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
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01.12.2015
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| Edition | English ed. |
| Subjects | |
| Online Access | Get full text |
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| Abstract | 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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| AbstractList | 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, |
| Author | Hamed Gamal El Dien Mohamed Hamdy Abdel Salam Abu EI-Ela Adel Hassan Youngwoo Kil |
| AuthorAffiliation | Geology Department, FaculW of Science, Tanta University, 31527 Tanta, Egypt Department of earth sciences, school of natural science, kanazawa university, Japan Department of Energy and Resources Engineering College of Engineering Chonnam National University, Yongbong-ro,Buk-gu, Gwangju, Korea |
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| Copyright | 2015 Geological Society of China |
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| DOI | 10.1111/1755-6724.12308_16 |
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| Notes | 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 11-2001/P ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| Title | Purang Ultramafic Complex and Their Geological Origin, Southwest Tibet |
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