塔里木盆地中—新生界构造单元划分
|
摘要
塔里木盆地作为典型的多旋回叠合盆地,中生代以来经历了印支、燕山和喜山等多期构造运动,造成中-新生界构造格局与古生界构造格局差异较大。应用航磁、重力、钻井、测井以及地震等资料,获得了盆地中-新生界地层分布、区域构造变形特点和含油气性特征,兼顾基底形态和后期改造作用影响,对塔里木盆地中-新生界构造单元划分为"三坳一隆一斜坡",即北部坳陷区、西南坳陷区、东南坳陷区、中央隆起区和东北斜坡区5个一级构造单元和11个二级构造单元。显然,该构造单元的划分对盆地中-新生界次生油气藏和隐蔽油气藏勘探具有重要意义。
As a typical multi-superimposed basin,Tarim Basin has undergone Indosinian,Yanshan and Himalayan movements since the Mesozoic,which resulted in the great different structural patterns between the Mesozoic-Cenozoic and the Paleozoic.Based on an integrated analysis of the aeromagnetic,gravity,drilling,logging and seismic data,the Mesozoic-Cenozoic stratigraphic distribution,structural deformation styles and petroliferous features have been obtained.Considering the pre-Mesozoic basement form and late reformation,the Mesozoic-Cenozoic in Tarim Basin can be divided into five structural units,i.e.the north depression,the southwest depression,the southeast depression,the central uplift and the northeast slope,which consists of eleven subunits of structures.Clearly,this division is very significant for the exploration of secondary reservoirs and subtle reservoirs in the Mesozoic-Cenozoic.
As a typical multi-superimposed basin,Tarim Basin has undergone Indosinian,Yanshan and Himalayan movements since the Mesozoic,which resulted in the great different structural patterns between the Mesozoic-Cenozoic and the Paleozoic.Based on an integrated analysis of the aeromagnetic,gravity,drilling,logging and seismic data,the Mesozoic-Cenozoic stratigraphic distribution,structural deformation styles and petroliferous features have been obtained.Considering the pre-Mesozoic basement form and late reformation,the Mesozoic-Cenozoic in Tarim Basin can be divided into five structural units,i.e.the north depression,the southwest depression,the southeast depression,the central uplift and the northeast slope,which consists of eleven subunits of structures.Clearly,this division is very significant for the exploration of secondary reservoirs and subtle reservoirs in the Mesozoic-Cenozoic.
引文
[1]贾承造.塔里木盆地中新生代构造特征与油气[M].北京:石油工业出版社,2004:1-169.
[2]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:自然科学版,1997,12(3):8-13.
[3]王汉生.新疆塔里木盆地构造演化与勘探大油气田的方向[J].新疆地质,1986,4(3):53-64.
[4]康玉柱.试论塔里木盆地油气分布规律及找油方向[J].地球科学:中国地质大学学报,1991,16(4):429-436.
[5]王步清,黄智斌,马培领,等.塔里木盆地构造单元划分标准、依据和原则的建立[J].大地构造与成矿学,2009,33(1):87-93.
[6]何登发,贾承造,李德生.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64-76.
[7]崔军文,唐哲民.塔里木盆地构造格架和构造应力场分析[J].岩石学报,2011,27(1):231-242.
[8]何碧竹,焦存礼,蔡志慧,等.塔里木盆地中部航磁异常带新解译[J].中国地质,2011,38(4):961-969.
[9]许炳如.根据航磁解释的塔里木盆地基岩分布[J].西安石油学院学报,1997,12(6):8-11.
[10]朱传庆,杨书江,李同彬,等.塔里木盆地主要断裂的地球物理特征及与天然地震的关系[J].地球物理学进展,2008,23(6):1685-1691.
[11]Hou Zunze,Yang Wencai.Multi-scale inversion of densitystructure from gravity anomalies in Tarim Basin[J].ScienceChina Earth Sciences,2011,54(3):399-409.
[12]He Dengfa,Li Desheng,Wu Xiaozhi,et al.Basic types andstructural characteristics of uplifts:An overview of sedimenta-ry basins in China[J].Acta Geologica Sinica,2009,83(2):321-346.
[13]张玮,漆家福,雷刚林,等.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,2010,31(6):567-571.
