引文
[1]魏国齐,刘德来,张林,等.四川盆地天然气分布规律与有利勘探领域[J].天然气地球科学,2005,16(4):437-442.Wei Guoqi,Liu Delai,Zhang Lin,et al.The exploration region andnatural gas accumulation in Sichuan Basin[J].Natural Gas Geoscience,2005,16(4):437-442.
[2]李智武,刘树根,陈洪德,等.川西坳陷复合-联合构造及其对油气的控制[J].石油勘探与开发,2011,38(5):538-551.Li Zhiwu,Liu Shugen,Chen Hongde,et al.Structuralsuperimposition and conjunction and its effects on hydrocarbonaccumulation in the Western Sichuan Depression[J].PetroleumExploration and Development,2011,38(5):538-551.
[3]张光荣,徐世琦,蒋小光,等.乐山—龙女寺古隆起区含气有利区带评价[J].天然气工业,2008,28(增刊A):19-21.Zhang Guangrong,Xu Shiqi,Jiang Xiaoguang,et al.Evaluation offavorable area of bearing gas in Leshan-Longnüsi Palaeouplift[J].Natural Gas Industry,2008,28(Supp.A):19-21.
[4]宋文海.乐山—龙女寺古隆起大中型气田成藏条件研究[J].天然气工业,1996,16(增刊):16-26.Song Wenhai.Research on reservoir-formed conditions oflarge-medium gas fields of Leshan-Longnüsi Palaeouplift[J].NaturalGas Industry,1996,16(Supp.):16-26.
[5]李伟,余华琪,邓鸿斌.四川盆地中南部寒武系地层划分对比与沉积演化特征[J].石油勘探与开发,2012,39(6):681-690.Li Wei,Yu Huaqi,Deng Hongbin.Stratigraphic division andcorrelation and sedimentary characteristics of the Cambrian incentral-southern Sichuan Basin[J].Petroleum Exploration andDevelopment,2012,39(6):681-690.
[6]李国辉,李翔,杨西南.四川盆地加里东古隆起震旦系气藏成藏控制因素[J].石油与天然气地质,2000,21(1):80-82.Li Guohui,Li Xiang,Yang Xi’nan.Controlling factors of Sinian gaspools in Caledonian Paleouplift,Sichuan Basin[J].Oil&GasGeology,2000,21(1):80-82.
[7]黄金亮,邹才能,李建忠,等.川南下寒武统筇竹寺组页岩气形成条件及资源潜力[J].石油勘探与开发,2012,39(1):69-75.Huang Jinliang,Zou Caineng,Li Jianzhong,et al.Shale gasgeneration and potential of the Lower Cambrian QiongzhusiFormation in Southern Sichuan Basin,China[J].PetroleumExploration and Development,2012,39(1):69-75.
[8]邓涛.四川盆地加里东古隆起的构造机制和成藏模式[J].石油实验地质,1996,18(4):356-360.Deng Tao.Tectonic mechanism and pooling model of the CaledonianPaleoswell in Sichuan Basin[J].Experimental Petroleum Geology,1996,18(4):356-360.
[9]魏国齐,焦贵浩,杨威,等.四川盆地震旦系—下古生界天然气成藏条件与勘探前景[J].天然气工业,2010,30(12):5-9.Wei Guoqi,Jiao Guihao,Yang Wei,et al.Hydrocarbon poolingconditions and exploration potential of Sinian-Lower Paleozoic gasreservoirs in the Sichuan Basin[J].Natural Gas Industry,2010,30(12):5-9.
[10]计德华,岳宏.川西南震旦系油气勘探前景的探讨[J].天然气工业,1986,6(1):10-14.Ji Dehua,Yue Hong.A discussion on oil and exploration prospects ofSinian in Southwest Sichuan[J].Natural Gas Industry,1986,6(1):10-14.
[11]徐永昌,沈平,李玉成.中国最古老的气藏:四川威远震旦纪气藏[J].沉积学报,1989,7(4):3-12.Xu Yongchang,Shen Ping,Li Yucheng.The oldest gas pool of China:Weiyuan Sinian gas pool,Sichuan Province[J].Acta SedimentologicaSinica,1989,7(4):3-12.
