岩性油气藏 ›› 2015, Vol. 27 ›› Issue (5): 196203.doi: 10.3969/j.issn.1673-8926.2015.05.032
刘晓鹏1,2,赵小会1,2,康 锐1,2,漆亚玲1,2
Liu Xiaopeng1,2, Zhao Xiaohui1,2, Kang Rui1,2, Qi Yaling1,2
摘要:
为了明确鄂尔多斯盆地北部二叠系盒 8 段大面积砂体的形成机理,在分析砂体展布特征的基础上,全面恢复了盒 8 期湖盆底形、湖泊与外界的连通性、物源供给及水动力条件等沉积古环境要素,并结合水槽沉积模拟实验,建立了盒 8 段沉积模式。 研究认为:充足的物源供给、较强的水动力、多水系输砂、平缓的湖盆底形、盆地快速稳定的沉降和湖岸线大范围反复波动,是盒 8 段大面积砂体形成的必要条件;鄂尔多斯盆地鄂托克前旗―榆林以南、L63井—S318井—Y101井—Y112 井以北区域,是下一步的有利勘探目标。
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