, S., Meschis, M., Shanks, R., Phillips, R., McCaffrey, K., Vittori, E., Iezzi, F., Robertson, J., Visini, F., and Iqbal, M.: Characteristics of slip-rate variability and temporal earthquake clustering across a distributed network of active normal faults from in situ 36Cl cosmogenic dating of fault scarp exhumation., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9870, https://doi.org/10.5194/egusphere-egu24-9870, 2024.

14:45–14:55
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EGU24-10100
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ECS
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On-site presentation
Claudia Sgambato, Joanna P. Faure Walker, Gerald P. Roberts, Zoë K. Mildon, and Marco Meschis

We investigate the Coulomb stress changes due to 30 strong earthquakes occurring on normal faults since 1509 A.D. in Calabria, Italy, including the influence of both coseismic and interseismic loading in our modelling. We compare the results to existing studies of stress interaction from the Central and Southern Apennines, Italy. The three normal fault systems have different geometries and long-term slip-rates. The Central Apennines hosts a complex fault system, with many faults across strike, so that when an earthquake occurs, many of the surrounding faults experience a stress decrease. The Southern Apennines and Calabria have a simpler geometry, with fewer faults, and faults are located predominantly along strike, therefore when an earthquake occurs the dominant process on the neighbouring faults is stress increase. We investigate how stress transfer may influence the occurrence of future earthquakes and what factors may govern the variability in earthquake recurrence in different fault systems. Within the analysed time period, the Calabrian, Central Apennines, and Southern Apennines fault systems have 91%, 73% and 70% of faults with a mean positive cumulative Coulomb stress change, respectively; this is due to fewer faults across strike, more across strike stress reductions, and greater along-strike spacing in the three regions respectively. In regions with close along strike spacing or few faults across strike, such as Calabria and Southern Apennines, the stress loading history is mostly dominated by interseismic loading and most faults are positively stressed before an earthquake occur on them (96% of all faults that ruptured in Calabria; 94% of faults in the Southern Apennines), and some of the strongest earthquakes occur on faults with the highest mean cumulative stress of all faults prior to the earthquake. In the Central Apennines, where across strike interactions are the predominant process, 79% of the earthquakes occur on faults that are positively stressed. The results highlight that fault system geometry plays a central role in characterizing the stress evolution associated with earthquake recurrence, and can possibly influence the occurrence of propagating triggered earthquake sequences.

How to cite: Sgambato, C., Faure Walker, J. P., Roberts, G. P., Mildon, Z. K., and Meschis, M.: Influence of fault system geometry and slip rates on earthquake triggering and recurrence variability, insights from Coulomb stress interactions during historical earthquake sequences in Italy, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-10100, https://doi.org/10.5194/egusphere-egu24-10100, 2024.

14:55–15:05
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EGU24-18876
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ECS
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On-site presentation
Octavi Gómez-Novell, Francesco Visini, Bruno Pace, José Antonio Álvarez-Gómez, and Paula Herrero-Barbero

The use of physics-based earthquake simulators is increasingly common in earthquake forecasting for seismic hazard. Their popularity is related to their ability to overcome completeness limitations of real seismicity catalogues, while reproducing complex earthquake rupture behavior and interaction patterns through the modelling of the physical processes involved in earthquake nucleation and rupture propagation. One common challenge when designing earthquake simulations is the selection of the input parameters that will produce the most feasible models in terms resemblance to natural earthquake processes and relationships, e.g., the rate-and-state frictional parameters – a, b – and the initial normal stress. The frequent lack of empirical data on such parameters, often bases their selection on non-systematic testing and qualitative model performance analysis, thus potentially reducing the objectivity of the modelling. We present a new quantitative approach to evaluate and rank the performance of multiple earthquake simulation models based on a workflow that scores each synthetic catalog according to their combined fit to objective seismological benchmarks. These benchmarks rely on widely used empirical earthquake data: 1) scaling relationships, 2) shape of the magnitude-frequency distribution and 3) rates of surface ruptures from paleoseismology. The approach permits an objective and effective approximation to model performance evaluation, allowing to easily identify which models (and input parameter combinations) simulate better natural earthquake relations and behavior. The algorithm-based approach also facilitates the exhaustive analysis of many input parameter combinations and allows the identification of systematic correlations between parameters and model performance. We validate the approach with earthquake simulations on a theoretical planar fault and with published simulations at the Eastern Betics Shear Zone (EBSZ) in southeastern Spain. In both cases, the method successfully ranks the models with better resemblance to natural catalogues, while avoiding self-correlation of the benchmark scores, i.e., the best model is not the best in all benchmarks but the better balanced across them. In the case of the EBSZ, our ranking analysis replicates the qualitative and manual analyses previously published, which reinforces the usefulness of the approach. We also identify very clear correlations between the model performance and the rate-and-state a and b parameters. In particular, we observe that larger differences between a and b tend to better model performance. Conversely, the initial normal stress does not correlate with the performance. Overall, we estimate that the approach can ease researchers on earthquake simulation design and building, and on better understanding the impact of selected input parameters into the physics-based models. Moreover, the model ranking results can be employed to drive further analysis such as weighting of earthquake forecast models in seismic hazard logic trees.

