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Sedimentary Characteristics of Oil Shale Deposit of the Huadian Formation of Paleogene in Huadian Basin

WANG Yong-li1,LIU Zhao-jun1,JING Hui-lin2,ZHANG Hai-long1,ZHANG Jian1   

  1. 1.College of Earth Sciences, Jilin University，Changchun 130061,China； 2.The Coalfield Perambulation Design Research Institute of Jilin Province, Changchun 130062,China
  • Received:2005-07-04 Revised:1900-01-01 Online:2005-11-26 Published:2005-11-26
  • Contact: WANG Yong-li

Abstract: The Huadian basin situated in southern Jilin Province of NE China is a halfgraben basin and lies to north of the Dunhua-Mishan faults. The thickness of oil shalebearing strata and monolayer increase gradually from north to south under the control of the contemporaneity fault (F1). The fault also controlled basin filling features of the Huadian basin. The whole sequence of Huadian Formation of Paleogene in Huadian basin comprises a complete 3rd order sequence. The oil shales within the sequence were deposited in semideep to deep lacustrine environments, and were developed during transgressive systems tract and highstand systems tract. In Huadian basin, there are 13 oil shale layers containing highmobile oil (commonly 8%~13%). These high quality oil shales may have the potential for industrial use.

Key words: Huadian basin, Huadian Formation of Paleogene, oil shale, sedimentary environment

CLC Number: 

  • P618.12
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