East Asia Lithosphere Structure and Evolution
East Asia Lithosphere Structure and Evolution
Session ID#: 121053
Session Description:
East Asia represents one of most tectonically active regions on Earth. As the end of the plate circuit, East Asian tectonics, lithosphere structure and mantle dynamics are important for understanding global plate tectonics and Earth evolution. Debated tectonic events include Paleozoic-Mesozoic craton destruction, intraplate orogeny and magmatism, sedimentary basins and complex continental blocks, as well as Cenozoic intra-continental deformation, extension, marginal sea opening, and topographic inversion. In view of the recent abundant research on the observation and modeling of lithospheric structure and dynamics, we hope to seek contributions from observational constraints, novel syntheses, and modeling of any aspect of East Asian continent and its rich Phanerozoic tectonic history. Related fields may include but are not limited to geology, geophysics, neotectonics, geochemistry, geochronology, seismology, stratigraphy, paleomagnetism, and geodynamics.
Co-Organized:
- S - Seismology
Index Terms:
0545 Modeling [COMPUTATIONAL GEOPHYSICS]
8011 Kinematics of crustal and mantle deformation [STRUCTURAL GEOLOGY]
8110 Continental tectonics: general [TECTONOPHYSICS]
8120 Dynamics of lithosphere and mantle: general [TECTONOPHYSICS]
Primary Convener: Shuwen Dong, SinoProbe Center, Chinese Academy of Geological Sciences, Beijing, China; Nanjing University, School of Geoscience and Engineering, Nanjing, China
Conveners: Oleg V Petrov, VSEGEI, Saint-Petersburg, Russia, Lijun Liu, University of Illinois at Urbana-Champaign, Urbana, IL, United States and Maximiliano Bezada, University of Minnesota, Earth Science, Minneapolis, MN, United States
Primary Liaison: Shuwen Dong, SinoProbe Center, Chinese Academy of Geological Sciences, Beijing, China; Nanjing University, School of Geoscience and Engineering, Nanjing, China
See more of: Tectonophysics