岩性油气藏 ›› 2021, Vol. 33 ›› Issue (6): 114123.doi: 10.12108/yxyqc.20210612
潘宾锋1, 高月泉1, 潘涛1, 李宗贤2, 王志伟1, 邱文波1, 封蓉1
PAN Binfeng1, GAO Yuequan1, PAN Tao1, LI Zongxian2, WANG Zhiwei1, QIU Wenbo1, FENG Rong1
摘要: 为研究银额盆地拐子湖凹陷北部地区烃源岩特征,评价其生烃潜力,开展了探井全井段泥岩的地球化学测试,以探讨北部与中部烃源岩差异性成因,评价研究区油气成藏的油源条件。结果表明:①拐子湖凹陷北部潜在烃源岩主要发育于白垩系苏红图组、巴音戈壁组三段和巴音戈壁组二段,泥岩的有机质丰度普遍较低,但局部井段存在“甜点”,有机质类型以Ⅲ型为主,烃源岩达到成熟—过成熟热演化阶段。②相比于中部,北部源岩条件明显变差,可能受控于边界断层活动和凹陷结构的差异性引起的烃源岩在形成环境与母源输入方面的差异。③研究区有效烃源岩下限为w(TOC)大于1.35%,区内W1井—W2井区有效烃源岩面积较大,厚度大于20 m的烃源岩面积约133 km2,W2井含气层和储层沥青的发现表明研究区烃源岩具有一定的生烃潜力,且有过油气成藏史。该研究成果可为拐子湖凹陷下一步勘探决策提供依据。
中图分类号:
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