2006
DOI: 10.1016/j.jafrearsci.2006.02.003
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Abu Hamamid Neoproterozoic Alaskan-type complex, south Eastern Desert, Egypt

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Cited by 73 publications
(65 citation statements)
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“…It is believed that the continuous reaction with enstatite led to the enrichment of Al and Mg in the Cr-spinel, whereas the enstatite became enriched in Cr and Fe. Similar interpretations were assigned to reverse zonation in spinel grains from the Rhum-layered mafic-ultramafic complex in Scotland [37] and also to spinel grains from the Gabbro Akarem Alaskan-type mafic-ultramafic complex in Egypt [24,75,76].…”
Section: Elemental Exchange With Coexisting Silicate Mineralsmentioning
confidence: 54%
“…It is believed that the continuous reaction with enstatite led to the enrichment of Al and Mg in the Cr-spinel, whereas the enstatite became enriched in Cr and Fe. Similar interpretations were assigned to reverse zonation in spinel grains from the Rhum-layered mafic-ultramafic complex in Scotland [37] and also to spinel grains from the Gabbro Akarem Alaskan-type mafic-ultramafic complex in Egypt [24,75,76].…”
Section: Elemental Exchange With Coexisting Silicate Mineralsmentioning
confidence: 54%
“…The thrust ophiolites are generally dismembered, representing remnants of oceanic lithosphere that coexisted with the ANS Neoproterozoic intra-oceanic arcs. The intrusive mafic-ultramafic complexes form undeformed, small, elliptical outcrops and are commonly concentrically zoned or layered intrusions as well as dyke-like intrusions (Helmy and El Mahallawi 2003;Farahat and Helmy 2006;Azer and Gharbawy 2011;Azer et al 2012). Neoproterozoic ophiolites are common in the central and southern sectors of the Eastern Desert of Egypt (Text- fig.…”
Section: Regional Geologymentioning
confidence: 99%
“…On the other hand, the ultramafic rocks of layered mafic-ultramafic intrusions show a wide variation in rock types, including wehrlite, dunite, lherzolite and pyroxenites with minor harzburgite. (Khudeir 1995;Helmy and El-Mahallawi 2003;Farahat and Helmy 2006;Helmy et al 2008;Azer and ElGharabawy 2011). The present study suggests harzburgite and dunite protoliths for the serpentinites of Gabal El-Degheimi due to the abundance of bastite and mesh textures, similar in this regard to the ophiolitic serpentinites of the ANS.…”
Section: Correlations With Other Late Neoproterozoic Ultramafic Rocksmentioning
confidence: 99%
“…Recent isotopic studies of one of these complexes revealed a Sm/Nd age of 770 Ma (Helmy et al, 2005). The evidence for island arc setting of these complexes comes from the general geologic context, field relations, mineralogy, and mineral and bulk -rock chemistry (Helmy and El Mahallawi, 2003;Farahat and Helmy, 2006).…”
Section: Geological Background and Petrographymentioning
confidence: 99%