岩性油气藏 ›› 2017, Vol. 29 ›› Issue (3): 7682.doi: 10.3969/j.issn.1673-8926.2017.03.009
程飞
CHENG Fei
摘要: 塔里木盆地奥陶系碳酸盐岩储层非均质性和各向异性极强,成因机理复杂,不同成因、机理及尺度的孔、洞、缝常伴生发育,单一的静态方法(钻井、岩心、测井和地震等)探测范围较小及精度不够准确,难以精细划分储层类型。在以动窥静,动静结合的思路下,深入剖析了145口井的动静态资料及其在不同储层类型中的响应特征,最终确定以试井渗透率、井储系数、井控半径、酸压停泵压力、累积产液压降曲线、钻井放空漏失、地震反射特征和测井曲线为主体,建立碳酸盐岩油藏储层类型识别模板,并划分出3种储层类型,即洞穴+裂缝孔洞型、洞穴型和裂缝-孔洞型。该方法克服了以往依靠单因素识别储层类型的局限性,拓展了动静态方法结合的研究思路,为碳酸盐岩油藏储层类型的识别提供了依据。
中图分类号:
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