江西省富有機(jī)質(zhì)頁(yè)巖層系構(gòu)造埋藏史與頁(yè)巖氣富集
[Abstract]:Taking the organic shale stratigraphy of Jiangxi Province as the research object, this paper adopts the systematic method of literature investigation, field geological investigation, experimental test, software simulation and theoretical research. Taking the history of structural burial and preservation and enrichment of rich organic shale series as the core scientific problems, on the basis of the restoration of tectonic evolution history in various regions, the burial history of rich organic shale strata is restored. The distribution relationship between burial, heating, maturity and hydrocarbon generation and the conditions of shale gas preservation were further studied, and the enrichment model of shale gas in Jiangxi Province was explored, and the favorable areas for enrichment were optimized. The results show that the formation process of rich organic shale strata is influenced by the multi-stage tectonic movements, such as Jinning, Caledonian, Hercynian, Indosinian and so on, resulting in the formation of multiple tectonic cycles. Except that the burial history of northwest Jiangxi belongs to "early fall and late lift" type, the buried history of northeast Jiangxi and Pingle depression all belong to "early lift and late fall" type, which has experienced many subsidence-uplift stages, and the maximum buried depth has occurred in the Himalayan period. The hydrocarbon generation peak of Cambrian shale in northwest Jiangxi is located at the end of Silurian period, the hydrocarbon generation peak of other shale strata is between Jurassic and Paleogene, and the hydrocarbon generation is accompanied by different degrees of tectonic uplift after hydrocarbon generation. Besides Lishuwo formation and Anyuan formation, the sealing ability of roof and floor is relatively low, Piyuancun formation, Wangyingpu Group, Guanyintang Group, Hetang Group, Leping Group, etc, have good self-sealing property in the study area, except that Lishuwo formation and Anyuan formation are relatively low. Xiaojiang edge group all have better conditions of top and floor sealing. The faults of Xiu Wufu syncline, Jiurui complex syncline, northern syncline, central syncline and eastern Pingle depression are less developed in this area, and the preservation conditions are better. Based on the relationship between burial and hydrocarbon generation and considering the preservation conditions, this paper summarizes the shale gas enrichment model in Jiangxi Province, and considers that the shale gas rich integrated reservoir has experienced the source-cap sedimentary period and the initial enrichment period. There are four stages of continuous enrichment period (volatile enrichment period) and preservation stereotype period, which are mainly controlled by preservation pattern period. The favorable areas for preservation and enrichment in the province are divided into 5 types, and nine enrichment favorable areas, such as Xiu Wu complex syncline, Jiurui complex syncline and central one, are selected in the whole province.
【學(xué)位授予單位】:中國(guó)礦業(yè)大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2015
【分類(lèi)號(hào)】:P618.13
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