Neoproterozoic (835–720 Ma) Serpentinites in the Eastern Desert, Egypt: Fragments of Forearc Mantle

Most Neoproterozoic ophiolites of the Arabian‐Nubian Shield show compositions consistent with formation in a suprasubduction zone environment, but it has not been clear whether this was in a forearc or back‐arc setting. Ophiolitic serpentinites are common in the Eastern Desert of Egypt, but their co...

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Veröffentlicht in:	The Journal of geology 2007-07, Vol.115 (4), p.457-472
Hauptverfasser:	Azer, Mokhles K., Stern, Robert J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Chemical composition Chromium Deserts Forearcs Geological time Minerals Olivine Peridotite Petrology Rocks Spinel Stratigraphy Tectonics Wadis
Online-Zugang:	Volltext
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