How to cite: Gómez-Novell, O., Visini, F., Pace, B., Álvarez-Gómez, J. A., and Herrero-Barbero, P.: A simple yet effective method to rank the performance of physics-based earthquake simulations, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18876, https://doi.org/10.5194/egusphere-egu24-18876, 2024.

15:05–15:15
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EGU24-10122
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ECS
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On-site presentation
Billy Andrews, Zoë Mildon, Manuel Lukas Diercks, Sam Mitchell, Gerald Roberts, Constanza Rodriguez Piceda, and Jenni Robertson

To undertake fault-based seismic hazard assessment, we need to accurately identify source faults and assess their slip-rate and kinematics through pertinent data collection. For example, converging slip vectors may be used to deduce whether isolated fault strands are connected at depth. Kinematic (slip vector) data can be collected through offset piercing points or from striations preserved on fault scarps. However, striations are surficial features and may therefore be readily eroded and not preserved or visible on degraded scarps. Tensional fracture networks are ubiquitous on bedrock fault scarps and extend deeper into the scarp, and therefore have a greater preservation potential when compared to striations. In this work we characterise fracture-scarp (F-S) lineation patterns across eight faults in Italy (Central Apennines) and Greece (Perachora Peninsula) to explore how these patterns relate to fault plane geometry and slip-vector.

Various fracture-scarp (F-S) lineation patterns (including sinistral/dextral en-echelon arrays, slip-parallel/-perpendicular fractures, and conjugate sets) are recognised. These patterns show evidence of progressive growth during exhumation. This suggests F-S lineations formed near the surface as the footwall uplifts, with larger features becoming more connected and smaller ones remaining ‘isolated’. The orientations of F-S lineations align within a pure or Riedel shear geometry where the shear sense is related to the rake of the slip vector. We propose that the observed patterns are controlled by fault plane orientation relative to a 3D strain ellipsoid and the progressive reduction of effective normal stress during footwall exhumation. As fractures form under the same stress regime as striations, they can serve as a kinematic indicator even on highly degraded active fault scarps.

How to cite: Andrews, B., Mildon, Z., Lukas Diercks, M., Mitchell, S., Roberts, G., Rodriguez Piceda, C., and Robertson, J.: Using fracture-scarp lineations as kinematic indicators on active normal fault scarps, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-10122, https://doi.org/10.5194/egusphere-egu24-10122, 2024.

15:15–15:25
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EGU24-12101
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ECS
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On-site presentation
Swakangkha Ghosh, George Philip, and Suresh Narayanapanicker

Himalayan seismicity exhibits a bimodal mechanism with great earthquakes (+M8) rupturing the upper locked segment of the Main Himalayan Thrust (MHT) and blind earthquakes (up to Mw ~ 7.8) rupturing the down-dip section of the decollement. However, few imbricate and out-of-sequence active structures have been overlooked with limited research in the hinterland regions with respect to active fault mapping and paleoseismological trench excavations. The present study focusses on the western section of the Trans-Yamuna Active Fault (TYAF) in northwestern Sub-Himalaya, hosting the Sirmurital Active Fault (SAF). The SAF exhibits a distinctive south-side up trace, obliquely cross-cutting the Main Boundary Thrust (MBT).

Satellite data, coupled with detailed field investigation confirms that the above fault dips 60˚ to the north, with a fault scarp of 40 m height. Minor strike-slip component is also confirmed with the presence of a subtle pressure ridge, and preliminary fluvial terrace mapping. Generation of a high-resolution Digital Elevation Model (DEM) from Cartosat-1 stereo pairs, and quantification with total station mapping of fault scarp further confirmed the terrace displacement. Subsequently, trench excavation (31 m in length) across the SAF at Sirmurital village provided compelling evidence of atleast two paleoearthquakes displacing and deforming Quaternary sediments along two identified fault strands. Soft-sediment deformation features complemented with injection features suggests its genetic link with paleoearthquakes. Radiocarbon dating analysis offers insights into the probable timing of the faulting events. Overall, the tectonic placement of the SAF provides a unique opportunity to document the occurrence of a normal fault in the hanging wall of a megathrust system and its potential to generate earthquakes in the highly populous mountainous belt of NW Sub-Himalaya. Therefore, the SAF along with the other associated faults, in the hinterland calls for detailed evaluation for a more comprehensive seismic hazard assessment.

 

Keywords: Out of sequence; Sirmurital Active Fault; Cartosat-1; Paleoearthquakes; Soft-sediment deformation; Seismic hazard 

 

How to cite: Ghosh, S., Philip, G., and Narayanapanicker, S.: Evidence of surface rupture associated with paleoearthquakes in the Trans Yamuna Segment of Northwestern Sub-Himalaya, India - Focus on the Sirmurital Active Fault , EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-12101, https://doi.org/10.5194/egusphere-egu24-12101, 2024.

15:25–15:35
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EGU24-16516
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ECS
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On-site presentation
Sarah Visage, Léa Pousse, Sophie Giffard-Roisin, Margaux Mouchené, Laurence Audin, and Sarah Perrinel

The understanding of seismic recurrence relies on the chronology and magnitude of earthquake ruptures that have occurred in the past along a given fault. Knowledge of the rupture history of a fault provides valuable insights into its potential future behavior, aiding in the assessment of seismic hazard. Geomorphic evidence of faults is thus crucial for constraining models of seismic recurrence through surface rupture. The advent of remote sensing and other high-resolution datasets (such as Pleiades and SPOT satellite images) has improved tectono-geomorphological studies, promising to improve earthquake recurrence models. While manual or semi-automatic measurements of fault offsets using topographic markers like rivers have been conducted (Manighetti et al., 2015, 2020; Zielke et al., 2012), recent advances in artificial intelligence (AI) open new avenues for geoscientific applications (Ren et al., 2020) to handle the amount of high-resolution datasets.

