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The Formation and Evolution of the Anatolian Tectonic Escape System, Past and Future
FILLING IN THE MARGINS: 3D ARCHITECTURE OF CONVERGENT MARGINS AND THE TRANSFERABILITY FROM SUBDUCTION TO COLLISION II ORAL
tectonophysics | 13 december 2023
Donna L. Whitney, Jonathan R. Delph, Christian Tey...
When subduction leads to collision, the extent and nature of deformation in the non-subducting plate is controlled by pre-collision structures/process...
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Structure of the Crust and Shallow Mantle of the Central Andes between 23°S and 37°S based on Ambient Noise Tomography
TECTONIC ANATOMY OF THE ANDES: MULTITEMPORAL AND MULTISPATIAL PROCESSES SHAPING THE OROGENIC SYSTEM I POSTER
tectonophysics | 12 december 2023
Sebastian Tauber, Ryan C. Porter, Susan L. Beck, E...
The Andes, located along the western margin of South America, are the largest modern mountain range formed due to subduction. Despite relatively consi...
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Preliminary Earthquake Catalog of the Southern Central Andes (~23-24° S) Recorded by the TANGO Seismic Deployment
TECTONIC ANATOMY OF THE ANDES: MULTITEMPORAL AND MULTISPATIAL PROCESSES SHAPING THE OROGENIC SYSTEM I POSTER
tectonophysics | 12 december 2023
Sankha Subhra Mahanti, Eric Kiser, Susan L. Beck, ...
The Andes Mountain Range exhibits distinct along strike variations in crustal thickness, shortening and uplift. To understand the driving processes fo...
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Deep lithospheric controls on the formation and evolution of the East Anatolian Fault Zone and Anatolia-Arabia-Africa Triple Junction
FILLING IN THE MARGINS: 3D ARCHITECTURE OF CONVERGENT MARGINS AND THE TRANSFERABILITY FROM SUBDUCTION TO COLLISION I POSTER
tectonophysics | 12 december 2023
Jonathan R. Delph, Donna L. Whitney, Michael A. Co...
The North and East Anatolian Fault Zones represent plate-bounding conjugate transform faults that enable the westward tectonic escape of the Anatolian...
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Catching the Nazca Slab in the Act of Flattening: Insights from joint ambient noise, local, and teleseismic tomography of Ecuador
TECTONIC ANATOMY OF THE ANDES: MULTITEMPORAL AND MULTISPATIAL PROCESSES SHAPING THE OROGENIC SYSTEM II ORAL
tectonophysics | 12 december 2023
Emily E. Rodriguez, Susan L. Beck, Mario Calixto C...
The northern Andean subduction zone of South America is characterized by accreted oceanic terranes and the subduction of several bathymetric highs wit...
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The Andes, From Slab to Surface Through Large-N, Radial-Receiver Function Analysis, at 24⁰S
TECTONIC ANATOMY OF THE ANDES: MULTITEMPORAL AND MULTISPATIAL PROCESSES SHAPING THE OROGENIC SYSTEM I POSTER
tectonophysics | 12 december 2023
Jim Bradford, Sankha Subhra Mahanti, Sebastian Tau...
The Andes across northern Chile and Argentina are of the largest and widest mountain belts associated with subduction. As part of the TransANdean Grea...
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TransANdean Great Orogeny (TANGO) – High-resolution Imaging of the Andean Cordillera from the Mantle to the Surface
TECTONIC ANATOMY OF THE ANDES: MULTITEMPORAL AND MULTISPATIAL PROCESSES SHAPING THE OROGENIC SYSTEM II ORAL
tectonophysics | 12 december 2023
Susan L. Beck, Diana Comte, Eric Kiser, Steven W. ...
The Andes contain some of the highest elevations and thickest crust on Earth. Despite the scale of this orogen, there is not a comprehensive framework...
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Are Volatiles From Subducted Ridges on the Pampean Flat Slab Fracking the Crust? Evidence From an Enhanced Seismicity Catalog
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
03 october 2023
Ariane Maharaj, Steven W. Roecker, Patricia M. Alv...
Seamounts and ridges are often invoked to explain subduction‐related phenomena such as flat slab generation, but the extent of their involvem...