About 182 item dissertation in line with Triassic query results,the following is 1 to 50(Search took 0.099 seconds)
- The Identification of Reservoirs Fractures and Evaluation of Optimized Well Pattern about Xifeng Oilfield,ZhaoZuo/Xi'an University of Petroleum,0/4
- Reservoir Description of the Chang4+5-Chang6of the Xinzhai Block in the Wuqi Area, Ordos Basin,WangChao/Xi'an University of Petroleum,0/1
- Integrated Research of Gas Exploration Technology in the Upper Triassic Formation in Southwestern Part of Sichuan Basin,LiYueGang/Southwest Petroleum University,0/24
- Types of Barrier Carbonate Platform and Their Evolution,ZhouJinGao/Southwest Petroleum University,0/38
- Research of the Oil and Gas Accumulation Conditions of Daheyan Region, Turpan-hami Basin in the Carboniferous-triassic,YangXiaoZuo/Ocean University of China,0/60
- Research on Tectono-Sedimentary Characteristic of Marine Strata from Caboniferous to Middle Triassic in Southern Qilian Area and Northern Belt of West Qinling Mountains,ChenYongZhen/Northwestern University,0/42
- The Changes of Depositional Environments and Its' Influence of the Early Triassic Nanlinghu Formation in Zuoshan Area, Susong County, Anhui Province,NingXiaoFeng/Hefei University of Technology,0/26
- Triassic Sequence Architecture of North Carnarvon Basin during Continental Margin Depression Period,HuangZhong/China University of Geosciences,0/8
- Sedimentary Characteristics and Environmental Significance in the Late Early Triassic along Lower Yangtze River of Anhui Province,LiJunQing/Hefei University of Technology,0/24
- Study of Trassic Cyclic Stratigraphy in Tarim Basin and Reseach on Recovery of Erosion Thickness by Sedimentation Rate,WangZhiChao/Chinese Geology University (Beijing),0/3
- Sedimentary Characterristics of the Upper Triassic Riganpeicuo Formation at Renacuo Area, Gaize, Tibet,HouEnGang/Chinese Geology University (Beijing),0/0
- Sedimentary Characteristic of Triassic in Sourthern of the East Kunlun and the Constraints on the Closing Time of A'nimaqing Ocean,YueYuanGang/Northwestern University,0/0
- The Northwest Sichuan Basin, two basic characteristics of Triassic boundary strata microbial rock and geological significance,TangHao/Southwest Petroleum University,0/31
- Triassic-Jurassic Volcanic Rocks in Western Liaoning:Implications for Lower Crustal Reworking and Lithospheric Destruction in the North Part of Eastern North China Craton,MaQiang/China University of Geosciences,0/28
- Triassic Shoshonite Association-A-type Granites Belt in South China and Its Geological Implications,LiuYuanYuan/China University of Geosciences,0/27
- Felsic Volcanism in South China Across the Permian-Triassic Boundary,GaoQiuLing/China University of Geosciences,0/24
- Diversity and Ecology of Acritarchs (Organic-walled Microphytoplankton) at the Permian-Triassic Boundary (PTB), South China,LeiYong/China University of Geosciences,0/15
- Study on Early-Middle Triassic Conodont Biostratigraphy in Nanpanjiang Area,YanChunBo/China University of Geosciences,0/33
- Coupling Climatic and Biodiversity Changes with Volcanisms during the Palaeozoic-Mesozoic Upheavals in South China,SunYaDong/China University of Geosciences,0/44
- Study on Turning Fracturing Stimulation Inner Fracture Technology in Triassic Oil Zone,WangZuo/Xi'an University of Petroleum,0/15
- Study on Sedimentary Facies and Reservoir Characteristics of Triassic in Yuqi Area,LiZhuo/Chengdu University of Technology,0/6
