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 in | Acta geologica Sinica (Beijing) Vol. 89; no. 2; pp. 22 - 24 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
Published |
Richmond
Wiley Subscription Services, Inc
01.12.2015
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Edition | English ed. |
Subjects | |
Online Access | Get full text |
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