[12]许海龙,魏国齐,贾承造,等.乐山—龙女寺古隆起构造演化及对震旦系成藏的控制[J].石油勘探与开发,2012,39(4):406-416.Xu Hailong,Wei Guoqi,Jia Chengzao,et al.Tectonic evolution of theLeshan-Longnüsi paleo-uplift and its control on gas accumulation in theSinian strata,Sichuan Basin[J].Petroleum Exploration andDevelopment,2012,39(4):406-416.
[13]陈宗清.四川盆地震旦系灯影组天然气勘探[J].中国石油勘探,2010,13(4):1-14.Chen Zongqing.Gas exploration in Sinian Dengying Formation,Sichuan Basin[J].China Petroleum Exploration,2010,13(4):1-14.
[14]邱蕴玉,徐濂,黄华梁.威远气田成藏模式初探[J].天然气工业,1994,14(1):9-13.Qiu Yunyu,Xu Lian,Huang Hualiang.Preliminary discussion onpool-formed patterns in Weiyuan Gas Field[J].Natural Gas Industry,1994,14(1):9-13.
[15]戴金星.威远气田成藏期及气源[J].石油实验地质,2003,25(5):473-479.Dai Jinxing.Pool-forming periods and gas sources of Weiyuan GasField[J].Experimental Petroleum Geology,2003,25(5):473-479.
[16]张声瑜,唐创基.四川盆地灯影组区域地质条件及含气远景[J].天然气工业,1986,6(1):3-9.Zhang Shengyu,Tang Chuangji.Regional geology conditions ofDengying Formation(Sinian)in Sichuan Basin and its gasprospects[J].Natural Gas Industry,1986,6(1):3-9.
[17]尹长河,王廷栋,王顺玉,等.威远、资阳震旦系干酪根与油裂解气的鉴别[J].沉积学报,2001,19(1):156-160.Yin Changhe,Wang Tingdong,Wang Shunyu,et al.Differences betweenKerogen and oil-cracked gases in Sinian reservoirs of Weiyuan andZiyang area[J].Acta Sedimentologica Sinica,2001,19(1):156-160.
[18]陈文正.再论四川盆地威远震旦系气藏的气源[J].天然气工业,1992,12(6):28-32.Chen Wenzheng.Discussing again on the source of Sinian gas poolin Weiyuan area in Sichuan Basin[J].Natural Gas Industry,1992,12(6):28-32.
[19]黄籍中,陈盛吉.四川盆地震旦系气藏形成的烃源地化条件分析:以威远气田为例[J].天然气地球科学,1993,4(4):16-20.Huang Jizhong,Chen Shengji.The source geochemical conditions ofSinian in Sichuan Basin:Take Weiyuan Gas Field as an example[J].Natural Gas Geoscience,1993,4(4):16-20.
[20]徐世琦,张光荣,李国辉,等.加里东古隆起震旦系的烃源条件[J].成都理工学院学报,2000,27(增刊):131-138.Xu Shiqi,Zhang Guangrong,Li Guohui,et al.The hydrocarbonsource condition of Sinian system of the Caledonian palaeo-uplift[J].Journal of Chengdu University of Technology,2000,27(Supp.):131-138.
[21]秦建中,刘宝泉.海相不同类型烃源岩生排烃模式研究[J].石油实验地质,2005,27(1):74-80.Qin Jianzhong,Liu Baoquan.Models of hydrocarbon generation andexploration and expulsion from various marine source rock[J].Experimental Petroleum Geology,2005,27(1):74-80.
[22]陈明,许效松,万方,等.上扬子台地晚震旦世灯影组中葡萄状-雪花状白云岩的成因意义[J].矿物岩石,2002,22(4):33-37.Chen Ming,Xu Xiaosong,Wan Fang,et al.Genesis and significanceof grape-and snowflake-shaped dolomite from Dengying Formationof upper Sinian in upper Yangtze platform region[J].Journal ofMineralogy and Petrology,2002,22(4):33-37.