干旱区生态环境知识资源中心(Arid): Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area,South Eastern Desert,Egypt:constraints from their mineralogical and geochemical characteristics

Arid

	Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area,South Eastern Desert,Egypt:constraints from their mineralogical and geochemical characteristics
	Mogahed Moustafa M; Saad Wlaa Mahmoud
来源期刊	中国地球化学学报
ISSN	2096-0956
出版年	2020
卷号	39 期号:6
英文摘要	Petrological and geochemical studies of Neoproterozoic metagabbros were carried out in the Muiswirab area,South Eastern Desert of Egypt.The Muiswirab area comprises of ophiolitic metagabbroic rocks (MOM),which are tectonically thrusted over a thick pile of metavolcanic rocks and intruded by syn-and post-tectonic granitoid rocks.The whole-rock geochemical variations coupled with chemical compositions of mineral constituents are used to attain the genesis and tectonic evolution of the studied metagabbros.The geothermobarometric investigation of the analyzed amphiboles from (MOM) revealed that these metagabbros underwent regional metamorphism under lower to upper greenschist facies (biotite zone) conditions (at a temperature of 450 to 500 ℃ and pressure of 1-3 kbar).Geochemically,the metagabbros (MOM) show tholeiitic affinity and exhibiting both arc-and MORB-like characters as evidenced by their clinopyroxene compositions and the Ti/V ratios (11.84-31.65),which considered as prominent features of forearc tectonic regime.The geochemical features suggest a probable fractionation of olivine clinopyroxene plagioclase as well as insignificant crustal contamination.The parental magma of the investigated MOM rocks seems to be developed in a sub-arc mantle wedge setting due to the enrichments of LILE (e.g.,Rb,Ba,Sr,Pb) over HFSE (e.g.,Ti,Nb,Y,Zr,Hf,Ta).The studied MOM rocks have lower values of Nb/U relative to MORB and OIB indicating that their geochemical variation produced due to the enrichment of a lithosphere mantle by OIB-like components.The ratios of Zn/Fet,La/Sm,Sm/Yb,Th/Yb and Nb/Yb indicate that the MOM rocks represent a fragment of oceanic crust originated at a supra-subduction zone environment and their parental magma developed by 5-30 % partial melting of a spinel lherzolite mantle rather than pyroxenite in an island arc setting and conformable with most of the Egyptian ophiolitic metagabbros.
英文关键词	Egypt Eastern Desert Muiswirab area Ophiolitic metagabbros N-MORB Arc tholeiites Forearc tectonic regime Volcanic-arc setting
类型	Article
语种	英语
收录类别	CSCD
WOS类目	Geology
CSCD记录号	CSCD:6880707
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/354028
推荐引用方式 GB/T 7714	Mogahed Moustafa M,Saad Wlaa Mahmoud. Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area,South Eastern Desert,Egypt:constraints from their mineralogical and geochemical characteristics[J],2020,39(6).
APA	Mogahed Moustafa M,&Saad Wlaa Mahmoud.(2020).Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area,South Eastern Desert,Egypt:constraints from their mineralogical and geochemical characteristics.中国地球化学学报,39(6).
MLA	Mogahed Moustafa M,et al."Geotectonic significance of the Neoproterozoic ophiolitic metagabbros of Muiswirab area,South Eastern Desert,Egypt:constraints from their mineralogical and geochemical characteristics".中国地球化学学报 39.6(2020).