鄂尔多斯地区中上元古界分布与沉积环境及其油气勘探潜力
[Abstract]:With the discovery of middle and upper Proterozoic oil and gas reservoirs at home and abroad, especially Jixian bitumen in the southwest margin of the Ordos Basin and natural gas in the Great Wall system in the Yimeng uplift area in the northern part of the basin, The Middle and Upper Proterozoic in Ordos area is becoming a potential oil and gas exploration field. Ordos area is located in the western part of North China craton, where the Middle and Upper Proterozoic unconformities cover the craton crystalline basement consolidated by Lv Liang movement. It is widely distributed and has no obvious metamorphism. However, in the past, oil and gas exploration focused on the Middle Palaeozoic, and few studies on the Middle and Upper Proterozoic have been made, which leads to the weak study of the Middle and Upper Proterozoic. In order to understand the oil and gas exploration potential of Middle and Upper Proterozoic in Ordos area, this paper, on the basis of systematical arrangement and summary of previous research results, through field investigation, profile measurement, analysis and test, combined with logging data, The classification and distribution characteristics, sedimentary facies and evolution of the Middle and Upper Proterozoic strata in the study area were comprehensively studied by drilling cores and the latest seismic profiles, gravity and magnetic data, and the favorable exploration potential areas were predicted. The following knowledge is obtained: (1) on the basis of zircon U-Pb age test and previous research results, the Huangqikou formation, Ruyang Group, Haiyuan Group belong to the Great Wall system and Wang Quankou formation belong to Jixian system. The division and correlation scheme of Middle and Upper Proterozoic strata in Ordos Basin and its periphery are drawn up, and the distribution maps of Great Wall system, Jixian system and Sinian system are drawn up. (2) using logging, seismic and geochemical test data and field observation, etc. The sedimentary facies and environment of the Middle Proterozoic in the study area are analyzed. The results show that Xionger Group is a sea-land interactive sedimentary environment; Gaoshanhe Group is tidal flat facies, Huangqikou formation is coastal-lagoon facies, Luonan Group and Wangchuankou formation are carbonate platform tidal flat facies, Baizhugou formation is coastal-shallow shelf facies, and Huangqiankou formation is coastal-lagoon facies, and Huangqankou formation is coastal-lagoon facies. The looping formation and Zhengmuguan formation are coastal-glacier facies sediments. (3) according to the evaluation criteria, combined with the organic geochemical test and analysis data, The middle and upper Proterozoic source rocks and favorable areas in the southern margin of the basin are evaluated. The mudstones of the Great Wall system and the Sinian system are poor source rocks with a certain hydrocarbon generation potential. Jixian marine carbonate rocks are poor-medium hydrocarbon source rocks, and have a certain hydrocarbon generation capacity. The mudstone of the Baizhugou formation is a non-hydrocarbon source rock. (4) combined with the distribution of the Middle and Upper Proterozoic and the analysis of the pool-forming assemblages, the favorable areas for oil and gas exploration are divided into three types: the upper generation and the lower reservoir type, the Jixian system self-generating type and the Great Wall system self-generating type.
【学位授予单位】:西北大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:P618.13
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