Mineralogical evidence for subduction zone ophiolite, Muztag, East Kunlun of Xinjiang

Kuangwu Yanshi

Volumn 22, Issue 3, 2002, Pages 1-4

  Lan, Chao li ^a   Li, Ji liang ^a   He, Shun li ^a   Wei, Jun zhi ^a  

^a CHINA UNIVERSITY OF PETROLEUM   (China)

Author keywords

East Kunlun Mountain; Muztag; Ophiolite; Spinel; Subduction zone

Indexed keywords

ENVIRONMENTAL IMPACT; TECTONICS; VOLCANIC ROCKS;

SUBDUCTION ZONE;

MINERALOGY;

FAULT; MINERALOGY; OPHIOLITE; SPINEL; SUBDUCTION ZONE;

CHINA;

EID: 0036759910     PISSN: 10016872     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (10)

1. Geologic evolution of northern Tibet: Results of an expedition to Ulugh Muztagh
2. Chromian spinel as a petrogenetic indicator in abyssal and alpine-type peridotites and spatially associated lavas
3. Petrology of a charomitite micropodiforn Hess Deep, equatorial Pacific: A comparison between abyssal and alpine-type podiforn chromitites
4. Origin and tectonic environment of podiform chromite deposits
5. Al- and Cr-rich chromites from the Mayari-Baracoa ophiolitic belt (eastern Cuba): Consequence of interaction between volatile-rich melts and peridotite in suprasubduction mantle
6. Origin of the Kunlun Mountains by arc-arc and arc-continent collisions