EGU26-972, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-972
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 16:15–18:00 (CEST), Display time Wednesday, 06 May, 14:00–18:00
 
Hall X4, X4.31
Tectono-Stratigraphic Characterization of the Paleocene–Eocene Interval in the Upper Assam Shelf Using Integrated 3D Seismic Attribute Analysis
Kurakula Kalyani1,2 and Param Kirti Rao Gautam1
Kurakula Kalyani and Param Kirti Rao Gautam
  • 1Wadia Institute of Himalayan Geology, Geophysics, Dehradun, India (kalyaniau23@gmail.com)
  • 2Academy of Scientific and Innovative Research, Ghaziabad, Uttar Pradesh, India,

This study presents a high-resolution tectono-stratigraphic characterisation of the Palaeocene–Eocene Sylhet–Kopili interval on the Upper Assam Shelf using a 371.5 km² 3D post-stack time-migrated seismic volume integrated with two deep wells. Targeting the 2.5–3.5 s TWT interval, time-slices (3.048–3.200 s) combined with geometric (dip, curvature), discontinuity (similarity), and amplitude-based (reflection magnitude) attributes reveal two distinct structural domains. The north-western sector is dominated by syn-depositional normal faults forming tilted blocks and fault-bend folds, whereas the south-eastern sector is characterized by E–W to ENE–WSW sinistral strike-slip faults, S-shaped bends, relay splays, and NE–SW transfer faults that generate localized transtensional pull-apart structures. Dip and curvature attributes enhance fault-plane continuity and fault-block geometries, while reflection magnitude highlights deformation-controlled variations in reflector strength and stratigraphic contrast within the Kopili and Prang intervals. Similarity and dip-magnitude co-interpretation sharply delineate fault segmentation, linkage zones, and deformation intensity, significantly improving structural resolution compared to conventional seismic interpretation. Synthetic ties to wells W-01 and W-02 (correlation 0.6–0.72) validate key horizons and strengthen structural control. This work provides the first high-resolution 3D multi-attribute imaging of the Sylhet-Kopili interval, resolving deformation styles previously undocumented in the Upper Assam Shelf. The resulting framework delineates multiple trap geometries-tilted blocks, horsts, and fault-bend closures—and demonstrates the value of integrated dip, curvature, similarity, and magnitude attributes for improving tectono-stratigraphic interpretation in foreland basin settings.

How to cite: Kalyani, K. and Kirti Rao Gautam, P.: Tectono-Stratigraphic Characterization of the Paleocene–Eocene Interval in the Upper Assam Shelf Using Integrated 3D Seismic Attribute Analysis, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-972, https://doi.org/10.5194/egusphere-egu26-972, 2026.