柴西地区新构造运动特征及其对成藏影响
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
柴达木盆地喜马拉雅晚期以来的新构造运动活跃,对油气藏形成起了关键作用。以露头调查、地震剖面地质构造解释和油藏解剖资料为基础,结合前人已有研究成果,对柴西地区新构造运动特征及其成藏作用开展研究。新构造运动在现今地貌上表现为狮子沟组区域性不整合和北西西走向的地面构造特征。新构造运动期间断裂表现为深大断裂的再活动和新断裂的形成,并形成反冲构造、断展背斜、纵弯背斜和滑脱褶皱4种构造样式。新构造运动促进了圈闭的形成,并且是油气充注和油气成藏的关键期。新构造运动作用下,构造圈闭形成期与油气充注期匹配越好,越有利于油气成藏;断裂对构造圈闭的破坏作用越小,越有利于油气成藏。
Since the late Himalayan Movement,neotectonic movements have been active and have played important roles on petroleum accumulation in the western Qaidam Basin.Based on the studies of outcrops,seismic profile geological tectonic interpretations and oil reservoir anatomies,combined with the previous research results,the features of neotectonic movements and their controlling effects on petroleum accumulations were discussed.The neotectonic movements resulted in the present regional unconformities in the Shizigou Formation and the NWW-oriented modern landscapes.During the neotectonic movements,deep faults activated again while new faults came into being,and 4 kinds of structural pattern were formed,including back thrust fault,propagation anticline,longitudinal bend anticline and detachment fold.The neotectonic movements promoted the formation of traps,and had controlling effects on petroleum charging and accumulations.Influenced by the neotectonic movements,the good matching of tectonic trap formation and petroleum charging as well as the weak destruction of fault on tectonic trap are favorable for petroleum accumulation.
引文
[1]郭旭东.北京第四纪地质导论[M].重庆:重庆出版集团,2007.
    [2]丁国瑜.新构造研究的几点回顾:纪念黄汲清先生诞辰100周年[J].地质论评,2004,50(3):252-255.
    [3]李祥根.中国新构造运动概论[M].北京:地震出版社,2003.
    [4]朱允铸,钟坚华,李文生.柴达木盆地新构造运动及盐湖发展演化[M].北京:地质出版社,1994.
    [5]郭占谦,师继红.新构造运动活跃的柴达木盆地含油气系统特征[J].大庆石油地质与开发,2001,20(1):9-12.
    [6]吴光大.柴达木盆地构造特征及其对油气分布的控制[D].长春:吉林大学,2007.
    [7]党玉琪,尹成明,赵东胜.柴达木盆地西部地区古近纪与新近纪沉积相[J].古地理学报,2004,6(3):297-306.
    [8]刘震,党玉琪,李鹤永,等.柴达木盆地西部第三系油气晚期成藏特征[J].西安石油大学学报:自然科学版,2007,22(1):1-6.
    [9]肖飞,包建平,朱翠山,等.柴达木盆地西部典型油田原油地球化学特征对比[J].地球科学与环境学报,2012,34(4):43-52.
    [10]李春昱,王荃,刘雪亚,等.亚洲大地构造图及说明书[M].北京:地图出版社,1982.
    [11]李兰斌,孙家振,夏晓燕,等.柴达木盆地西南地区褶皱构造样式[J].石油实验地质,2012,34(1):30-35.
    [12]陈袁,牟中海,马达德,等.柴达木盆地西部地区盆山接触关系研究[J].断块油气田,2012,19(4):414-417.
    [13]吕宝凤,张越青,杨书逸.柴达木盆地构造体系特征及其成盆动力学意义[J].地质论评,2011,57(2):167-173.
    [14]罗群.柴达木盆地成因类型探讨[J].石油实验地质,2008,30(2):114-120.
    [15]金之钧,张明利,汤良杰,等.柴达木中新生代盆地演化及其控油气作用[J].石油与天然气地质,2004,25(6):603-608.
    [16]杨明慧.柴达木盆地新构造运动主要特征与成因机制[J].海洋地质与第四纪地质,1997,17(3):71-78.
    [17]陈启林.大型咸化湖盆地层岩性油气藏有利条件与勘探方向:以柴达木盆地柴西南古近纪为例[J].岩性油气藏,2007,19(1):46-51.
    [18]罗群,庞雄奇.柴达木盆地断裂特征与油气区带成藏规律[J].西南石油学院学报,2003,25(1):1-5.
    [19]戴俊生,曹代勇.柴达木盆地构造样式的类型和展布[J].西北地质科学,2000,21(2):57-62.
    [20]余一欣,汤良杰,马达德,等.柴达木盆地构造圈闭特征与含油气性[J].西安石油大学学报:自然科学版,2006,21(5):1-5.
    [21]党玉琪,熊继辉,刘震,等.柴达木盆地油气成藏的主控因素[J].石油与天然气地质,2004,25(6):614-619.

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