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作 者:Muhammad Asif Noonari Surih Sibaghatullah Jagirani Huafeng Tang Asghar A. A. D. Hakro Ali Ghulam Sahito Kaleemullah Jagirani Shahid Ali Shaikh Muhammad Dodo Jagirani Muhammad Asif Noonari;Surih Sibaghatullah Jagirani;Huafeng Tang;Asghar A. A. D. Hakro;Ali Ghulam Sahito;Kaleemullah Jagirani;Shahid Ali Shaikh;Muhammad Dodo Jagirani(College of Earth Science, Jilin University, Changchun, China;Centre for Pure and Applied Geology University of Sindh, Jamshoro, Pakistan;Institute of Tibetan Plateau Research, Chinese Academy of Science, Beijing, China;Oil and Gas Development Company Limited, Islamabad, Pakistan;Department of Geography University of Sindh, Jamshoro, Pakistan)
机构地区:[1]College of Earth Science, Jilin University, Changchun, China [2]Centre for Pure and Applied Geology University of Sindh, Jamshoro, Pakistan [3]Institute of Tibetan Plateau Research, Chinese Academy of Science, Beijing, China [4]Oil and Gas Development Company Limited, Islamabad, Pakistan [5]Department of Geography University of Sindh, Jamshoro, Pakistan
出 处:《Open Journal of Geology》2021年第6期183-196,共14页地质学期刊(英文)
摘 要:This study determines the geochemical and depositional environment analysis of the sediments of the Sohnari Member of the Laki Formation, Northern Kirthar Fold Belt of Pakistan. The Energy-Dispersive-X-Ray Spectroscopy (EDS) technique is used for the detection of major elements and the effects of shifting depositional climatic conditions of six representative samples which were acquired from the Sohnari Member of the Laki Formation at Lakhra area, Sindh, Pakistan. The sedimentological studies clarify that the sediments the Sonahri Member are relatively immature and most migrated in clastic mode. The availability of Silica shows that the Member was formed due to biochemical precipitation and detrital mode and was deposited at a fast rate of sediment deposition under the fluvio-deltaic depositional system. This is also deduced that the rapid rate of sediment deposition might be created a reducing atmosphere and allowing for the mineralization of sulphur.This study determines the geochemical and depositional environment analysis of the sediments of the Sohnari Member of the Laki Formation, Northern Kirthar Fold Belt of Pakistan. The Energy-Dispersive-X-Ray Spectroscopy (EDS) technique is used for the detection of major elements and the effects of shifting depositional climatic conditions of six representative samples which were acquired from the Sohnari Member of the Laki Formation at Lakhra area, Sindh, Pakistan. The sedimentological studies clarify that the sediments the Sonahri Member are relatively immature and most migrated in clastic mode. The availability of Silica shows that the Member was formed due to biochemical precipitation and detrital mode and was deposited at a fast rate of sediment deposition under the fluvio-deltaic depositional system. This is also deduced that the rapid rate of sediment deposition might be created a reducing atmosphere and allowing for the mineralization of sulphur.
关 键 词:Energy Dispersive X-Ray Spectroscopy GEOCHEMISTRY Sohnari Member the Laki Formation Northern Kirthar Fold Belt of Pakistan
分 类 号:P53[天文地球—古生物学与地层学]
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