摘 要:烏爾遜凹陷斷裂的形成具有較明顯的分期特征,通過分析構造層序界面、生長指數、斷層活動速率以及伸展率等,得出本區斷裂的形成演化先后經歷了早期伸展、中期走滑和晚期反轉三個階段;結合各變形時期的主要斷裂對油氣成藏的影響,認為伸展斷陷期的主要控陷斷裂控制了烴源巖的分布;主干控陷斷層是油氣運移的主要通道;伊敏組沉積末期形成的南北向斷裂與長期發育的北東東向油源斷裂近正交組合,在大磨拐河組和伊敏組形成大量的圈閉,是油富集的主要區帶。
關鍵詞:烏爾遜凹陷 斷裂演化 油源斷層 油氣藏
中圖分類號:P618.13 文獻標識碼:A 文章編號:1674-098X(2011)03(c)-0138-02
Faults evolution and its impact on hydrocarbon accumulation in Wuerxun depression
ZHANG Ming-xue ZHANG Tian-yao LIU Qiang
(1 Dongbei Petroleum Institute, Daqing 163318, China;
2 Jilin division of Daqing Logging Company of Exploration Drilling Engineering Company Jilin 138000,China);
Abstract:The formation of faults in Wuerxun depression has obvious characters of substage ,by analysising the tectonic sequence boundaries,growth index,faults acting rate and stretch,we considered the evolution of the fault had under gone early extension,middle strile-slip and late reversion three stages. By researching the effection of the main faults formed in different periods on hydrocarbon,we have concluded the main faults which controled the depression controled the distribution of hydrocarbon rock; the main controlling faults was the main hydrocarbon migration channel; faults in the direction of SN formed at the end of Yimin group and long-term development oil source faults which in the direction of NNE perpendicular array, forming a lot of traps in Damoguaihe and Yimin group,was one of the main oil enrichment zones.
Key words:Wuerxun depression;fault evolution;source fault;oil and gas reservoir
海拉爾盆地處在內蒙古自治區呼倫貝爾盟境內,盆地內劃分為三坳兩隆五個一級構造單元,進一步分為16個凹陷、4個凸起共20個二級構造單元。烏爾遜凹陷是海拉爾盆地貝爾湖坳陷的一個二級構造單元,是海拉爾盆地最有潛力的勘探地區之一[1,2]。
烏爾遜凹陷為一南北向展布、西斷東超的箕狀斷陷[3]。該區構造復雜,斷裂十分發育,目前已經發現的油氣藏大部分與斷層密切相關。隨著勘探工作的深入,迫切需要運用新的理論對一些現有的層系進行系統深入細致的研究,深化石油地質特征的認識。因此,本文深入剖析烏爾遜凹陷斷裂構造特征,確定斷裂的發生、發展及其演化過程,進而探討斷裂對油氣成藏的控制作用,以利于斷陷盆地區油氣的進一步勘探?!?br>