Paleomagnetic Evidence for 25–15 Ma Crust Fragmentation of North Indochina (23–26°N): Consequence of Collision With Greater India NE Corner?
Author:
Affiliation:
1. Istituto Nazionale di Geofisica e Vulcanologia Rome Italy
2. Dipartimento di Scienze Biologiche, Geologiche e AmbientaliUniversità degli Studi di Catania Catania Italy
3. School of Earth and Space SciencePeking University Beijing China
Funder
National Natural Science Foundation of China
National Basic Research Program of China
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008308
Reference115 articles.
1. When and where did India and Asia collide?
2. Geometry, kinematics, and regional significance of the Chong Shan shear zone, Eastern Himalayan Syntaxis, Yunnan, China
3. Discordant paleomagnetic pole positions as evidence of regional shear in the western Cordillera of North America
4. Analysis of late Jurassic-recent paleomagnetic data from active plate margins of South America
5. Northwest-trending, middle Cenozoic, left-lateral faults in southern Yunnan, China, and their tectonic significance
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