This study takes on the challenge of measuring slip offsets of faults using a Convolutional Neural Network (CNN) applied to synthetic Digital Elevation Models (DEM). The methodology involves generating realistic synthetic landscape models (DEM) using the Landlab software (Hobley et al., 2017), simulating slip faults based on the method of Reitman et al. (2019). The approach includes creating synthetic DEMs with Landlab, incorporating fault effects such as erosion, slip rates, and variable fault zone widths. Preliminary work in this study involves automating the creation of synthetic DEMs for a 2D prototype with a variable slip fault. A regression CNN model (with three convolutional layers followed by max-pooling layers and fully connected layers) is trained on these synthetic datasets, achieving slip offsets of ±3 meters on validation data. The model is then tested on real data labeled by experts, yielding satisfactory preliminary results.

This study demonstrates the potential of CNNs for measuring slip offsets of faults using synthetic DEMs. The successful application of AI to geosciences paves the way for more efficient and automated analysis of fault activity in landscapes, thereby contributing to an enhanced assessment of seismic risks.

How to cite: Visage, S., Pousse, L., Giffard-Roisin, S., Mouchené, M., Audin, L., and Perrinel, S.: Characterisation of strike-slip fault offsets using convolutional neural networks, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16516, https://doi.org/10.5194/egusphere-egu24-16516, 2024.

15:35–15:45
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EGU24-2671
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ECS
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Virtual presentation
Falak Zahoor, Villayat Ali, Bashir Ahmad, and Inaam ul Haq Jeelani

A high-angle reverse fault was identified near the Aharbal Falls in the Shopian District of the southern Kashmir Basin and was subsequently named as Lamni Fault by Zahoor et al. (2023). The rise of the Pir Panjal range due to the higher tectonic activity in the southern part of Kashmir (Dar et al., 2014) has led to the overthrusting of the Early Permian Panjal Traps over the Pleistocene Fluvio-Glacial Deposits. The presence of the fault was experimentally validated through the conduction of single-station microtremor horizontal-to-vertical spectral ratio (MHVSR) method, supported by the results from multichannel simulation with one-receiver (MSOR) surface wave tests across the suspected fault zone in Shopian. The fault zone was demarcated at the location by identifying anomalously high H/V amplitudes (>8) at high frequencies (>4Hz) as opposed to the low values (2-3) in the surrounding host rock. As an extension of the work, we seek to conduct the microzonation of the region laced by the Lamni Fault in the Sedow area of Shopian, Kashmir, using the atypical HVSR amplitudes as the markers of high risk. The MHVSR method has been successfully employed for investigating buried and exposed faults like Erft-Sprung normal fault, Tremestieri normal fault, southern Crete of Greece, Longmen Shan fault zone, etc. (Hinzen, 2004; Lombardo and Rigano 2006; Moisidi et al., 2012; Zhang et al., 2019). The low-velocity fractured fault zone is known trap seismic waves and hence lead to large amplifications of the waves which is thus reflected in the HVSR curves as well as in earthquake recordings e.g., in San Andreas fault zone (Li et al., 2000) and San Jacinto fault zone (Roux et al., 2016). Utilising this behaviour of the fractured fault zones, microzonation of the Sedow locality which lies in the vicinity of the detected Lamni Fault was conducted by performing about 50-60 single-station MHVSR tests over an area of about 2 km x 2 km. The area has several residential buildings along with local government school buildings as well as a mosque, thus demanding serious consideration of the increased seismic hazard due to the presence of the fault. Zones of anomalous H/V amplitudes were found in the region surrounded by stable low estimates. This may have serious implications for the seismic hazard estimates in the region surrounding the fault zone also supported in earlier studies in other regions of the world (e.g., Spudich and Olsen, 2001; Donati et al., 2001; Rovelli et al., 2002). It is recommended that a zone be defined at a significant width around the fault zone in which constructions may be avoided or else special considerations for the increased seismic hazard be considered for the existing buildings. Such a buffer zone has been named the Alquist-Priolo zone, APZ in earlier studies (Spudich and Olsen, 2001; Bryant, 2010). The APZ is considered an important inclusion in seismic hazard and microzonation process to aid in urban planning and development in a region.

How to cite: Zahoor, F., Ali, V., Ahmad, B., and Jeelani, I. U. H.: Seismic risk microzonation mapping using microtremor recordings for an urban area in the vicinity of Lamni Fault, southern Kashmir Basin , EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2671, https://doi.org/10.5194/egusphere-egu24-2671, 2024.

