基于岩性相单元的低孔低渗碎屑岩储层质量精细评价——以珠江口盆地HZ25-7构造古近系文昌组为例

作    者:杨玉卿1,崔维平1,冯进2,张伟1
单    位:(1中海油田服务股份有限公司; 2中海石油(中国)有限公司深圳分公司)
基金项目:中国海洋石油总公司“十二五”重大科技项目“中国近海低孔低渗油气藏勘探开发关键技术与实践”研究成果
摘    要:
针对深层系储层勘探评价中遇到的岩性复杂、物性变化大的难题,以珠江口盆地HZ25-7构造古近系文昌组低孔低渗储层为例,利用电成像测井纵向分层的高分辨率优势,在宏观岩性识别和沉积层理构造解释的基础上,以微尺度的岩性相为单元,共划分出14种岩性相类型,分析了目的层段2种河道单元内部的岩性相组合序列,揭示了储层纵向上的非均质性特征。根据岩心物性分析并刻度常规测井和电成像测井,对各类岩性相单元开展物性评价。结果表明,在相同的成岩作用背景下,粒度和沉积层理构造对物性有明显控制作用:随着粒度由粗变细,层理构造由槽状交错层理、板状交错层理到块状层理,储层物性逐渐变差。在文昌组寻找优质储层,应以河道单元中上部岩性较粗且交错层理发育的高能沉积岩性相单元为主要目标。
关键词:珠江口盆地;古近系;碎屑岩;岩性相;低孔低渗储层;层理构造;储层评价

Evaluation of the Clastic Reservoir with Low-porosity and Low-permeability Based on Lithofacies Unit: A Case of Paleogene Wenchang Formation in Structure HZ25-7, Zhujiangkou Basin

Author's Name: Yang Yuqing, Cui Weiping, Feng Jin, Zhang Wei
Institution: China Oilfield Services Limited
Abstract:
The clastic rocks buried deeply are complex and heterogeneous, especially for the low-porosity and low-permeability rocks, and how to find and characterize the relatively high quality parts of the reservoir is worth exploring. In our case the drilling core is relatively limited, so the electrical image logging with a high resolution of longitudinal layering becomes valuable. In the study of the Paleogene Wenchang Formation reservoir in Structure HZ25-7, Zhujiangkou Basin, 14 types of lithofacies were divided by identification of lithology, grain size and bedding structure according to cores and resistivity images. And 6 lithofacies sequences were described in the two types of channel units, including branch channel of delta-plain and distributary channel of delta-front, which revealing the vertical heterogeneity of reservoir. According to the porosity and permeability of core samples, together with the conventional logging and electrical image logging calibrated by the core, the reservoir can be effctively evaluated on lithofacies units. In the same diagenetic background, particle size and bedding have obvious control effect on reservoir properties. From coarse to fine, the reservoir properties gradually deteriorated; from trough-like interlaced bedding to plate-like interlaced bedding, and then to massive bedding, the reservoir properties gradually get worse. The favorable lithologicfacies in Wenchang Formation developed in the upper part of the river unit with coarse particle and staggered bedding.
Keywords: Clastic rock; Lithofacies(Lithologic facies); Bedding structure; Low porosity-low permeability reservoir; Reservoir evaluation; Paleogene; Zhujiangkou Basin
投稿时间: 2016-06-12  
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