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《Bulletin of Mineralogy,Petrology and Geochemistry》 2017-01
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Formation of Authigenic Clay Minerals in Hydrothermal Events Developed Regions:A Case Study from the Fushan Depression,Beibuwan Basin

LIU En-tao;WANG Hua;SHEN Neng-ping;ZHAO Jian-xin;FENG Yue-xing;UYSAL I Tongu;Faculty of Marine Sciences,China University of Geosciences;Key Laboratory of Tectonics and Petroleum Resources,China University of Geosciences;State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences;Radiogenic Isotope Facility,School of Earth Sciences,The University of Queensland;  
The formation process of authigenic clay minerals is a scientific issue that has received widespread attention,and a better understanding of this process is of great significance for thermal history analysis of basins. In this study,we conducted a systematic study of mineralogy,Rb-Sr isotopic dating and ~(40)Ar-~(39)Ar dating on the different size fractions of clay minerals separated from sandstones in the adjacent area of a large-scale igneous intrusion in the Fushan Depression,Beibuwan Basin. Our results suggest that authigenic clays in coarse sandstones are ideal for the dating due to enrichment of pure clay minerals. Rb-Sr isochron dating determined the formation age of authigenic clay minerals( at ~ 31 Ma),which matches well with the youngest zircon U-Pb ages of the igneous rocks. By contrast,~(40)Ar-~(39)Ar dating provided an unreliable age because of a serious loss of 40 Ar. This study suggests that the formation process of authigenic clay minerals in hydrothermal-developed regions is mainly controlled by short-time hydrothermal event( igneous intrusion) rather than long-time stepwise burial.
【Fund】: 中央高校基本科研业务费和专项资金资助项目(26420160184);; 国家自然科学基金项目(41472084);; 教育部构造与油气资源重点实验室开放基金项目(TPR-2014-16)
【CateGory Index】: P618.13
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