THE SEDIMENTARY FACIES OF THE SECOND MEMBER OF BAOQUANLING FORMATION AROUND FZ4 EXPLORATORY WELL IN THE FANGZHENG FAULTED DEPRESSION
LIU Qun1, GUO Wei2, JIN Zhen-hua3
1. Heilongjiang Institute of Geophysical Exploration, Harbin 150036, China; 2. Jilin University, Changchun 130061, China; 3. Jilin Institute of Geological Sciences, Changchun 130012, China
Abstract：Based on the drill hole, logging and seismic data, the styles and distribution of the sedimentary facies of the second member of Baoquanling Formation in Fangzheng faulted depression are studied with sedimentological and geophysical theories. The results show that the sedimentary facies types are mainly fan delta facies, lacustrine facies and sublacustrine fan facies. According to the correlation between sedimentary facies and seismic facies, it is identified that the second member of Baoquanling Formation belongs to the fan delta-shore shallow lake-semi-deep lake sedimentary system with developed horizontal drainage.
刘群, 郭巍, 金珍花. 方正断陷方4井区宝泉岭组二段沉积相研究[J]. 地质与资源, 2014, 23(6): 567-573.
LIU Qun, GUO Wei, JIN Zhen-hua. THE SEDIMENTARY FACIES OF THE SECOND MEMBER OF BAOQUANLING FORMATION AROUND FZ4 EXPLORATORY WELL IN THE FANGZHENG FAULTED DEPRESSION. GEOLOGY AND RESOURCES, 2014, 23(6): 567-573.
2014, Vol. 23 
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