Posters on site: Tue, 16 Apr, 10:45–12:30 | Hall X2

Display time: Tue, 16 Apr, 08:30–Tue, 16 Apr, 12:30
Chairpersons: Francesco Iezzi, Jenni Robertson, Alessandro Valentini
X2.55
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EGU24-18523
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ECS
Adriana Fatima Ornelas-Agrela, Carlos Gamboa-Canté, María Belén Benito, Alicia Rivas-Medina, and Ligia Quirós-Hernandez

Incorporating faults as independent seismic sources in Probabilistic Seismic Hazard Assessment (PSHA) significantly influences the ground motion values when compared to classical zoning methods (CZM). This practice holds particular relevance for populations situated top or near active faults. Some hybrid methods (HM) and fault-based methods, implemented in Spain, show that Peak Ground Acceleration (PGA) values increase in the vicinity of the fault traces. In some cases the hazard levels may double, consistent with the PGA observed in recent earthquakes (Rivas-Medina, A., 2018; Gómez-Novell O., 2020). Despite the existence of methods that combine zones and faults in seismic sources characterization, there is a lack of allocation of seismic potential between these two types of sources. Additionally, there is an increasing use of geological data since seismic catalogs alone are insufficient to fully characterize the seismic potential of faults. This limitation becomes particularly evident in slow deformation zones, such as southeastern Spain, where the recurrence period of faults exceeds the temporal coverage of the seismic catalog.

The present investigation addresses two key aspects: how to quantify the geological information of the faults and transfer it to recurrence models, and how to distribute the seismic potential of the region between faults and zone. This research contemplates two steps. In the first step, four methods were applied: 1) Moment rate-based method, 2) Slip rate-based method, both proposed by Bungum (2007); 3) the hybrid method developed by Rivas-Medina et al. (2018), which considers both zone-type and fault-type sources; and 4) SHERIFS, a fault system-based assessment proposed by Cartier et al. (2019). In the second step, Faults and Area Moment Sharing (FAMS) (Ornelas-Agrela et al., 2022*) is applied. This new method enables characterizing the faults based on their associated seismicity, improving the distribution of seismic potential between faults and zones. The five methods were applied to multiple seismogenic zones within southeastern Spain, recognized as one of the most seismically active areas in the country. An analysis was conducted, highlighting the sensitivity of the results of PSHA implementation. The preliminary results of the FAMS method application are presented.

* first presented by Ornelas-Agrela, A. et al. at the Iberfault2022 congress in Teruel, Spain.

How to cite: Ornelas-Agrela, A. F., Gamboa-Canté, C., Benito, M. B., Rivas-Medina, A., and Quirós-Hernandez, L.: Review of methods that implement active faults characterization for PSHA in Southern Spain. Preliminary results of the application of the FAMS method., EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18523, https://doi.org/10.5194/egusphere-egu24-18523, 2024.

X2.56
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EGU24-1056
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ECS
Rukhshar Husain and Javed N Malik

The Indian plate is currently underthrusting beneath the Tibetan plateau along the Main Himalayan Thrust (MHT). The strain is getting accumulated during the inter-seismic period on MHT due to this ongoing convergence. The accumulated strain energy is released in a stick-slip fashion on MHT causing destructive earthquakes. Several strong earthquakes within the Himalayan zone have been reported in previous studies such as 1897 at Shillong (Mw 8.2), 1905 at Kangra (Mw 7.8), 1934 at Bihar-Nepal (Mw 8.1), 1950 at Assam (Mw 8.4), 2005 at Muzaffarabad (Mw 7.6), 2015 at Gorkha (Mw 7.8), and 2015 in Afghanistan (Mw 7.6). Based on the distribution of recent and historic earthquake activity in the Himalayas, three seismic gaps can be distinguished from west to east: the Kashmir Seismic Gap (west of the 1905 Kangra earthquake), the Central Seismic Gap (between the 1905 and earthquakes), and the Assam Seismic Gap (between the 1897 and 1950 earthquakes). The major objective of this study is to investigate the hinterland region in the NW Himalaya, which is relatively less explored in terms of its Active Tectonics & Paleoseismology as compared to the deformation front along the Main Himalayan Thrust (MFT). The Nahan salient and Kangra re-entrant are characterised by a complicated pattern of fault distribution which has been proposed in previous studies to get activated, either individually or alongside the Main Frontal thrust, during past large to great-magnitude earthquakes. A detailed tectono-geomorphic map has been prepared using the Cartosat-1 dataset, and geomorphic markers suggestive of recent tectonic activity have been identified in the study region. An exhaustive fieldwork has been conducted, during which a total of 13 samples were collected for Optically Stimulated Luminescence (OSL) dating and Carbon dating to identify signatures of past earthquakes and assess the possibility and degree to which the 1905 earthquake has affected the region. Based on the detailed tectono-geomorphological and paleoseismological investigations, we will be able to assess regional seismic hazards.

(*Author RH aka Rukhshar)

How to cite: Husain, R. and Malik, J. N.: Active Fault and Paleoseismological studies in the hinterland region of NW Himalaya, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-1056, https://doi.org/10.5194/egusphere-egu24-1056, 2024.

X2.57
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EGU24-5155
Marco Meschis, Gerald Roberts, Claudia Sgambato, Alessandro Maria Michetti, Franz Livio, Zoe Mildon, Joanna Faure Walker, Francesco Iezzi, Jennifer Robertson, Alessandro Gattuso, Marino Domenico Barberio, Paolo Randazzo, and Antonio Caracausi

In this study, we present scaling relationships between fault lengths, fault slip-rates and historical seismicity for an active normal fault system, seismically accommodating crustal extension within the upper plate of the Ionian subduction zone (southern Italy). This crustal extension is confirmed by historical seismicity and instrumental geodesy, with GNSS-derived values of horizonal deformation within a range of 2-3 mm/yr throughout Calabria and the Messina Strait region. We collated data for fault slip-rates, fault lengths and historical earthquakes for a given fault to explore whether fault slip-rates are correlated with fault size and their geometric moment.

