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1)  The shale rock of the upper Paleozoic
上古生界泥质岩
2)  the upper Paleozoic
上古生界
1.
Gas pool-forming conditions for Bohai Bay Basin and Ordos Basin in the Upper Paleozoic;
渤海湾盆地及鄂尔多斯盆地上古生界天然气成藏条件分析
2.
Characteristics of the reservoir porosity structures and their controlling factors from the Upper Paleozoic in the northern part of west margin, Ordos Basin;
鄂尔多斯盆地西缘北段上古生界储集层研究
3.
The Tectonic Environment,Typical Gas Pools and Exploration Direction of Coal type Gas Provinces in China Ⅰ——Coal type Gas of the Upper Paleozoic;
中国煤型气区的构造环境、典型气藏及勘探方向Ⅰ——上古生界煤型气
3)  Upper Palaeozoic
上古生界
1.
Characteristics of Upper Palaeozoics Sandstone Reservoirs in the Middle of Ordos Basin;
鄂尔多斯盆地中部上古生界砂岩储集层特征
2.
Segmentation of North China craton and gas-bearing problem in upper Palaeozoic of North China Plain.;
华北克拉通分割与华北平原上古生界含气问题
3.
Distribution and genesis of large-scale Upper Palaeozoic lithologic gas reservoirs on Yi-Shaan Slope;
伊陕斜坡上古生界大面积岩性气藏分布与成因
4)  Neopaleozoic [,ni:əu,peiliə'zəuik]
上古生界
1.
Reservoir characteristics of neopaleozoic in the east of ordos basin;
鄂尔多斯盆地东部上古生界储层特征
2.
The Study on the Assemblage of Generating-Reservoir-Cover in Neopaleozoic of Hangjinqi Area in the North of Ordos Basin;
鄂尔多斯杭锦旗地区上古生界生储盖组合研究
3.
Neopaleozoic Petroleum Reservoir Geology & Pool-Forming Conditions in the South of North China Basin;
华北盆地南部上古生界储层地质与油气成藏条件研究
5)  Upper Paleozoic
上古生界
1.
Analysis on control factors of sandstone reservoir of the Upper Paleozoic in Ordos Basin;
鄂尔多斯盆地上古生界砂岩储集层控制因素分析
2.
Evaluation method for petroleum exploration prospect of hydrocarbon-generation paleo-strata in superimposed basins——A case study of the Upper Paleozoic strata of Zhoukou Depression in the southern North China;
叠合盆地老烃源岩系油气勘探前景评价方法——以南华北周口坳陷上古生界为例
3.
Upper Paleozoic-Lower Mesozoic in the Coqên basin, Tibet, China:A potential petroleum-bearing sedimentary sequence.;
西藏措勤盆地的上古生界—下中生界:潜在的油气沉积建造
6)  upper palaeozoic gas bearing sandstone
上古生界含气砂岩
补充资料:泥质岩
泥质岩
argillaceous rocks

   含有大量粘土矿物,且粒径小于0.0039毫米的沉积岩。又称粘土质岩。包括泥岩、粘土岩、页岩、板岩等。因形成条件不同,有白、灰白、灰、黄、绿、红褐、棕等各种颜色。常见胶状、豆状、鲕粒状结构和鳞片状、毡状、格子状构造。主要由粘土矿物(高岭石、埃洛石、蒙脱石、水云母、海泡石等)、碎屑矿物(石英、长石、云母等)和某些自生非粘土矿物(铁、锰的氧化物、氢氧化物和碳酸盐矿物等)组成。依混入物可分为粉砂泥质岩、砂质泥质岩等;依粘土矿物,可分为高岭石泥质岩、蒙脱石泥质岩、水云母泥质岩等。泥质岩是沉积岩中分布最广的一类岩石,约占沉积岩总面积的60%。泥质岩具有可塑性、耐火性、烧结性、干缩性、吸附性、吸水膨胀性等特点,被工业部门广泛利用。
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