四川盆地下二叠统灰岩储层中，较大储量缝洞系统以东吴期暴露溶蚀形成的管道状溶洞系统为主要储集空间。
The tubular cave system resulted from erosion in Dongwu stage are the main reservoir space of Lower Permian limestone reservoirs in Sichuan Basin.
对塔里木盆地石炭系低成熟的泥岩和灰岩生油岩进行了热模拟实验研究。
In this paper, low mature mudstone and limestone from Carboniferous System in Tarim Basin have been studied by the thermal simulating experiment.
鄂尔多斯盆地东部地区太原组广泛发育的气源岩为生物灰岩、暗色泥岩和煤。
Biologic limestone, black mudstone and coal in Taiyuan group of lower Permian in east part of Ordos basin.
柴达木盆地第三系藻(蓝细菌)灰岩储层分布较广，是柴达木盆地第三系碳酸盐岩储层中最重要的油气储层。
Tertiary algal (cyanobacteria) limestones reservoirs in the western Qaidam basin are characterized by widespread distribution and being the most important in the carbonate reservoirs.
柴达木盆地第三系藻灰岩储层分布较广，是柴达木盆地第三系碳酸盐岩储层中最重要的油气储层。
Distributed in extensive areas, Tertiary algal limestone reservoirs in Qaidam basin are the most important oil and gas reservoirs in the Tertiary carbonate rock reservoirs in the basin.
塔里木盆地石炭系生屑灰岩段的主要沉积相类型划分为滨岸相和碳酸盐台地相两大类。
The sedimentary facies of Carboniferous Bioclastic Limestone Member is mainly classified into shore and carbonate platform facies in Tarim basin.
西汉水群出露于盆地的南部，以板岩、千枚岩及砂岩为主，夹灰岩块和生物礁；
The Xihanshui Group, which distributes in the southern of the basin, is mainly slates, phyllites and sandstones with carbonatite and reef blocks.
盆地周围为前震旦纪变质岩系及古生代灰岩、页岩组成的高丘、低山。
Of, belonging to, or being the geologic time, system of rocks, and sedimentary deposits of the sixth period of the Paleozoic Era, characterized by the development of coal-bearing rock formations.
中三叠个旧组以白云岩、灰岩和泥岩为主，属于个旧-那坡弧后裂谷盆地热沉降背景下形成的沉积序列。
Gejiu Formation in Triassic was mainly comprised of dolomite, limestone and mudstone, belonging to the sedimentary sequences of Gejiu-Napo back-arc rift basin under the regime of thermal subsidence.
中三叠个旧组以白云岩、灰岩和泥岩为主，属于个旧-那坡弧后裂谷盆地热沉降背景下形成的沉积序列。
Gejiu Formation in Triassic was mainly comprised of dolomite, limestone and mudstone, belonging to the sedimentary sequences of Gejiu-Napo back-arc rift basin under the regime of thermal subsidence.
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