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Mineralogy and element geochemistry of the Sohnari rocks of Early Eocene Laki Formation in the southern indus basin,Pakistan:Implications for paleoclimate,paleoweathering and paleoredox conditions

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Energy Geoscience 2023年第1期4卷 143-157页

作者： Asghar A.A.D.Hakro Sajjad Ali Abdul Shakoor Mastoi Riaz Hussain Rajper Rizwan Sarwar Awan Muhammad Soomar Samtio Hong Xiao Xiaolin Lu Centre for Pure&Applied Geology University of SindhJamshoro76080Pakistan Xinjiang Centre for Mineral Resources Xinjiang Institute of Ecology and GeographyUrumqiXinjiang830011China College of Geosciences China University of PetroleumBeijing102249China State Key Laboratory of Petroleum Resources and Prospecting China University of PetroleumBeijing102249China School of Resources and Environmental Engineering Hefei University of TechnologyHefei Anhui230009China

The Sohnari Member of the Early Eocene Laki Formation is massively deposited in the southern indus basin of Pakistan and is considered a potential source rock to generate ***,the detailed paleoclimatic,paleoweathering,and depositional conditions of the Sohnari Member have not been studied *** research mainly discusses the detailed mineralogical(bulk and clay)and elemental geochemistry of the Laki Formation from two outcrop sections(Jhimpir and Lakhra)in the southern indus basin,*** bulk minerals,including quartz(low),hematite,calcite,halite,gypsum,and clay minerals such as kaolinite,chlorite,smectite and illite have been discussed *** results demonstrate the paleo-environment of studied area was arid with enhanced saline and weak to strong oxidizing depositional *** chemical index of alteration(CIA)values in Jhimpir and Lakhra sections are in the ranges of 41.30-97.93 and 22.30-96.19,respectively,indicating that the Sohnari sediments experienced weak to intense chemical weathering in the source *** interpretation of the A-CN-K ternary diagram is consistent with the clay mineral contents in the studied sediments,which is characterized by the predominance of kaolinite,gibbsite and chlorite,demonstrating the weak to strong weathering state under warm and humid climatic *** chemical indices such as Sr/Ba,δU,V/Cr,Ni/Co,and Cu/Zn,U/Th and Ba/Ga show that Sohnari rocks of Early Eocene Laki Formation underwent strong evaporation,oxic water column with warm to humid and minor contact of cold climatic *** on our present data,it can be concluded that the sediments of Sohnari Member of Laki Formation from Jhimpir and Lakhra areas of southern indus basin in Pakistan are related to Indio-Eurasian collision and came from the Indian shield rocks that were deposited in a brackish water body with a minor contact of the freshwater oxidizing paleo-environment depositional conditions.

关键词： Mineralogy Geochemistry Paleoclimate Sohnari southern indus basin Lakhra

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