[14]马东华,杨子江.塔里木盆地西南新生代盆地演化特征[J].新疆地质,2003,21(1):92-95.
[15]吕海涛,张仲培,邵志兵,等.塔里木盆地巴楚-麦盖提地区早古生代古隆起的演化及其勘探意义[J].石油与天然气地质,2010,31(1):76-83.
[16]丁文龙,林畅松,漆立新,等.塔里木盆地巴楚隆起构造格架及形成演化[J].地学前缘,2008,15(2):242-251.
[17]李德伦,段吉业,梁桂香,等.英吉苏凹陷中-新生代构造特征及成因机制探讨[J].中国地质,2003,30(2):123-129.
[18]潘正中,郭群英,王步清,等.塔东南地区构造单元划分新方案[J].新疆石油地质,2007,28(6):781-783.
[19]武芳芳,朱光有,张水昌,等.塔里木盆地油气输导体系及对油气成藏的控制作用[J].石油学报,2009,30(3):332-341.
[20]金之钧,云金表,周波,等.塔里木斜坡带类型、特征及其与油气聚集的关系[J].石油与天然气地质,2009,30(2):127-135.
[2]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:自然科学版,1997,12(3):8-13.
[3]王汉生.新疆塔里木盆地构造演化与勘探大油气田的方向[J].新疆地质,1986,4(3):53-64.
[4]康玉柱.试论塔里木盆地油气分布规律及找油方向[J].地球科学:中国地质大学学报,1991,16(4):429-436.
[5]王步清,黄智斌,马培领,等.塔里木盆地构造单元划分标准、依据和原则的建立[J].大地构造与成矿学,2009,33(1):87-93.
[6]何登发,贾承造,李德生.塔里木多旋回叠合盆地的形成与演化[J].石油与天然气地质,2005,26(1):64-76.
[7]崔军文,唐哲民.塔里木盆地构造格架和构造应力场分析[J].岩石学报,2011,27(1):231-242.
[8]何碧竹,焦存礼,蔡志慧,等.塔里木盆地中部航磁异常带新解译[J].中国地质,2011,38(4):961-969.
[9]许炳如.根据航磁解释的塔里木盆地基岩分布[J].西安石油学院学报,1997,12(6):8-11.
[10]朱传庆,杨书江,李同彬,等.塔里木盆地主要断裂的地球物理特征及与天然地震的关系[J].地球物理学进展,2008,23(6):1685-1691.
[11]Hou Zunze,Yang Wencai.Multi-scale inversion of densitystructure from gravity anomalies in Tarim Basin[J].ScienceChina Earth Sciences,2011,54(3):399-409.
[12]He Dengfa,Li Desheng,Wu Xiaozhi,et al.Basic types andstructural characteristics of uplifts:An overview of sedimenta-ry basins in China[J].Acta Geologica Sinica,2009,83(2):321-346.
[13]张玮,漆家福,雷刚林,等.塔西南坳陷西昆仑山前冲断带的收缩构造变形模式[J].新疆石油地质,2010,31(6):567-571.
[14]马东华,杨子江.塔里木盆地西南新生代盆地演化特征[J].新疆地质,2003,21(1):92-95.
[15]吕海涛,张仲培,邵志兵,等.塔里木盆地巴楚-麦盖提地区早古生代古隆起的演化及其勘探意义[J].石油与天然气地质,2010,31(1):76-83.
[16]丁文龙,林畅松,漆立新,等.塔里木盆地巴楚隆起构造格架及形成演化[J].地学前缘,2008,15(2):242-251.
[17]李德伦,段吉业,梁桂香,等.英吉苏凹陷中-新生代构造特征及成因机制探讨[J].中国地质,2003,30(2):123-129.
[18]潘正中,郭群英,王步清,等.塔东南地区构造单元划分新方案[J].新疆石油地质,2007,28(6):781-783.
[19]武芳芳,朱光有,张水昌,等.塔里木盆地油气输导体系及对油气成藏的控制作用[J].石油学报,2009,30(3):332-341.
[20]金之钧,云金表,周波,等.塔里木斜坡带类型、特征及其与油气聚集的关系[J].石油与天然气地质,2009,30(2):127-135.
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