塔里木盆地主要古隆起的形成、演化及控油气地质条件分析
|
摘要
古隆起的分布及其形成演化对油气的聚集具有决定作用。综合利用地震、测井和分析测试资料,对塔里木盆地不同地质时期的古隆起分布及其演化进行了分析,对塔中、塔北和巴楚3个古隆起的性质、演化特征及油气成藏地质条件进行了对比,指出油气关键成藏期的古隆起及其后期的发展演化影响着盆地的地质结构,制约着油气的聚集与分布,认为由此决定的不同时期的成藏主控因素和油气聚集区显著不同,例如加里东运动晚期,塔北隆起和塔中隆起是油气聚集的有利区;海西运动晚期,塔北隆起、巴楚隆起、塔中隆起和塔东隆起及其斜坡带是油气的有利聚集区;喜马拉雅运动期,巴楚隆起及其围斜部位则是主要的油气勘探有利区,塔东地区也值得重视。
The distribution, formation and evolution of paleohighs play a decisive role for hydrocarbon accumulation. Based on the seismic, log and test data, this paper systemically studies the distribution and evolution of different geological paleohighs in Tarim Basin. Through the comprehensive comparison of the properties and evolutional characteristics and hydrocarbon geological conditions of three paleohighs (Tazhong, Tabei and Bachu), it analyzes the favorable exploration domains during different periods, and indicates that the paleohigh in the crucial hydrocarbon-accumulation period and its later evolution impact on the basin's geological structure and restrict the hydrocarbon accumulation and distribution. These lead to different main controlling factors of hydrocarbons and different hydrocarbon accumulation zones in different periods. Tabei and Tazhong are the favorable accumulation areas in the late Caledonian period. These highs and their slopes of Tabei, Bachu, Tazhong, Tadong are the favorable accumulation areas in the late Hercynian period. In the Himalayan period, Bachu high and its ramp are the main favorable areas for exploration, and Tadong also deserves attention.
The distribution, formation and evolution of paleohighs play a decisive role for hydrocarbon accumulation. Based on the seismic, log and test data, this paper systemically studies the distribution and evolution of different geological paleohighs in Tarim Basin. Through the comprehensive comparison of the properties and evolutional characteristics and hydrocarbon geological conditions of three paleohighs (Tazhong, Tabei and Bachu), it analyzes the favorable exploration domains during different periods, and indicates that the paleohigh in the crucial hydrocarbon-accumulation period and its later evolution impact on the basin's geological structure and restrict the hydrocarbon accumulation and distribution. These lead to different main controlling factors of hydrocarbons and different hydrocarbon accumulation zones in different periods. Tabei and Tazhong are the favorable accumulation areas in the late Caledonian period. These highs and their slopes of Tabei, Bachu, Tazhong, Tadong are the favorable accumulation areas in the late Hercynian period. In the Himalayan period, Bachu high and its ramp are the main favorable areas for exploration, and Tadong also deserves attention.
引文
[1]康玉柱.塔里木盆地油气藏(田)特征[J].石油实验地质,2000,22(2):115-120.
[2]尚雅珍,王保才,解晨,等.塔中地区油气运聚特征[J].海相油气地质,2004,9(1/2):97-104.
[3]肖香娇,唐明龙.塔里木盆地将成为我国陆上最大的产气区[J].天然气地球科学,2003,14(1):35-39.
[4]戴金星.加强天然气地学研究勘探更多大气田[J].天然气地球科学,2003,14(1):3-14.
[5]刘朝露,贾承造,夏斌,等.塔东地区盆山耦合与油气成藏模式研究[J].天然气地球科学,2005,16(5):552-558.
[6]张宗命,贾承造.塔里木克拉通盆地内古隆起及其找油气方向[J].西安石油学院学报,1997,12(3):8-13,42.
[7]贾承造.塔里木盆地构造特征与油气聚集规律[J].新疆石油地质,1999,20(3):177-183.
[8]何登发,李德生.塔里木盆地构造演化与油气聚集[M].北京:地质出版社,1996:92-107.
[9]周新源,王清华,杨文静,等.塔里木盆地天然气资源及勘探方向[J].天然气地球科学,2005,16(1):7-11.
[10]徐国强,刘树根,李国蓉,等.塔中、塔北古隆起形成演化及油气地质条件对比[J].石油与天然气地质,2005,26(1):114-119,129.
[2]尚雅珍,王保才,解晨,等.塔中地区油气运聚特征[J].海相油气地质,2004,9(1/2):97-104.
[3]肖香娇,唐明龙.塔里木盆地将成为我国陆上最大的产气区[J].天然气地球科学,2003,14(1):35-39.
[4]戴金星.加强天然气地学研究勘探更多大气田[J].天然气地球科学,2003,14(1):3-14.
[5]刘朝露,贾承造,夏斌,等.塔东地区盆山耦合与油气成藏模式研究[J].天然气地球科学,2005,16(5):552-558.
[6]张宗命,贾承造.塔里木克拉通盆地内古隆起及其找油气方向[J].西安石油学院学报,1997,12(3):8-13,42.
[7]贾承造.塔里木盆地构造特征与油气聚集规律[J].新疆石油地质,1999,20(3):177-183.
[8]何登发,李德生.塔里木盆地构造演化与油气聚集[M].北京:地质出版社,1996:92-107.
[9]周新源,王清华,杨文静,等.塔里木盆地天然气资源及勘探方向[J].天然气地球科学,2005,16(1):7-11.
[10]徐国强,刘树根,李国蓉,等.塔中、塔北古隆起形成演化及油气地质条件对比[J].石油与天然气地质,2005,26(1):114-119,129.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心