新疆石油地质
新疆石油地質
신강석유지질
XINJIANG PETROLEUM GEOLOGY
2010年
2期
118-121
,共4页
吴晓智%李佰华%吕修祥%谢会文%刘志刚
吳曉智%李佰華%呂脩祥%謝會文%劉誌剛
오효지%리백화%려수상%사회문%류지강
库车前陆盆地%走滑断裂%构造分段%构造分带%油气聚集
庫車前陸盆地%走滑斷裂%構造分段%構造分帶%油氣聚集
고차전륙분지%주활단렬%구조분단%구조분대%유기취집
Kuqa foreland basin%strike-slip fault%structural segmentation%structural zonation%hydrocarbon accumulation
在塔里木板块与准噶尔板块碰撞而形成的天山造山带中,产生了分别平行和垂直于天山的走滑断裂系.平行于天山的走滑断裂对盆地不同构造带的形成及改造具有重要的作用,而垂直于天山的走滑断裂则造成了库车前陆盆地的构造分段现象.走滑断裂可形成一系列与走滑相关圈闭,为油气提供聚集场所.主干走滑断裂分隔性较好,派生走滑断裂的连通性较好,因此库车前陆盆地的油气主要聚集在派生走滑断裂发育的地区,而主干走滑断裂则使油气性质东、西分段,南、北分带.
在塔裏木闆塊與準噶爾闆塊踫撞而形成的天山造山帶中,產生瞭分彆平行和垂直于天山的走滑斷裂繫.平行于天山的走滑斷裂對盆地不同構造帶的形成及改造具有重要的作用,而垂直于天山的走滑斷裂則造成瞭庫車前陸盆地的構造分段現象.走滑斷裂可形成一繫列與走滑相關圈閉,為油氣提供聚集場所.主榦走滑斷裂分隔性較好,派生走滑斷裂的連通性較好,因此庫車前陸盆地的油氣主要聚集在派生走滑斷裂髮育的地區,而主榦走滑斷裂則使油氣性質東、西分段,南、北分帶.
재탑리목판괴여준갈이판괴팽당이형성적천산조산대중,산생료분별평행화수직우천산적주활단렬계.평행우천산적주활단렬대분지불동구조대적형성급개조구유중요적작용,이수직우천산적주활단렬칙조성료고차전륙분지적구조분단현상.주활단렬가형성일계렬여주활상관권폐,위유기제공취집장소.주간주활단렬분격성교호,파생주활단렬적련통성교호,인차고차전륙분지적유기주요취집재파생주활단렬발육적지구,이주간주활단렬칙사유기성질동、서분단,남、북분대.
In Tianshan orogen formed by collision between Tarim plate and Junggar plate shaped strike-slip fault system vertical and parallel to Tianshan orogen. The strike-slip fault system parallel to it is of an important effect on the formation and reformation of different structural zones in Kuqa foreland basin, while that of vertical to it gives rise to the structural segmentation in it. Strike-slip faults can form a series of related traps which provide sites for hydrocarbon accumulation. The arterial strike-slip faults have good sealing ability to stop hydrocarbon migration from one side to the others, while the derived strike-slip ones have good connectivity. Hence, the hydrocarbons in this basin could mainly accumulate in area with derived strike-slip faults; the arterial strike-slip faults allow the hydrocarbons to distribute by east-west segmentation and south-north zoning.