赛汉塔拉凹陷断裂系统及其控藏作用
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摘要
在精细解释地震剖面基础上,详细分析了断裂系统特征,划分了早期伸展、中期张扭和晚期反转等三套断裂系统。断裂生长演化控制生储盖、圈闭、运聚等成藏要素,从而控制成藏作用。
This paper has a detailed discussion on fault system on the basis of careful explanation of seismic profile data of the Saihan Tal depression. The study indicates that oil gas reservoir formation in the depression is controlled by fault system its evolution.
引文
[1]Lezzar K E,Tiercelin J J,Turdu C L,et al.Control of normal fault interaction on the distribution of major Neogene sedimentary depocenters,Lake Tanganyika,East African rift[J].AAPG,2002,86(6):1027-1060.
    [2]漆家福,肖焕钦,张卫刚.东营凹陷主干边界断层(带)构造几何学、运动学特征及成因解释[J].石油勘探与开发,2003,30(3):8~12.
    [3]任纪舜,陈廷愚,牛宝贵.中国东部及邻区大陆岩石圈的构造演化与成矿[M].北京:科学出版社,1990.
    [3]任纪舜,王作勋,陈炳蔚等.从全球看中国大地构造—中国及邻区大地构造图简要说明[M].北京:地质出版社,1999.
    [4]程裕淇.中国区域地质概论[M].北京:地质出版社,1994.
    [5]Li J Y.Permian geodynamic setting of Northeast China and adjacent regions:closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate.Journal of Asian Earth Sciences,2006,26(3-4):207-224.
    [6]闫文华,张万福,张立新,等.二连盆地赛汉塔拉凹陷地质综合评价及目标优选[J].石油地球物理勘探,2008,43(1):139-145.
    [7]屈晓艳,杨明慧,罗晓华,等.二连盆地赛汉塔拉凹陷伸展构造特征及其控藏作用[J].现代地质,2013,27(5):1023-1032.

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