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- W2391633188 abstract "The Kaiping Depression is located on the western Zhujiangkou Basin. It is a Paleogene faulted basin in the NE- ENE direction. Based on results obtained from drills and seismic reflections, five sedimentary facies are identified in the Enping Formation.The shallow lake facies is seismic facies characterized by medium frequency, strong amplitude, continuity and parallel sheet, distributed in the center depression. Littoral lake facies includes seismic facies characterized by medium- high frequency, medium amplitude,continuity, and sub-parallel sheet, on-lap seismic facies characterized by medium frequency, medium-week amplitude and medium continuity, and micro-waved seismic facies characterized by medium-high frequency, week amplitude and medium continuity, deposited on the southwestern depression. Delta facies includes progradation seismic facies characterized by high frequency, varying amplitude and medium continuity and weak- progradation seismic facies characterized by medium- high frequency, medium- week amplitude and medium continuity, mainly developed on the east and northeast. Fan delta facies is tangle-some wedge seismic facies,,characterized by low frequency, week amplitude, and low continuity, distributed on the down-thrown sides of west depression-controlling faults. Alluvial fan facies is tangle-some filling seismic facies, characterized by low frequency, week amplitude, low continuity, limited on the up-thrown side of a west depression-controlling fault." @default.
- W2391633188 created "2016-06-24" @default.
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- W2391633188 date "2014-01-01" @default.
- W2391633188 modified "2023-09-24" @default.
- W2391633188 title "Seismic Reflection and Depositional System of the Enping Formation in the Kaiping Depression of the Zhujiangkou Basin" @default.
- W2391633188 hasPublicationYear "2014" @default.
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