中国西北部鄂尔多斯盆地石炭系本溪地层煤岩气地质特征及勘探突破

IF 7 Q1 ENERGY & FUELS
Zhe ZHAO , Wanglin XU , Zhenyu ZHAO , Shiwei YI , Wei YANG , Yueqiao ZHANG , Yuanshi SUN , Weibo ZHAO , Yunhe SHI , Chunlin ZHANG , Jianrong GAO
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引用次数: 0

摘要

为探索鄂尔多斯盆地石炭系本溪地层煤岩气的地质特征和勘探潜力,本文对鄂尔多斯盆地煤岩分布、煤岩储层、煤岩质量以及煤岩气特征、资源量和富集程度进行了系统研究。煤岩气是一种有别于煤层气的优质资源,在埋藏深度、气源、储层、含气量、碳同位素组成等方面具有独特的特征。本溪地层煤岩面积 16×104 平方公里,厚度 2 米至 25 米不等,主要由明亮和半明亮煤组成,结构原始,挥发分和灰分含量低,煤质较好。中高级煤岩的总有机碳(TOC)含量在 33.49% 至 86.11% 之间,平均为 75.16%。它们具有较高的热演化程度(Ro 为 1.2%-2.8%)和较高的瓦斯生成能力。它们还具有较高的稳定碳同位素值(δ13C1 为-37.6‰至-16‰;δ13C2 为-21.7‰至-14.3‰)。深部煤岩发育有基质孔隙,如气泡孔隙、有机孔隙和无机矿物孔隙,这些孔隙与裂隙和断裂共同构成良好的储层空间。煤岩储层的孔隙度为 0.54%-10.67%(平均为 5.42%),渗透率为 (0.001-14.600)×10-3 μm2(平均为 2.32×10-3 μm2)。纵向上有五种煤岩瓦斯积聚消散组合,其中以煤岩-泥岩瓦斯积聚组合和煤岩-石灰岩瓦斯积聚组合最为重要,封孔条件好,瓦斯测井总烃峰值高。构建了煤岩瓦斯积聚模型,包括广泛分布的持续产气的中高等级煤岩、作为大型储层空间的基质孔隙和煤岩裂隙/断裂、提供密封性的致密盖岩、源储一体化以及五种高效富集模式(侧向挤压复合、透镜状、低振幅构造、鼻状构造和岩性自密封)。根据煤岩气的地质特征,将本溪地层划分为 8 个演替,估算埋深大于 2 000 米的煤岩气资源量大于 12.33×1012 立方米。在上述认识的指导下,部署了风险勘探工作。据此钻探的两口井获得了工业气流,推动了探井和评价井的进一步部署。取得了可能储量过万亿立方米、探明储量过千亿立方米的实质性突破,对我国天然气增储和高效开发具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological characteristics and exploration breakthroughs of coal rock gas in Carboniferous Benxi Formation, Ordos Basin, NW China

To explore the geological characteristics and exploration potential of the Carboniferous Benxi Formation coal rock gas in the Ordos Basin, this paper presents a systematic research on the coal rock distribution, coal rock reservoirs, coal rock quality, and coal rock gas features, resources and enrichment. Coal rock gas is a high-quality resource distinct from coalbed methane, and it has unique features in terms of burial depth, gas source, reservoir, gas content, and carbon isotopic composition. The Benxi Formation coal rocks cover an area of 16×104 km², with thicknesses ranging from 2 m to 25 m, primarily consisting of bright and semi-bright coals with primitive structures and low volatile and ash contents, indicating a good coal quality. The medium-to-high rank coal rocks have the total organic carbon (TOC) content ranging from 33.49% to 86.11%, averaging 75.16%. They have a high degree of thermal evolution (Ro of 1.2%–2.8%), and a high gas-generating capacity. They also have high stable carbon isotopic values (δ13C1 of –37.6‰ to –16‰; δ13C2 of –21.7‰ to –14.3‰). Deep coal rocks develop matrix pores such as gas bubble pores, organic pores, and inorganic mineral pores, which, together with cleats and fractures, form good reservoir spaces. The coal rock reservoirs exhibit the porosity of 0.54%–10.67% (averaging 5.42%) and the permeability of (0.001–14.600)×10−3 μm2 (averaging 2.32×10−3 μm2). Vertically, there are five types of coal rock gas accumulation and dissipation combinations, among which the coal rock-mudstone gas accumulation combination and the coal rock-limestone gas accumulation combination are the most important, with good sealing conditions and high peak values of total hydrocarbon in gas logging. A model of coal rock gas accumulation has been constructed, which includes widespread distribution of medium-to-high rank coal rocks continually generating gas, matrix pores and cleats/fractures in coal rocks acting as large-scale reservoir spaces, tight cap rocks providing sealing, source-reservoir integration, and five types of efficient enrichment patterns (lateral pinchout complex, lenses, low-amplitude structures, nose-like structures, and lithologically self-sealing). According to the geological characteristics of coal rock gas, the Benxi Formation is divided into 8 plays, and the estimated coal rock gas resources with a buried depth of more than 2 000 m are more than 12.33×1012 m3. The above understandings guide the deployment of risk exploration. Two wells drilled accordingly obtained an industrial gas flow, driving the further deployment of exploratory and appraisal wells. Substantial breakthroughs have been achieved, with the possible reserves over a trillion cubic meters and the proved reserves over a hundred billion cubic meters, which is of great significance for the reserves increase and efficient development of natural gas in China.

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