TS2.7 | Alpine-Mediterranean Tectonics: Subduction, Continental Collision, Magmatism and Volcanism
EDI
Alpine-Mediterranean Tectonics: Subduction, Continental Collision, Magmatism and Volcanism
Co-organized by GD9
Convener: Claudia Piromallo | Co-conveners: Nevena Andrić-Tomašević, Marcel Thielmann, Silvia Crosetto

Tectonics in the Alpine-Mediterranean region has been studied intensively for almost two centuries, starting with field observations and increasingly accompanied by geochemical analyses, seismicity and geohazard studies, geophysical imaging, geodesy and geodynamic modelling. Significant progress has been made in understanding the tectonic processes in the region. The area has been the breeding ground for new concepts such as subduction, nappe tectonics or exhumation of ultra-high pressure metamorphic rocks. Due to its considerable complexity, the area has been and continues to be a test bed for new imaging and geodynamic modelling techniques. However, important questions regarding the driving forces, the three-dimensional lithospheric stress field, seismic coupling, and magma ascent remain unanswered. The session will serve as an interdisciplinary platform to present recent results and new concepts, as well as to highlight open questions and methodological challenges. We invite contributions from relevant fields that help to quantify geodynamic drivers of past and present plate kinematics and lithospheric deformation. In particular, presentations on the results of passive seismic experiments and quantitative comparisons of models, concepts, and field observations are welcome.

Tectonics in the Alpine-Mediterranean region has been studied intensively for almost two centuries, starting with field observations and increasingly accompanied by geochemical analyses, seismicity and geohazard studies, geophysical imaging, geodesy and geodynamic modelling. Significant progress has been made in understanding the tectonic processes in the region. The area has been the breeding ground for new concepts such as subduction, nappe tectonics or exhumation of ultra-high pressure metamorphic rocks. Due to its considerable complexity, the area has been and continues to be a test bed for new imaging and geodynamic modelling techniques. However, important questions regarding the driving forces, the three-dimensional lithospheric stress field, seismic coupling, and magma ascent remain unanswered. The session will serve as an interdisciplinary platform to present recent results and new concepts, as well as to highlight open questions and methodological challenges. We invite contributions from relevant fields that help to quantify geodynamic drivers of past and present plate kinematics and lithospheric deformation. In particular, presentations on the results of passive seismic experiments and quantitative comparisons of models, concepts, and field observations are welcome.