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煤系气储层孔隙发育特征与成藏潜力——以尼泊尔低喜马拉雅造山带Tansen地区为例
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作者 桑树勋 何俊杰 +5 位作者 韩思杰 kumar khadka 周效志 刘世奇 UPENDRA Baral SAUNAK Bhandari 《油气藏评价与开发》 北大核心 2025年第6期947-958,共12页
煤系气是非常规天然气的重要类型,其成储、成藏是构造沉积作用耦合配置下的结果,尼泊尔低喜马拉雅造山带是研究复杂构造区煤系气储层发育与富集规律的重点区域。以尼泊尔低喜马拉雅造山带Tansen地区Gondwana群和Surkhet群煤系气储层为... 煤系气是非常规天然气的重要类型,其成储、成藏是构造沉积作用耦合配置下的结果,尼泊尔低喜马拉雅造山带是研究复杂构造区煤系气储层发育与富集规律的重点区域。以尼泊尔低喜马拉雅造山带Tansen地区Gondwana群和Surkhet群煤系气储层为研究对象,分析了冈瓦纳及前陆盆地煤系气储层类型与组合特征,不同煤系气储层微观孔裂隙形貌发育与孔隙结构特征,探讨了逆冲推覆作用下煤系气储层孔裂隙演化过程与优势孔裂隙形成机制,最后,初步预测了煤系气潜在有利储层、有利区与资源潜力。研究结果表明:①尼泊尔低喜马拉雅造山带煤系气储层组合类型主要包括“源储一体型”的煤层-页岩气型、“下生上储型”的煤层-致密砂岩气型和页岩-致密砂岩气型以及“源储紧邻型”的煤层-页岩-致密砂岩气型;②页岩矿物相关的中孔与有机质微孔发育,孔容占总孔容64.6%,比表面积占总比表面积98.1%,煤层主要发育微孔,总比表面积达8.22 m^(2)/g,致密砂岩以粒间孔和微裂隙为主,渗透性在各类储层中最高;③页岩孔裂隙具有破坏和新生双重效应,逆冲推覆作用下不同岩性煤系气储层孔裂隙系统演化各异,煤层主要发生构造揉皱作用并发育更多微孔,致密砂岩则主要表现为构造裂隙的形成与扩展;④Tansen地区东南部Jhadewa矿区是煤系气潜在有利区,Surkhet群Bhainskati组煤层-页岩组合是煤系气优势储层类型,初步估算该地区煤系气资源量达5.04×10^(8) m^(3)。研究旨在初步查明尼泊尔低喜马拉雅造山带煤系气潜在有利储层与有利区,为尼泊尔油气资源评价与勘探研究提供方向。 展开更多
关键词 尼泊尔 低喜马拉雅造山带 煤系气储层 组合类型 孔隙-裂隙 成储成藏潜力
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Impacts of Himalayan tectonism on Eocene gas shale and its pore structure within the Lesser Himalayas,Nepal:Insights for shale gas accumulation and preservation
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作者 kumar khadka Si-Jie Han +6 位作者 Shu-Xun Sang Jun-Jie He Upendra Baral Saunak Bhandari Debashish Mondal Xiao-Zhi Zhou Shi-Qi Liu 《Petroleum Science》 2026年第1期103-126,共24页
This study investigates the complex relationship between organic matter(OM),tectonic deformation,and pore structure development in Eocene Bhainskati shale within the Lesser Himalayan foreland basin,Nepal,to assess its... This study investigates the complex relationship between organic matter(OM),tectonic deformation,and pore structure development in Eocene Bhainskati shale within the Lesser Himalayan foreland basin,Nepal,to assess its implications for shale gas accumulation and preservation.We hypothesize that tectonic deformation and variations in organic matter have a significant impact on pore size distribution,connectivity,and gas retention,thereby influencing shale gas potential.We characterized pore types and quantified pore size distributions using scanning electron microscopy(SEM),mercury intrusion capillary pressure(MICP)techniques,and low-pressure gas adsorption methods.Our findings indicate a predominance of mesopores(1-10 nm range,with a notable peak at 4 nm),suggesting substantial contributions to surface area from micropores and fine mesopores.Thermal maturity negatively impacts porosity and surface area.At the same time,tectonic activity enhances microfracture development,increasing permeability and gas transport,particularly in the Surkhet area,which exhibits higher pore volume and specific surface area than the Tansen area.Tectonic forces shift the shale from brittle to ductile behavior,altering pore connectivity.Himalayan tectonic forces significantly influence shale structure,pore sizes,gas preservation,and migration,enhancing gas adsorption by increasing surface area but posing challenges due to potential gas escape along faults and folds.Understanding the impact of tectonic activity on shale deformation in similar basins within the Himalayas and the adjacent region is vital for assessing shale gas potential and optimizing exploration strategies in tectonically active Nepal Himalayan regions.This study highlights the dual role of tectonics in both promoting and complicating the formation,accumulation,and preservation of shale gas reservoirs,offering critical insights for future exploration efforts. 展开更多
关键词 Gas shale Eocene foreland basin Pore structure Tectonic deformation Himalayan tectonics Gas preservation
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