论四川盆地下三叠统飞仙关组天然气勘探
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摘要
近10余年来,四川盆地东北部下三叠统飞仙关组天然气勘探取得了显著突破,发现了普光、罗家寨、渡口河和铁山等大型气田。天然气主要富集于广梁海槽两侧台地边缘鲕粒滩相区。由于鲕粒滩地势较高,受海盆震荡影响,鲕粒滩经常露出水面遭受淡水淋溶,经混合水白云岩化作用及其后的溶蚀作用,鲕粒滩成片变为鲕粒溶孔白云岩、鲕粒溶孔灰质白云岩或鲕粒溶孔白云质灰岩,平均孔隙度高达8.16%,平均渗透率为93.326×10-3μm2,成为四川盆地最好的储层。气藏多为岩性-构造复合气藏。利用鲕粒滩地震异常识别模式,在盆地东部已发现104个鲕粒滩地震异常,为进一步勘探提供了新的目标。
        Some giant gas fields such as Puguang,Luojiazhai,Dukouhe and Tieshan gas fields have been discovered in Feixianguan Formation of the Lower Triassic in Sichuan Basin in recent decade years.Natural gas mainly accumulated in oolite beach sedimentary facies of carbonate platform edge around Guangliang trough in Sichuan Basin.The topography of oolite beach was high.The oolite beach was often uncovered and subjected to freshwater leaching due to sea basin vibration.The sheets of oolite were changed into the dolomite with dissolved pore of oolite,calcite dolomite with dissolved pore of oolite and dolomitic limestone with dissolved pore of oolite.These rocks in Sichuan Basin are the best reservoirs with the mean porosity of 8.16% and the mean permeability of 93.326×10-3 μ m2.The major gas reservoirs in Sichuan Basin were litho-structural combined reservoirs.There found 104 seismic anomalies of oolite beach in the eastern Sichuan Basin using the recognition mode of seismic anomaly of oolite beach.The new targets for future gas exploration in Sichuan Basin were provided.
引文
[1]中国科学院南京地质古生物研究所.西南地区地层古生物手册[M].北京:科学出版社,1974:226-327.Nanjing Institute of Geology and Palaeontology of Chinese Acade-my of Sciences.A handbook of the stratigraphy and palaeontologyof southwest China[M].Beijing:Science Press,1974:226-327.
    [2]刘宝?.沉积岩石学[M].北京:地质出版社,1980:421-424.Liu Baojun.Sedimentary petrology[M].Beijing:Geological Pub-lishing House,1980:421-424.
    [3]陈宗清.鄂西利川复向斜南部石炭系—三叠系储层与评价[J].海洋石油,2002,114(4):24-31.Chen Zongqing.Reservoirs and estimation of Carboniferous-Trias-sic in Southern Lichuan Synclinorium,West Sichuan Province[J].Offshore Oil,2002,114(4):24-31.
    [4]罗志立.中国西南地区晚古生代以来地裂运动对石油等矿产形成的影响[J].四川地质学报,1981,2(1):1-22.Luo Zhili.Effect of taphrogenesis on various deposits formationsince Late Palaeozoic in southwest China[J].Acta Geologica Si-chuan,1981,2(1):1-22.
    [5]陈宗清.川东石炭系天然气富集因素[J].石油与天然气地质,1983,4(3):310-317.Chen Zongqing.Enriching factors of natural gas in Carboniferous Sys-tem of East Sichuan[J].Oil and Gas Geology,1983,4(3):310-317.
    [6]杜远生,殷鸿福,王治平.秦岭构造带晚加里东—早海西期的盆地格局与构造演化[J].地球科学——中国地质大学学报[J],1997,2(1):1-22.Du Yuansheng,Yin Hongfu,Wang Zhiping.Basin pattern and tec-tonic evolution from Late Caledonian period to Early Hercynionperiod in Qinling tectonic belt[J].Earth Science——Journal ofChina University of Geosciences,1997,2(1):1-22.
    [7]穆曙光,周茂,华永川.川东北地区下三叠统飞仙关组白云岩成因类型[J].天然气工业,1994,14(3):23-27.Mu Shuguang,Zhou Mao,Hua Yongchuan.Dolomite genetic typesin Feixianguan Formation of Lower Triassic Series in northeastarea of Sichuan[J].Natural Gas Industry,1994,14(3):23-27.
    [8]王新建,赵献文.川东飞三段鲕粒灰岩成岩作用与储集特征[J].天然气工业,1986,6(2):28-33.Wang Xinjian,Zhao Xianwen.Diagenesis and reservoir character-istics of the oolitic limestone of Fei-3Member in Eastern Sichuan[J].Natural Gas Industry,1986,6(2):28-33.
    ①王一刚,刘划一,文应初,等.川东上二叠统生物礁气藏形成条件及勘探目标评价研究.四川石油管理局,1998.
    ①王世谦,陈盛吉,张华义,等.四川盆地油气资源评价.四川石油管理局,2002.
    ①王世谦,陈盛吉,张华义,等.四川盆地油气资源评价.四川石油管理局,2002.
    ②王一刚,杨雨,文应初,等.四川盆地东北部长兴组—飞仙关组成藏条件研究及勘探目标评价.四川石油管理局,2000.
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