桦甸盆地古近系桦甸组油页岩矿床沉积特征

Abstract

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 3^rd 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

WANG Yong-li,LIU Zhao-jun,JING Hui-lin,ZHANG Hai-long,ZHANG Jian. Sedimentary Characteristics of Oil Shale Deposit of the Huadian Formation of Paleogene in Huadian Basin[J].J4, 2005, 35(06): 720-0724.

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