Subduction zone decoupling and rapid forearc spreading at an active continental margin: Evidence from an SSZ-type ophiolite in Qilian Orogen, NW China
Author:
Funder
National Natural Science Foundation of China
Publisher
Elsevier BV
Reference102 articles.
1. An oblique subduction model for closure of the proto-tethys and palaeo-tethys oceans and creation of the Central China Orogenic Belt;Allen;Earth Sci. Rev.,2023
2. Xigaze forearc basin revisited (South Tibet): Provenance changes and origin of the Xigaze Ophiolite;An;Geol. Soc. AM. Bull.,2014
3. SHRIMP Pb/U zircon ages constrain gabbroic crustal accretion at Atlantis Bank on the ultraslow-spreading southwest indian ridge;Baines;Earth Planet. Sci. Lett.,2009
4. Temporal evolution of mantle wedge oxygen fugacity during subduction initiation;Brounce;Geology,2015
5. Subduction zone decoupling/retreat modeling explains south Tibet (xigaze) and other supra-subduction zone ophiolites and their UHP mineral phases;Butler;Earth Planet. Sci. Lett.,2017
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