Dolomite dissociation indicates ultra-deep (>150 km) subduction of a garnet-bearing dunite block (the Sulu UHP terrane)

Bin Su(Institute of Geology and Geophysics), Jingbo Liu(Fujian Medical University), Shun Guo(Chinese Academy of Sciences), Yi Chen(Institute of Tibetan Plateau Research)
American Mineralogist
November 1, 2017
10.2138/am-2017-5982
Cited by 9

Related Papers

Mineral Inclusions in Zircon from Gneisses in the Ultrahigh‐Pressure Zone of the Dabie Mountains, China
|The Journal of Geology|2001|169
Fluid–rock interaction and element mobilization in UHP metabasalt: Constraints from an omphacite–epidote vein and host eclogites in the Dabie orogen
|Lithos|2011|90
A transitional eclogite- to high pressure granulite-facies overprint on coesite–eclogite at Taohang in the Sulu ultrahigh-pressure terrane, Eastern China
|Lithos|2000|89
Nitrogen-doped carbon encapsulated trimetallic CoNiFe alloy nanoparticles decorated carbon nanotube hybrid composites modified separator for lithium‑sulfur batteries
|Journal of Energy Storage|2024|88
Detrital zircon U–Pb geochronological and sedimentological study of the Simao Basin, Yunnan: Implications for the Early Cenozoic evolution of the Red River
|Earth and Planetary Science Letters|2017|80