We present new results showing a robust correlation between fault lengths and fault slip-rates, which supports the idea of a relationship for a given fault between fault slip-rates and the geometric moment.

We discuss our results in terms of how these correlations should be used if regional deformation is accommodated by localised strain on faults mostly arranged along strike rather than distributed strain on multiple faults across-strike. For instance, we compare our empirical correlation between fault lengths and fault throw-rates over the Middle-Late Pleistocene in Calabria and the Messina Strait with those from Central and Southern Apennines over the Holocene, characterized by strain distributed on multiple faults across-strike and strain localised on faults mostly arranged along-strike, respectively.

Tectonic and seismic hazard implications are discussed for future investigations based on fault slip-rates, fault size and historical seismicity.

How to cite: Meschis, M., Roberts, G., Sgambato, C., Michetti, A. M., Livio, F., Mildon, Z., Faure Walker, J., Iezzi, F., Robertson, J., Gattuso, A., Barberio, M. D., Randazzo, P., and Caracausi, A.: Empirical scaling correlations between fault lengths and fault slip-rates in seismically-active extensional regions: The Calabria and Messina Strait region (southern Italy) as case study, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-5155, https://doi.org/10.5194/egusphere-egu24-5155, 2024.

X2.58
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EGU24-7698
Hector Perea, Octavi Gómez-Novell, María José Jiménez, Mariano García, Lucía Lozano, Julián García-Mayordomo, José Luis Sánchez-Roldán, Ariadna Canari Bordoy, and Sara Martínez-Loriente

The Alboran Sea is one of the most seismically regions of Western Europe, accommodating an important part of the current NW-SE convergence between the African and Eurasian plates (4-5 mm/yr). Despite the Alboran Sea is considered as a region of relatively low tectonic deformation and diffuse seismicity, the major faults within have been responsible of large earthquakes (IEMS>IX) since historical times (e.g., 1522 Almería, 1790 Oran, 1804 Alboran, 1910 Adra or 2016 Al-Idrissi earthquakes). One of the main issues for the characterization of the seismic hazard in the Alboran Sea, common to many low-deformation regions, lies in accurately constraining the seismic parameters that define fault activity and their behavior (i.e., slip rates, earthquake recurrence and multi-fault rupture capability, among others). This issue is further aggravated by the fact that these faults are mostly located offshore, making their investigation more challenging. As a result, most faults in the Alboran Sea have poor slip and activity rate estimates, while their capability to interact and rupture in complex rupture patterns has not been explored yet. In this study, we compute several models of earthquake rupture rates for the Alboran Sea with the SHERIFS code and using a systematic parameter exploration tree to determine the parameters of each model. We base the exploration tree on the slip rate and multi-fault rupture scenarios, allowing us to investigate the epistemic uncertainty linked to these parameters. To check the feasibility of the computed earthquake rates of each model, we compare them with the observed seismicity rates in the region. As a result, this enables us to identify which parameter combinations best match the recorded seismicity, prioritizing those that perform better for the hazard assessment. In addition, these optimal values might be used as indicators for further studies focused on better constraining the fault parameters in some faults, as well as for preliminary fault-based seismic hazard assessments. By extension, the limitations of the modelling in terms of slip rate budget distribution and fault rupture scenarios can also be used to determine which areas should be prioritized for further research. We expect that the results of our work enhance discussion among researchers working in the area and motivate further investigations into fault dynamics.

How to cite: Perea, H., Gómez-Novell, O., Jiménez, M. J., García, M., Lozano, L., García-Mayordomo, J., Sánchez-Roldán, J. L., Canari Bordoy, A., and Martínez-Loriente, S.: Exploring the uncertainties of the fault source parameters in the Alboran Sea for seismic hazard using earthquake rate modelling tools, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-7698, https://doi.org/10.5194/egusphere-egu24-7698, 2024.

X2.59
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EGU24-7956
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ECS
Giorgio Valentini, Tiziano Volatili, Paolo Galli, and Emanuele Tondi

This research examines the influence of static Coulomb Stress Transfer (CST) in shaping the seismic cycles associated with the Central Apennine Fault System (CAFS), an active tectonic region that witnessed numerous destructive seismic events over the last millennium.

We selected 15 seismic events in the CAFS, dating from 1279 CE to the present, all exceeding Mw 6.0. Out of these, 9 events were specifically chosen for CST analysis, based on their spatial-temporal proximity to later activated faults. The study not only investigates static stress transfer for each event, but also considers the cumulative CST from recent earthquakes, providing a holistic view of the current stress environment. Following a novel approach, we utilized a three-dimensional fault modeling technique, with ellipses representing the 2D geometry of faults at depth. This approach accounts for strike variations and employs a variable strike three-dimensional elliptical model for enhanced precision in CST calculations.

