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- The Upper Triassic ,Lower and Middle Jurassic loos... 找矿目的层是上三叠统和下、中侏罗统的疏松砂岩层。
- The island-arc volcanic rocks are observed in the Upper Triassic Rola Kangri Group. 新发现上三叠统若拉岗日群岛弧相火山岩；
- Formation factors and mechanism of the laumontite in upper Triassic Yanchang group of Jingan oilfield are analyzed. 分析了靖安油田上三叠系延长统浊沸石的形成条件及形成机理。
- Chuxiong basin is a Mesozoic-Cenozoic sedimentary basin developed on the basis of Upper Triassic Epoch faulting-subsiding basin. 楚雄盆地为晚三叠世断陷盆地基础上发展起来的中新生代沉积盆地。
- Dark mudstones and the turbidites of deep lake facies were discovered recently in the Member 1 of Yanchang Formation,Upper Triassic in Ordos Basin. 鄂尔多斯盆地三叠系延长组长1段发育一套深湖相浊积岩及数层暗色泥岩。
- In the tight Upper Triassic sandstone with low porosity and permeability, the distributary channel sand body would be the beneficial target. 在致密低孔低渗的上三叠统厚层砂岩中，分流河道砂体储集性能最好，是勘探的有利目标层。
- The Upper Triassic in the western Sichuan foreland basin can be divided into 4 third order sequences and 12 system tracts. 摘要应用层序地层学方法将川西前陆盆地上三叠统划分为4个三级层序和12个体系域。
- Dark mudstones and the turbidites of deep lake facies were discovered recently in the Member 1 of Yanchang Formation, Upper Triassic in Ordos Basin. 摘要鄂尔多斯盆地三叠系延长组长1段发育一套深湖相浊积岩及数层暗色泥岩。
- The Upper Triassic Yanchang Formation in the Fuxian area is totally a very low porosity and permeability sandstone reservoir. 研究表明,陕北富县延长组总体为特低孔渗砂岩储层。
- The widely developed Upper Triassic coalmeasure source rocks have provided sufficient gases for the pool formed in the Western Sichuan Depression. 川西坳陷广泛发育上三叠统煤系烃源岩,为煤成气成藏提供了充足的气源。
- The upper Triassic in Fuxian area, the geochemistry characters and the distributing mode of REE curve was consistented with the Archaean and the early Proterozoicmetamorphic rock. 富县地区延长组REE地球化学特征及REE分配模式曲线与盆地东北缘太古代及早元古代变质岩一致，而且，镇泾地区和盆地东北缘变质岩REE分配模式也基本一致，说明鄂尔多斯地区在太古代及早元古代为一统一的基底，只是西南及东北构造演化的过程不同，证明了它们物质来源都基本继承了原始物质的特征。
- Since the beginning of the upper Triassic epoch, the Indian plate upthrusted to the north over the Tethys oceanic crust and led to the closure of the Tethys in Eocene epoch. 晚三迭世开始,印度板块在特提斯洋壳上向北仰冲,并导致特提斯在始新世的关闭。
- Tectonic evolution analysis indicates that Wenjiang Structure is a palaeo-present-congruent structure and very close to Upper Triassic gas-generating center. 构造演化分析认为,温江构造为古今叠合型构造,紧邻上三叠统生气中心。
- The Upper Triassic classic reservoir of west Sichuan is a kind of sandstone with low porosity and permeability , intercalated by mudstone layers with abnormally high pressure. 川西上三叠统碎屑岩储层是一套低孔、低渗，具高异常地层压力的致密砂泥岩层。
- Upper Triassic clasolite reservoirs in West Sichuan are a set of tight sand-mud rocks with low porosity-low permeability, high aqueous saturation and abnormal high pressure. 川西上三叠统碎屑岩储层是一套低孔渗，高含水饱和度，具高异常地层压力的致密砂泥岩层。
- Several kinds of biomarker of the source rocks in the Member 1 of Yanchang Formation, Upper Triassic in Shaanbei area have been detected by GC and GC/MS. 本文研究了陕北地区三叠系延长组长1段烃源岩的生物标志化合物特征及其有机质母源类型和有机质成熟度。
- Rare earth elements(REE) and trace elements were used to analyse source rock and source direction of Yanchang Formation of the Upper Triassic in Ordos Basin. 利用稀土元素和微量元素,分析鄂尔多斯盆地中部上三叠统延长组母岩类型和物源方向。
- Xiashi - Chenzhaigou and Xiashi -shimen faults have relative large influence on the preservation of the Upper Triassic, which is well preserved in the l... 在其下盘，上三叠统地层保存良好，在其上盘即推覆体上，上三叠统地层往往遭受严重剥蚀。
- YANG Xiao-ping,QIU Yi-nan.Formation process and distribution of laumontite in Yanchang Formation (Upper Triassic)of Ordos Basin[J].Acta Sedimentologica Sinica,2002,20(4):628-632. [2]杨晓萍;裘怿楠.;鄂尔多斯盆地上三叠统延长组浊沸石的形成机理、分布规律与油气关系[J]
- Aim To discuss the characteristic of high-resolution sequence stratigraphy of member 6 of Yanchang Formation,Upper Triassic in Yujiawan area,Zichang,Ordos Basin. 目的探讨鄂尔多斯盆地子长地区上三叠统延长组长6段基准面旋回层序的识别方法、结构特征、变化规律及成因机理。
