Mineralogy, Petrology and Geochemistry of Peridotites from the Northern Ophiolititc Sub-belt, Western Yarlung Zangbo Suture Zone, Tibet
Ophiolites, mostly found in orogenic belts, represent fragments of palaeo-oceanic lithosphere emplaced on the continent through tectonic processes (Bizimis et al., 2000; Dilek and Fumes, 2011, 2014; Pearce, 2014). These remnants of ancient oceanic lithosphere have recorded important information for...
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Published in | Acta geologica Sinica (Beijing) Vol. 89; no. s2; pp. 44 - 46 |
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Main Authors | , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Richmond
Blackwell Publishing Ltd
01.12.2015
Wiley Subscription Services, Inc |
Edition | English ed. |
Subjects | |
Online Access | Get full text |
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Summary: | Ophiolites, mostly found in orogenic belts, represent fragments of palaeo-oceanic lithosphere emplaced on the continent through tectonic processes (Bizimis et al., 2000; Dilek and Fumes, 2011, 2014; Pearce, 2014). These remnants of ancient oceanic lithosphere have recorded important information for the magmatic, |
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Bibliography: | 11-2001/P Ophiolites, mostly found in orogenic belts, represent fragments of palaeo-oceanic lithosphere emplaced on the continent through tectonic processes (Bizimis et al., 2000; Dilek and Fumes, 2011, 2014; Pearce, 2014). These remnants of ancient oceanic lithosphere have recorded important information for the magmatic ArticleID:ACGS12308_31 ark:/67375/WNG-JD4JV6WT-3 istex:7919B4D9F0F92EBC132FD61504BAC6027E7C23FC ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1000-9515 1755-6724 |
DOI: | 10.1111/1755-6724.12308_31 |