Our case studies within the CAFS suggest that CST might have been a critical factor in either triggering or inhibiting fault activities. Instances of fault reactivation following high stress transfers and scenarios showing the dampening effects of stress shadows were observed. This intricate understanding of CST has practical implications, offering insights into potential future earthquake patterns and aiding in devising targeted risk mitigation strategies.

The complexity of CAFS reveals intricate stress patterns emerging from the interplay of different seismic episodes. These patterns of stress lobes interact in complex ways, influencing adjacent faults by amplifying, neutralizing, or diversifying their CST impacts. Through detailed analyses and cutting-edge modeling techniques, our study provides valuable insights for future research directions and practical approaches to seismic risk reduction. It underscores the strong impact of CST on shaping a region's seismic history and highlights the necessity of ongoing research in this vital area of geosciences.

How to cite: Valentini, G., Volatili, T., Galli, P., and Tondi, E.: A Millennial Perspective on Coulomb Stress Transfer Impact in the seismicity of the Central Apennine Fault System, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-7956, https://doi.org/10.5194/egusphere-egu24-7956, 2024.

X2.60
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EGU24-10216
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ECS
Manuel Diercks, Zoe Mildon, Sarah Boulton, Ekbal Hussain, Cihat Alçiçek, Tunahan Aykut, and Cengiz Yıldırım

Earthquakes on normal faults cause negative Coulomb stress transfer (CST) onto receiver faults located across-strike, which, in theory, delays or prevents rupture. Nevertheless, earthquakes on such across-strike faults are frequently observed. This study explores why, and how, large earthquakes can be triggered on faults repeatedly receiving negative coseismic CST. Two triggering mechanisms are hypothesised: (1) Positively stressed patches or segments of faults, resulting from heterogeneous stress transfer, act as triggers to rupture earthquakes on faults that are on average negatively stressed. (2) Negative coseismic CST is compensated by interseismic loading and other processes building up positive stress on the source faults. To test both hypotheses, a 400-year earthquake sequence is modelled, located in the fault network of the Western Anatolian Extensional Province (SW Türkiye). The fault network features multiple active faults located along-strike and across-strike of another, as well as faults in a variety of orientations, suitable to explore stress-triggering mechanisms in a structurally complex setting. Detailed information on fault location, geometry, and mechanism is compiled from field investigations, literature review, and geodetic data. Based on instrumental and historical earthquake catalogues, and the suitability of the source fault network, a sequence of earthquakes is determined to investigate the two hypotheses by comparing the effects of coseismic CST and interseismic loading.

Results show that, out of 28 modelled large (MW ≥6) earthquakes, 6 were triggered on faults receiving significant negative coseismic CST. For five of these, negative coseismic CST is compensated by processes increasing CST. Only for one studied example, highly stressed positive fault segments on an otherwise negatively stressed fault could have been the driving mechanism leading to rupture of a large earthquake. Given all model uncertainties, stress-heterogeneities cannot be validated as a probable triggering mechanism for faults in the stress shadow of neighbouring faults. In contrast, earthquakes on normal faults located across-strike of another can only delay, but in most cases not prevent failure, as interseismic loading usually exceeds negative coseismic CST.

To reinforce these results, the impact of the modelled fault geometry and slip rates, used to calculate interseismic loading, is evaluated. Models of strike- and dip-variable faults, following the actual surface fault traces, are compared with simplified, planar fault models. Simplified models feature exaggerated areas of positive and negative CST on source faults prior to earthquakes, essentially distorting the stress field and causing stress-heterogeneities that are less pronounced in more realistic models. This observation highlights the necessity of modelling fault geometry as realistic as possible, especially when models are used in fault-based SHA. The impact of slip rates on model results is less drastic, so long as slip rates are used that are determined on similar time scales as the model duration. For the studied fault network short-term (geodetic) and long-term (‘geologic’) slip rates vary from the ‘Holocene’ slip rates by an order of magnitude. If used for modelling interseismic loading, the stress state and recurrence intervals of faults would be drastically under- or overestimated.

How to cite: Diercks, M., Mildon, Z., Boulton, S., Hussain, E., Alçiçek, C., Aykut, T., and Yıldırım, C.: Fault interactions and Coulomb stress-triggering in complex fault networks, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-10216, https://doi.org/10.5194/egusphere-egu24-10216, 2024.

X2.61
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EGU24-1045
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ECS
Poorvi Narayana and Javed N Mailk

The Northwestern Himalayas have been host to many earthquakes, with the recent 1905 Kangra Mw 7.8. Studies suggest the seismic gap in the Northwestern Himalayas to be more than Mw 7.8 in general, and of about Mw 8.4 in the Nahan region of the Northwestern Himalayas. There are studies suggesting the rupture of the Himalayan Frontal Thrust (HFT) and hinterland subsidiary faults by the Earthquakes in the region. In this study, we focused the Khetpurali Taksal Fault (KTF), which is one of the corroboration. It is an out-of- sequence ~ 250 km long dextral strike-slip fault with an NNW-SSE trend. KTF, which is bounded to the west by the Nahan Salient, and in the east by the Dehradun re-entrant; marks the boundary between the Central Himalayas (convergence rate ~ 18 ± 1 mm/y and obliquity ~0°) and the Northwestern Himalayas (convergence rate ~13.6–14 ± 1 mm/yr and obliquity ~ 15°-30°), which runs through the ~ 100km locked width of the Main Himalayan Trust (MHT). The dextral strike-slip motion has caused the displacement of some quaternary deposits along the KTF. It plays a key role in the slip partitioning between the active thrust and the oblique faults with the HFT displaying the thrusting and oblique component in the Pinjore Garden fault, Jhajra fault, and Barsar fault of the same region in the Northwestern Himalayas. This study is focused on the active fault along the KTF. We prepared the geomorphic map and delineated the extent of the KTF using the high-resolution Cartosat-1 data. Our studies show the presence of displaced terraces, lateral offset of streams, sag ponds, and pressure ridges along the KTF. A displacement of 250m to 1350m has been observed. Samples from the displaced terraces are analyzed by OSL dating technique to find out the slip along the KTF. Understanding the slip along KTF will enhance the understanding of slip partitioning taking place in the Nahan Region as a whole, which will help understand the geodynamics of the region and thus in seismic hazard assessment.

