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Wet Alluvial Fan Sedimentary in the Guantao Formation of Shuyi Area

Guo Jianhua

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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 effec t on sedimentary facies.

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What this paper is about

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 effec t on sedimentary facies.

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Available 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 effec t on sedimentary facies.

Key concepts: Facies, Clastic rock, Geology, Alluvial fan, Lithology, Sedimentary rock, Conglomerate, Feature (linguistics)

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