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《Journal of Jilin University(Earth Science Edition)》 2006-06
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The Forming Environment and Sedimentary Evolution of the Oil Shale Intergrowthing with Salt Alkali Mine——With the Oil Shale Deposit of Wucheng,Tongbai Basin as an Example

ZHOU Zhen-qi~1,DONG Qing-shui~2,HOU Gang-fu~2,XU Sheng-chuan~2,MIAO Chang-sheng~21.College of Resources,China University of Geoscience,Wuhan 430074,China2.College of Earth Sciences,Jilin University,Changchun 130061,China  
The oil shale of Wulidui Formation in the Wucheng Basin,Tongbai occurs as brown-black,thin and soft slices with an average oil yield up to 6.2%.Many sparsely disseminated and nodular pyrite can be found in the oil shales.With the oil shale occurring in the bottom,trona,salt,dolomite and silty mud rock also the oil shale make up many sedimentary rhythms.The study show that the oil shale was formed in a closed intermountainal basin under muggy climate,stable tectonic environment and sparse supply of terrestrial debrics.Standing water featured by week deoxidize-deoxidize and brackish water-saltwater is suggested for their deposition.Within a prevailing dry,but sometimes with dry-wet alternated,closed intermountainal basin,the oil shale of Wulidui Formation,together with trona,salt,dolomite and silty mud rock,underwent a climatic variation circle from hot-humid →dry-heat→ intensively dry-heat→dry-heat→hot-humid.
【Fund】: 国家重大专项(ZP-Y-01)
【CateGory Index】: P618.12
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