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- W2362134334 abstract "Spatial distribution and thickness changes of volcanic rocks are the crux of exploration and development for reservoirs related to volcanic rocks and their underlying strata.Based on boreholes,the comprehensive model of lithology,logging and seismology,as well as logging and seismic interpretation,spatial distribution and main controlling factors of Permian volcanic rocks in Manxi-Awati area in the Tarim Basin were studied.The results show that there are four stages of magmatism,which are early pyroclastic rock stage,basalt eruption,rhyolite eruption,later tuff stage.Basalt,basic ignimbrite,rhyolite,acid ignimbrite,airfall tuff,sandstone,mudstone could be distinguished by optimized identification models based on abundant log data.Meticulous characterization of spatial distribution show that the thickness of widely distributed basalt gradually decreased from west to east,thickness of limited distributed rhyolite varied significantly,and the thickness of widely distributed airfall tuff gradually decreased from south to north.Three main controlling factors(i.e.lithology of volcanic rocks,volcanic eruption process and paleotopography features)determined different superimposed patterns and development modes of volcanic rocks of each period.Permian volcanic rocks possess accumulation conditions in Manxi-Awati area and the study of spatial distribution lays foundation for high quality reservoir prediction and further exploration and development." @default.
- W2362134334 created "2016-06-24" @default.
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- W2362134334 date "2014-01-01" @default.
- W2362134334 modified "2023-09-23" @default.
- W2362134334 title "Spatial Distribution and Main Controlling Factors of Permian volcanic Rocks in Manxi-Awati area in the Tarim Basin" @default.
- W2362134334 hasPublicationYear "2014" @default.
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