Mantle Flow Deflected by Arc–Continent Collision and Continental Subduction in Eastern Indonesia
Author:
Affiliation:
1. Department of Earth Science, University of Southern California, Los Angeles, California, U.S.A.
2. Research School of Earth Sciences, Australian National University, Canberra, Australian Capital Territory, Australia
Abstract
Publisher
Seismological Society of America (SSA)
Subject
Geophysics
Link
https://pubs.geoscienceworld.org/ssa/srl/article-pdf/93/3/1812/5596129/srl-2021281.1.pdf
Reference146 articles.
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2. Geological evidence for the geographical pattern of mantle return flow and the driving mechanism of plate tectonics;Alvarez;J. Geophys. Res.,1982
3. Amaru M. L. 2007. Global travel time tomography with 3-D reference models, Ph.D. Thesis, Utrecht University, Utrecht, Netherlands.
4. Subduction and eduction of continental crust: Major mechanisms during continent-continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides;Andersen;Terra Nova,1991
5. The geology of Portuguese Timor;Audley-Charles;Geol. Soc. Lond. Mem.,1968
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1. Protolith origin and plate tectonic setting of metamorphic complexes in the Timor fold and thrust belt, Indonesia;Earth-Science Reviews;2023-11
2. Unraveling an enigmatic boundary along the Sunda-Banda volcanic arc;Earth and Planetary Science Letters;2022-12
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