Purang Ultramafic Complex and Their Geological Origin, Southwest Tibet

Neoproterozoic ophiolitic Serpentinites are common in the Arabian-Nubian Shield （ANS） of the Eastern Desert （ED） of Egypt, which were formed in arc stage in different tectonic setting. Thus they might subject to exchange with the crustal material derived from recycling subducting oceanic lithosphere...

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Published inActa geologica Sinica (Beijing) Vol. 89; no. 2; pp. 22 - 24
Main Authors Dien, Hamed Gamal El, Hamdy, Mohamed, El-Ela, Abdel Salam Abu, Hassan, Adel, Kil, Youngwoo
Format Journal Article
LanguageEnglish
Published Richmond Wiley Subscription Services, Inc 01.12.2015
EditionEnglish ed.
Subjects
China, People's Rep., Xizang
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Summary:Neoproterozoic ophiolitic Serpentinites are common in the Arabian-Nubian Shield （ANS） of the Eastern Desert （ED） of Egypt, which were formed in arc stage in different tectonic setting. Thus they might subject to exchange with the crustal material derived from recycling subducting oceanic lithosphere. This caused metasomatism enriching the rocks in incompatible elements and forming non- residual minerals. Herein,
Bibliography:Neoproterozoic ophiolitic Serpentinites are common in the Arabian-Nubian Shield （ANS） of the Eastern Desert （ED） of Egypt, which were formed in arc stage in different tectonic setting. Thus they might subject to exchange with the crustal material derived from recycling subducting oceanic lithosphere. This caused metasomatism enriching the rocks in incompatible elements and forming non- residual minerals. Herein
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ISSN:1000-9515
1755-6724
DOI:10.1111/1755-6724.12308_16