岩性油气藏 ›› 2015, Vol. 27 ›› Issue (3): 8286.doi: 10.3969/j.issn.1673-8926.2015.03.012
马庆佑,田 鹏,吕海涛,沙旭光
MA Qingyou, TIAN Peng, LU Haitao, SHA Xuguang
摘要:
塔里木盆地古城墟隆起 GL3 井在鹰山组发现了大量固体沥青,其主要赋存于泥晶砂屑灰岩及云质灰岩的溶孔和裂缝中。通过岩心观察、显微照片和沥青反射率(Rb)等分析,发现沥青边界较清晰,不溶于有机溶剂氯仿,无荧光显示,Rb 为 2.76%~2.85%,与焦沥青的基本特征相似,表现为古油藏裂解的残迹。 GL3 井鹰山组沥青的发现具有两大地质意义:①沥青发育段与围岩波阻抗的差异可能是 GL3 井鹰山组“串珠状”地震强反射形成的主要原因,会造成对该井储层预测的偏差;②根据包裹体测温,沥青和天然气成因、埋藏史及生烃史分析,恢复 GL3 井古油藏的成藏过程,其大致可分为加里东中—晚期古油藏形成与喜马拉雅晚期古油藏裂解成气并转变为焦沥青残迹的两大过程。该研究这对深化古城墟隆起成藏过程研究具有一定意义。
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