干旱区生态环境知识资源中心(Arid): Geochemistry of an Alaskan-type mafic-ultramafic complex in Eastern Desert, Egypt: New insights and constraints on the Neoproterozoic island arc magmatism

Arid

	Geochemistry of an Alaskan-type mafic-ultramafic complex in Eastern Desert, Egypt: New insights and constraints on the Neoproterozoic island arc magmatism
	Abdallah Shehta E; Ali Shehata; Obeid Mohamed A
来源期刊	Geoscience Frontiers
ISSN	1674-9871
出版年	2019
卷号	10 期号:3 页码:941-955
英文摘要	Mikbi intrusion (MI) is a part of the Neoproterozoic Nubian Shield located along the NE-SW trending major fracture zones prevailing southern Eastern Desert of Egypt. In this study, we present for the first time detailed mineralogical and bulk-rock geochemical data to infer some constraints on the parental magma genesis and to understand the tectonic processes contributed to MI formation. Lithologically, it is composed of fresh peridotite, clinopyroxenite, hornblendite, anorthosite, gabbronorite, pyroxene amphibole gabbro, amphibole gabbro and diorite. All rocks have low Th/La ratios (mostly <0.2) and lack positive Zr and Th anomalies excluding significant crustal contamination. They show very low concentrations of Nb, Ta, Zr and Hf together with sub-chondritic ratios of Nb/Ta (2-15) and Zr/Hf (19-35), suggesting that their mantle source was depleted by earlier melting extraction event. The oxygen fugacity (logfO_2) estimated from diorite biotite is around the nickel-nickel oxide buffer (NNO) indicating crystallization from a relatively oxidized magma. Amphiboles in the studied mafic-ultramafic rocks indicate relative oxygen fugacity (i.e. ∆NNO; nickel-nickel oxide) of 0.28-3 and were in equilibrium mostly with 3.77-8.24 wt.% H_2O_(melt) (i.e. water content in the melt), consistent with the typical values of subduction-related magmas. Moreover, pressure estimates (0.536.79 kbar) indicate polybaric crystallization and suggest that the magma chamber(s) was located at relatively shallow crustal levels. The enrichment in LILE (e.g., Cs, Ba, K and Sr) and the depletion in HFSE (e.g., Th and Nb) relative to primitive mantle are consistent with island arc signature. The olivine, pyroxene and amphibole compositions also reflect arc affinity. These inferences suggest that their primary magma was derived from partial melting of a mantle source that formerly metasomatized in a subduction zone setting. Clinopyroxene and bulkrock data are consistent with orogenic tholeiitic affinity. Consequently, the mineral and bulk-rock chemistry strongly indicate crystallization from hydrous tholeiitic magma. Moreover, their trace element patterns are subparallel indicating that the various rock types possibly result from differentiation of the same primary magma. These petrological, mineralogical and geochemical characteristics show that the MI is a typical Alaskan-type complex.
英文关键词	Alaskan-type complex Neoproterozoic Arc magmatism Eastern desert Egypt
类型	Article
语种	英语
开放获取类型	DOAJ Gold
收录类别	CSCD
WOS研究方向	Geology
CSCD记录号	CSCD:6493366
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/336114
作者单位	Abdallah Shehta E, Geology Department, Faculty of Science, Zagazig University, Zagazig, 44519, Egypt.; Ali Shehata, Geology Department, Faculty of Science, Minia University, Minia, 61519, Egypt.; Obeid Mohamed A, Geology Department, Faculty of Science, Fayoum University;;Faculty of Petroleum and Mining Sciences, Alexandria University (Matrouh Branch), ;;, Fayoum;;Egypt, Egypt;; 63514;;.
推荐引用方式 GB/T 7714	Abdallah Shehta E,Ali Shehata,Obeid Mohamed A. Geochemistry of an Alaskan-type mafic-ultramafic complex in Eastern Desert, Egypt: New insights and constraints on the Neoproterozoic island arc magmatism[J],2019,10(3):941-955.
APA	Abdallah Shehta E,Ali Shehata,&Obeid Mohamed A.(2019).Geochemistry of an Alaskan-type mafic-ultramafic complex in Eastern Desert, Egypt: New insights and constraints on the Neoproterozoic island arc magmatism.Geoscience Frontiers,10(3),941-955.
MLA	Abdallah Shehta E,et al."Geochemistry of an Alaskan-type mafic-ultramafic complex in Eastern Desert, Egypt: New insights and constraints on the Neoproterozoic island arc magmatism".Geoscience Frontiers 10.3(2019):941-955.