How to cite: Narayana, P. and Mailk, J. N.: Tectono-Geomorphic Studies along the Khetpurali Taksal Fault, Northwestern Himalayas, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-1045, https://doi.org/10.5194/egusphere-egu24-1045, 2024.

X2.62
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EGU24-13958
Research on the mechanism of earthquake induced debris flow disaster in Caotan Village, Zhongchuan Township, Minhe County, Qinghai Province, China
(withdrawn after no-show)
Wenliang Jiang, Yi Luo, Qisong Jiao, and Qiang Li
X2.63
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EGU24-15619
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ECS
Sylvain Palagonia, Frédérique Leclerc, Christophe Larroque, Lucilla Benedetti, Nathalie Feuillet, Paraskevi Nomikou, Maxime Henriquet, Valery Guillou, and Fabio Manta

The study of normal fault-generated landforms, such as fault scarps, is commonly performed to investigate fault evolution and the recurrence and magnitude of earthquakes. The Amorgos region (Cyclades, Greece), located in the central part of the Aegean Sea, is structured by ~70km large NE-SW normal faults accommodating the back-arc extension of the Hellenic arc and the Anatolian extrusion. These faults are able to generate large earthquakes such as the Amorgos event (Ms=7.8) on July 09, 1956, followed by a second shock (Ms=7.2) 12 minutes later. This destructive event was the largest Mediterranean earthquake of the 20th century and caused severe damage, especially on Santorini Island. It also triggered a tsunami with reported run-ups reaching locally 30m along the southern coast of Amorgos Island. The submarine Amorgos fault, structuring the island’s southern coast and cumulating a ~2 km high vertical offset, is suggested to be the source of the 1956 main shock and tsunami. However, the accurate position of the 1956 rupture and the magnitude of the slip at surface are unknown, as the fault outcrops at 700m below sea level, as well as the pace at which this fault breaks. Considering that normal faults frequently accommodate the deformation on multiple splays, and within their damage zone, we searched whether the onland faults found within the cumulative scarp of the Amorgos fault ruptured during the 1956 event. We first performed a morphological study of the Chozoviotissa fault segment with satellite imagery, Structure-from-motion modelling, and field observations. We found evidence of recent deformation along this fault, in particular a ~70 cm high fresh ribbon at the base of the fault scarp. To provide chronological constraints, we sampled along-dip the carbonate-rich fault scarp for TCNs (Terrestrial Cosmogenic Nuclides) dating using the chlorine-36 element. This paleoseismic approach provides new insights on the recent slip history of this secondary fault, which is important to better evaluate the activity of the Amorgos fault system and improve the hazard assessment of the archipelago.

How to cite: Palagonia, S., Leclerc, F., Larroque, C., Benedetti, L., Feuillet, N., Nomikou, P., Henriquet, M., Guillou, V., and Manta, F.: Deciphering the recent activity of normal faults in the Hellenic Volcanic Arc from combined morpho-tectonics analysis and TCNs method dating (36Cl), Amorgos Island (Greece) , EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15619, https://doi.org/10.5194/egusphere-egu24-15619, 2024.

X2.64
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EGU24-16169
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ECS
Michele Locatelli, Laura Crispini, Marco Scambelluri, Laura Federico, Daniele Spallarossa, Danilo Morelli, and Paola Cianfarra

Understanding the source processes and wave propagation in heterogeneous rock media is one of the most challenging frontiers to improve the seismic risk assessments in densely populated areas. In this framework, the sector of the Voltri Massif (NW Italian Alps) forming the hinterland of the city of Genoa is a natural laboratory to investigate (i) the interaction between rock faulting and fluid circulation during (potential) paleo-seismic activity and (ii) the detection, location, and source characterization of micro-earthquakes along tectonic lineaments developed inland and offshore the city area (i.e., in the Ligurian Sea). Our multi-scale and multidisciplinary study is part of the PNRR research program RETURN (“Multi-risk science for resilient communities under a changing climate”): it will include the structural and petrographic characterization of fault rocks (i.e., serpentinite breccias), the quantification of serpentinite carbonatization and its impact on the fault strength, and the analysis of the network of inland-offshore tectonic lineaments. This work, coupled with the analysis of historical seismic clusters, is crucial to identify suitable areas for the deployment of high-resolution seismometers and for tracing the spatial-temporal evolution of micro-earthquakes and their static and dynamic source parameters.

