Tectonic evolution of the Beishan orogen in central Asia: Subduction, accretion, and continent-continent collision during the closure of the Paleo-Asian Ocean

J Li, C Wu, X Chen, AV Zuza, PJ Haproff, A Yin… - …, 2023 - pubs.geoscienceworld.org
The Beishan orogen is part of the Neo-proterozoic to early Mesozoic Central Asian Orogenic
System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc …
被引用次数：29 相关文章

Tectonic evolution of the Beishan orogen in central Asia: Subduction, accretion, and continent-continent collision during the closure of the Paleo-Asian Ocean

J Li, C Wu, X Chen, AV Zuza, PJ Haproff, A Yin, Z Shao - GSA Bulletin, 2022 - par.nsf.gov
The Beishan orogen is part of the Neoproterozoic to early Mesozoic Central Asian Orogenic
System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc …
[PDF] researchgate.net

[PDF][PDF] Tectonic evolution of the Beishan orogen in central Asia: Subduction, accretion, and continent-continent collision during the closure of the Paleo-Asian Ocean

J Li, C Wu, X Chen, AV Zuza, PJ Haproff… - Geological Society of …, 2022 - researchgate.net
The Beishan orogen is part of the Neoproterozoic to early Mesozoic Central Asian Orogenic
System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc …

Tectonic evolution of the Beishan orogen in central Asia: Subduction, accretion, and continent-continent collision during the closure of the Paleo-Asian Ocean

J Li, C Wu, X Chen, AV Zuza… - … Society of America …, 2023 - ui.adsabs.harvard.edu
The Beishan orogen is part of the Neo-proterozoic to early Mesozoic Central Asian Orogenic
System in central Asia that exposes ophiolitic complexes, passive-margin strata, arc …