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碳酸盐岩风化壳储层特征与成因:以鄂尔多斯盆地高桥地区奥陶系马家沟组马5段为例

Characteristics and Genesis of Carbonate Weathering Crust Reservoirs: A Case from the Ma5Member of Ordovician in Gaoqiao Area, Ordos Basin, China.

作者信息

Ren Qiang, Sun Zhen, Wang Hu, Wan Cixuan, Li Tian, Li Qihui, Yan Zhen

机构信息

School of Geology Engineering and Geomatics, Chang'an University, Xi'an 710054, China.

The Sixth Gas Production Plant, PetroChina Changqing Oilfield Company, Xi'an, Shaanxi 710018, China.

出版信息

ACS Omega. 2024 Jul 31;9(32):34329-34338. doi: 10.1021/acsomega.4c00292. eCollection 2024 Aug 13.

DOI:10.1021/acsomega.4c00292
PMID:39157125
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11325425/
Abstract

The hydrocarbon reserves in carbonate rocks account for about half of the global hydrocarbon reserves and are an important reservoir type. The Ordovician Majiagou Formation in the central Ordos Basin is a representative weathering crust reservoir. The Caledonian movement uplifted the stratum as a whole, and subsequently, 120 million years of exposed weathering, denudation, and leaching created this unique karst paleomorphology. Dolomite reservoirs have developed dissolved pores and microfractures, which are the best reserved spaces for natural gas and good hydrocarbon migration channels. This paper takes the Ma5Member (hereinafter referred to as Ma5) carbonate reservoir in Gaoqiao Gas Field as the research target, based on the core, thin section, cathodoluminescence, logging data, etc., and systematically study the effect of karstification on the reservoir and the genesis of the dolomite reservoir. The results show that the depositional period of the Ordovician Majiagou strata is a regression cycle and the depositional environment is a limited evaporative tidal flat. The reservoir lithology of Ma5 is mainly gypsiferous dolomite and micrite dolomite. The reservoir space types consist of intergranular pores, gypsum mold pore, intragranular dissolution pores, intercrystalline pores, and microfractures. The porosity has values from 0.3 to 11.2% (mostly less than 5.0%) with an average of 3.3%, and the permeability ranges from 0.003 to 13.2 mD (mostly less than 1 mD) with an average of 0.36 mD. Karstification is divided into three periods, including syngenetic karst, eogenetic karst, and burial karst. The sedimentary microfacies determine the material basis of the reservoir, and multistage karstification finally modifies the physical properties. By deeply exploring the formation mechanism and influencing factors of the carbonate reservoir in the Ordovician Majiagou Formation, it provides an important theoretical basis and practical guidance for oil and gas exploration and development. At the same time, it also has important reference value for understanding and predicting the development law and distribution characteristics of carbonate reservoirs under similar geological background.

摘要

碳酸盐岩中的油气储量约占全球油气储量的一半,是一种重要的储层类型。鄂尔多斯盆地中部的奥陶系马家沟组是典型的风化壳储层。加里东运动使地层整体抬升,随后历经1.2亿年的暴露风化、剥蚀和淋滤,形成了这种独特的岩溶古地貌。白云岩储层发育了溶蚀孔隙和微裂缝,是天然气最佳的储集空间和良好的油气运移通道。本文以高桥气田马五段(以下简称马5)碳酸盐岩储层为研究对象,基于岩心、薄片、阴极发光、测井资料等,系统研究了岩溶作用对储层的影响及白云岩储层的成因。研究结果表明,奥陶系马家沟地层沉积期为一个海退旋回,沉积环境为局限蒸发潮坪。马5储层岩性主要为含膏白云岩和微晶白云岩。储集空间类型有粒间孔隙、膏模孔隙、粒内溶孔、晶间孔隙和微裂缝。孔隙度为0.3%~11.2%(多数小于5.0%),平均为3.3%;渗透率为0.003~13.2 mD(多数小于1 mD),平均为0.36 mD。岩溶作用分为同生岩溶、表生岩溶和埋藏岩溶三个阶段。沉积微相决定了储层的物质基础,多期岩溶作用最终改造了储层物性。深入探究奥陶系马家沟组碳酸盐岩储层的形成机制及影响因素,为油气勘探开发提供了重要的理论依据和实践指导。同时,对于认识和预测相似地质背景下碳酸盐岩储层的发育规律及分布特征也具有重要的参考价值。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/13a6/11325425/14d0c6b947e9/ao4c00292_0010.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/13a6/11325425/b8093751d9e2/ao4c00292_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/13a6/11325425/ef197c6a8221/ao4c00292_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/13a6/11325425/5363faface16/ao4c00292_0007.jpg
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