The detailed structural mapping of selected fault zones has revealed a complex, multi-stage deformation history, with older ductile structures (paragenesis: antigorite + ilmenite ± chlorite ± pyrite ± chalcopyrite, likely ascribed to the alpine-subduction and collision stages) cut by steeply dipping fault planes NNE-SSW striking. These latter are subparallel with the (low magnitude) seismic clusters detected in the area and develop multiple, anastomosed fault cores consisting of serpentinite-rich ultracataclasites, locally bound by chrysotile-rich shear bands. The faults damage zones textures (e.g., breccias and microbreccias), the paragenesis of newly formed shear bands and associated veins (chrysotile + chlorite) and the orientation of these faults (NNE-SSW striking, subparallel to the Miocene-age lineaments detected in the Gulf of Genoa) suggest recent tectonic reactivation at the regional scale.

Future developments of the research project will include more detailed, high-magnification microscopy of selected samples (e.g., raman, field emission SEM, EBSD and microprobe), regional scale morphotectonic characterization by satellite image analysis, and integration of field and seismic data. This will clarify the link between inland-offshore tectonic lineaments and the (low magnitude) seismicity of the area.

How to cite: Locatelli, M., Crispini, L., Scambelluri, M., Federico, L., Spallarossa, D., Morelli, D., and Cianfarra, P.: Analysis of active and fossil seismic structures: a multidisciplinary study for the seismic risk assessment in low-seismicity regions, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-16169, https://doi.org/10.5194/egusphere-egu24-16169, 2024.

X2.65
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EGU24-3159
Lingyuan Meng, Yang Zang, and Mengyu Xie

The January 10, 2022, MS 6.9 Menyuan, China, earthquake occurred caused by strike-slip faulting in the tectonically complex region of the northeastern Tibetan Plateau, and ten people were injured in Menyuan City. The September 8, 2023, MS 6.9 Morocco, earthquake occurred in the African Plate at shallow depth with oblique-reverse faulting. At least 2,900 people were killed and more than 5,000 injured in Morocco till to September 13, 2023. International media reports of such kind of disasters by the Morocco earthquake only resulted from poor building structure design and low-solidity housing, such as in Marrakech, southwest of the epicenter. The surface wave magnitude (MS) of the two earthquakes is the same, and the moment magnitude (MW) and energy magnitude (Me) of the Menyuan mainshock are slightly lower than those of the Morocco event. Although the scalar moment and radiated seismic energy from Morocco dynamic rupture are only 2~3 times of the Menyuan earthquake, the density of urban residents nearby and around the epicenter of the Morocco mainshock is at least more than a hundred times higher than that around the epicenter of the Menyuan even. For the Morocco sequence, the USGS reported the number of aftershocks higher than MW4.0 is only seven and the largest is 4.9. In contrast, there are two aftershocks higher than MS5.0 in the Menyuan sequence recorded by the China Earthquake Networks Center, 5.1 and 5.2, respectively. Normally, a similar magnitude does not reflect the equivalent seismic moment, release of radiated energy, and the occurrence of strong aftershocks. Meanwhile, devastating loss of life and injuries are not only due to the design of the building and the quality of the house.

Acknowledgment: This research is supported by the Spark Program of Earthquake Sciences (XH22012YC)

How to cite: Meng, L., Zang, Y., and Xie, M.: The Differential of Casualties, Energy Radiation, and Characteristics of Sequences from the Same MS: The Menyuan MS 6.9 2022 and Morocco MS 6.9 2023 Earthquakes, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-3159, https://doi.org/10.5194/egusphere-egu24-3159, 2024.

X2.66
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EGU24-18480
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ECS
Sylvain Michel, Oona Scotti, Sebastien Hok, Harsha Bhat, Navid khairdast, Michelle Almakari, and Jinhui Cheng

The efficiency of an earthquake to cross a barrier can be evaluated based on geometric and frictional properties of faults, and specific seismic parameters such as the stress drop during an earthquake. Numerical modelling of seismic cycles allows to generate thousands of seismic events and to explore the effect of the physical properties with respect to a barrier effectiveness criteria. The probability of an event passing a barrier can thus be evaluated on the basis of this barrier effectiveness criteria. Such approach has been used for frictional barriers and fault bends. In this study we focuses on earthquake fault jumps which has been observed on multiple occasions such as the latest 2024 M7.5 earthquake in Japan. We use the quasi-dynamic algorithm VEGA, which numerically simulates seismic cycles of 2D fault networks and is based on rate and state friction. The problem is simplified to two planar faults separated by a gap. Among other parameters, we explore the effect of the overlap, distance and angle between the two faults. The loading of a fault network can be done in multiple ways. We thus explore the impact on the dynamics of sequences of earthquakes either from a far-field stress loading or from imposing a back slip rate loading on each fault. We also look at the effect of adding creeping - velocity strengthening - sections at the borders of the faults. We finally compare our results with the statistics of jump probabilities from published observed seismic events. Our study allows for a rapid assessment of thousands of earthquake scenarios and is a promising approach to facilitate the integration of earthquake physics into seismic hazard.

How to cite: Michel, S., Scotti, O., Hok, S., Bhat, H., khairdast, N., Almakari, M., and Cheng, J.: Evaluating probabilities of earthquake fault jumps from 2D numerical simulation of seismic cycles, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-18480, https://doi.org/10.5194/egusphere-egu24-18480, 2024.