Highly depleted harzburgite–dunite–chromitite complexes from the Neoproterozoic ophiolite, south Eastern Desert, Egypt: A possible recycled upper mantle lithosphere-Reference-Cited by-同舟云学术

Highly depleted harzburgite–dunite–chromitite complexes from the Neoproterozoic ophiolite, south Eastern Desert, Egypt: A possible recycled upper mantle lithosphere

Published:2013-08 Issue: Volume:233 Page:173-192
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Ahmed Ahmed Hassan

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference121 articles.

1. Geochemistry and tectonic evolution of the Neoproterozoic Wadi Ghadir ophiolite, Eastern Desert, Egypt;Abd El-Rahman;Lithos,2009

2. Diversity of platinum-group minerals in podiform chromitites of the late Proterozoic ophiolite, Eastern Desert, Egypt: genetic implications;Ahmed;Ore Geology Reviews,2007

3. Unexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonic implications;Ahmed;Contributions to Mineralogy and Petrology,2002

4. Platinum-group minerals in podiform chromitites of the Oman ophiolite;Ahmed;Canadian Mineralogist,2003

5. Petrological characteristics of podiform chromitites and associated peridotites of the Pan African ophiolite complexes of Egypt;Ahmed;Mineralium Deposita,2001

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