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GUO Jian-hua, ZHU Mei-heng, YANG Shen-gu, LIU Chen-sheng. Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area[J]. Acta Sedimentologica Sinica, 2003, 21(3): 367-372.
Citation: GUO Jian-hua, ZHU Mei-heng, YANG Shen-gu, LIU Chen-sheng. Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area[J]. Acta Sedimentologica Sinica, 2003, 21(3): 367-372.

Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area

  • Received Date: 2002-04-06
  • Rev Recd Date: 2002-06-21
  • Publish Date: 2003-09-10
  • According to core observation, the coarse clastic rock in the area is studied in detail with seismic data and well logging date. The result shows that the coars e clastic rock is formed in wet alluvial fan. The lithologic character, geolog ic climate feature and the types of micro-facies in the Guantao Formation are analyzed and the models of facies are also concluded in this paper. Through detailed study, the paper further illuminate that the base level cycle has effect on sedimentary facies.
  • [1] 辽河油田石油地质志编辑委员会.中国石油地质志(卷三)-辽河油田[M].北京:石油工业出版社,1993.31~123[Editorial Committee of "Petrileum Geology of Liaohe Oil-field". Petroleum Geology of China(Vol.3)[M]. Beijing:Petroleum Industry Press,1993.31~123]
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    [6] Cross T A. Controls on coal distrbution in trasgressive-regressive cycles, Upper Cretaceous, Eastern Interior, U S A[A]. In:Wilaus C K, et al eds. Sea-level Changes:An Integrated Approach[C]. SEPM. SPec. Publ.,1998,42:371~380
    [7] 邓宏文.美国层序地层研究中的新学派-高分辨率层序地层学[J].石油天然气地质,1995,16(2):90~97[Deng Hongwen. A new School of thoutght in sequence stratigraphic studies in U.S.:High-reslution sequence stratigrphy[J]. Oil and Gas Geology, 1995,16(2):90~97]
    [8] 郭建华,宫少波,吴东胜等. 陆相断陷湖盆T-R旋回沉积层序与研究实例[J].沉积学报,1998,16(1):8~14[Guo Jianhua, Gong Shaobo,Wu Dongsheng. Sedimentary sequence of T-R cycle and a case study in the continental fault lacustrine basin[J]. Acta Sedimentologica Sinica,1988,16(1):8~14]
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    [10] Ryang W H, Chough S K. Sequential development of alluvial/lacustrine system:southeastern Eumsung, Basin,Korea[J]. Journal of Sedimentary Research,1997,67(1):274~285
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  • Received:  2002-04-06
  • Revised:  2002-06-21
  • Published:  2003-09-10

Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area

Abstract: According to core observation, the coarse clastic rock in the area is studied in detail with seismic data and well logging date. The result shows that the coars e clastic rock is formed in wet alluvial fan. The lithologic character, geolog ic climate feature and the types of micro-facies in the Guantao Formation are analyzed and the models of facies are also concluded in this paper. Through detailed study, the paper further illuminate that the base level cycle has effect on sedimentary facies.

GUO Jian-hua, ZHU Mei-heng, YANG Shen-gu, LIU Chen-sheng. Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area[J]. Acta Sedimentologica Sinica, 2003, 21(3): 367-372.
Citation: GUO Jian-hua, ZHU Mei-heng, YANG Shen-gu, LIU Chen-sheng. Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area[J]. Acta Sedimentologica Sinica, 2003, 21(3): 367-372.
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