1、

An analysis of Late Permian Early Triassic sedimentary evolution and tectonic setting in the Linxi region shows that the Late Paleozoic plate tectonic movement in the southern Da Hinggan Mountains continued till the Indosinian tectonic cycle.

林西地区晚二叠世早三叠世的沉积构造演化特征揭示,大兴安岭南部的晚古生代板块构造活动一直到印支构造旋回才结束。

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2、

Late Paleozoic Strata and Tectonic Facies in the Northern Margin of the Eastern Kunlun Orogen and their Tectonic Implications

东昆仑南缘晚古生代地层组合、大地构造相及大地构造意义

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3、

Tectonic Framework and Evolution of Ordos Massif in Early Paleozoic

鄂尔多斯地块早古生代构造格局及演化

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4、

Based on the Middle-Late Paleozoic pillow lava and Permian-Triassic tectonic melange, this paper shows that there is a melange zone along Qinzhou-Cenxi-Luoding-Yunfu.

作者等在两广交界罗定一带新发现了中晚古生代的枕状熔岩和二叠&三叠纪的构造混杂岩,结合区域构造,分析并提出了钦州-岑溪-罗定-云浮构造混杂带的存在。

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5、

The tectonic evolutionary process of the Paleozoic metamorphic rocks series have been discussed primary.

并初步探讨了古生代变质岩系的构造演化过程。

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6、

Compound ancient tectonic system and natural gas of Early Paleozoic in Ordos Basin

鄂尔多斯盆地早古生代复合的古构造体系与天然气

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7、

Early Paleozoic Tianshui-Wushan Tectonic zone of the Northern Margin of West Qinling and its Tectonic Evolution

西秦岭北缘早古生代天水&武山构造带及其构造演化

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8、

The Upper Paleozoic Carboniferous-Permian source rocks are mainly coal measure strata, with thickness in the range of 150~ 500m, low to medium organic matter abundance, and type ⅲ kerogen.

上古生界石炭&二叠系烃源岩主要为煤系地层,厚度为150~500m,有机质丰度属于低-中等,有机质类型为Ⅲ型。

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9、

Au ( Cu, Ni, Cr) subseries related to Na-rich and high-alkaline basalt and tholeiite of paleozoic arc island(ⅱ);

古生代岛弧区与富钠高碱玄武岩拉斑玄武岩有关的Au(Cu、Ni、Cr)成矿亚系列;

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10、

Discussion On Time-Depth Conversion for Paleozoic

古生界时深转换关系探讨

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11、

These offered new information for studying sedimentary environment, regression time and direction in Late Paleozoic in northern Xinjiang.

综合古生物、地球化学、沉积等特征认为本区晚二叠世为近海陆缘湖泊沉积环境。这为研究新疆北部晚古生代沉积环境、海退时间及方向提供了新的信息。

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12、

The predominance of C_ 29 sterane in early Paleozoic and Precambrian rocks and crude oils is puzzling, because the predominance of C_ 29 sterane is often taken as the result of high terrestrial plant input.

在早古生代与前寒武纪的石油与源岩中,经常出现令人困惑的C29甾烷优势,而在有机地球化学中C29甾烷优势被认为是陆相有机质输入的标志。

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14、

Study of the thermal history reconstruction for Lower Paleozoic carbonate succession

沉积盆地下古生界碳酸盐岩地区热历史恢复方法探索

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15、

The melanic mudstones, coal beds and limestones in the lower part of the Carboniferous-Permian of the Upper Paleozoic are of high organic matter content, high thermal evolution level and high gas generating potential, which provided sufficient gas source for forming Paleozoic gas reservoirs;

上古生界石炭&二叠系下部沉积的暗色泥岩、煤层和石灰岩有机质含量高、热演化程度高、生气能力强,为古生界气藏的形成提供了充足的气源;

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16、

Genesis of coal metamorphism of Late Paleozoic coals in the south of North China-a further approach to the effects of thermal groundwater on coal metamorphism

华北地区南部晚古生代煤的变质成因&地下水热液对煤变质作用影响的进一步探讨

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17、

These data suggest that the granulite facies metamorphism lasted for about 27 Ma and was related to crustal thickening associated with the Early Paleozoic continental collision between the Qilian and Qaidam blocks, and to subsequent thermal relaxation and exhumation.

这些年龄结果显示麻粒岩相变质作用持续了大约27Ma,这可能与早古生代祁连地块与柴达木地块碰撞作用所引起的地壳加厚和后来的热松驰有关。

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18、

The Paleozoic strata of the Jilin geosynclinal area

吉林槽区的早古生代地层

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19、

Redetermination of the boundary between Chinese platform and Da Hinggan Ling-Mongolian Paleozoic geosynclinal folded belt

中华地台与兴蒙古生代地槽褶皱区界线的重新厘定

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20、

Determined by characteristics of sedimentagraph, undersize sedimentary faces and field test pressure in Ordos lower Paleozoic, Ordovician reservoirs are of a pressure system of oil gas.

依靠沉积相、沉积微相以及实测地层压力的差异对鄂尔多斯盆地古生界含油气系统进行划分,论证了奥陶系天然气藏落在一个含油气压力系统中。

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