- Study on the Characteristic of Petrology and Diagenesis of the Reservoir in the4Th Member of Xu Jia He Formation in Upper Triassic of Sichuan Foreland Basin,TianZuo/Chengdu University of Technology,0/57
- The Description of Chang6Segment Reservoir in Huai Shuang Zhuang Exploration Area of Yan Chang Oil Field,FuBin/Xi'an University of Petroleum,0/96
- The Reservoirs Characteristics of the Mid-triassic Leikoupo Ormation, in the Central Segment of the Western Sichuan Epression,MiSeZiHa/Chengdu University of Technology,0/60
- Characters and Importances of Earliest Triassic Anachronistic Limestones in Northwestern Sichuan Area,WangYanYan/Chengdu University of Technology,0/65
- Geochemistry Characterics of Late-Triassic Source Rocks in Qiangtang Basin, Qinghai-Tibet Plateau,ChenWenBin/Chengdu University of Technology,0/71
- The Research of Stratum Characteristics and Restored Prototype Basin in Hami Depression,ZhouHaiTing/Ocean University of China,0/94
- Evaluation of the southern Qilian basin reservoir characteristics of Triassic hydrocarbon source rock and reservoir characters,YangMengHui/Northwestern University,0/88
- Reservoir Seismic Prediction in the Sequence Stratigraphic,ZhangZuoHua/Chengdu University of Technology,0/125
- Geochemical Characteristics and Comparison of T3-K Source Rocks in the West and Middle Sichuan,LuoZuo/Chengdu University of Technology,0/113
- Integrated Study of Reservoir Geology of Karamay Formation in Liudong District,HuangYuJin/Yangtze University,0/124
- Study on the Relationship between Reservoirs Rocks Characteristics and Sedimentary–diagenesis Evolution of Triassic Jialingjiang Formation in Sichuan Basin,LinXiong/Chengdu University of Technology,0/302
- Research on Sequence Stratigraphy of the Upper Permianseries Changxing Formation and the Lower Triassic Fei Xianguan Formation in Western Sichuan Basin,HuangDan/Yangtze University,0/173
- Reservoir Forming Condition of the Xujiahe Formation of the Upper Triassic in Yuanba Area Sichuan Basin,PanChangLin/Chengdu University of Technology,0/477
- Reservoir Characteristics and Exploration Prospect of Triassic Leikoupo Formation-Ma’antang Formation in the Central and Northern Parts of Western Sichuan Basin,QinChuan/Chengdu University of Technology,1/182
- The Mesozoic Tectonic-magmatic Evolution Process and Gold Metallogenesis in Chifeng-chaoyang Region, Northern North China Craton,FuLeBing/China University of Geosciences,1/603
- Paleomagnetic Results from Sills in Luanshanzi Fonnation in Kuancheng Luojiagou Area, Hebei, and Their Tectonic Implications,LvJing/Chinese Geology University (Beijing),0/29
- A Study on Geologic Feature and Structural Setting of the Lower Triassic Hongshuichuan Formation in Eastern Section of the East Kunlun Orogen,YangZhongZhi/Chang'an University,0/35
- Provenance Analysis of Sandstone, Character of Paleocurrent Direction and Geotectonic Significance of Triassic in South of Gonghe Basin in East Kunlun,ChenZhen/Chinese Geology University (Beijing),0/102
- Sedimentary-Tectonic Evolution from Permian to Triassic in Luoji, Zhongdian County,FuXiaoWen/Chengdu University of Technology,4/38
- Cenozoic Thermal History of the Longmenshan Thrust Belt: Implication for the Uplift Mechanism in the Eastern Margin of the Tibetean Plateau,TanXiBin/Institute of Geology of China Earthquake Administration,1/177
- Mesozoic Tectonic Evolution of the Southeast China Block,MengLiFeng/Zhejiang University,1/742
- Sedimentary Characteristics and Tectonic Setting of the Middle Triassic Pingxiang Basin, Guangxi,SongBo/Chinese Academy of Geological Sciences,0/22
- The Lower Triassic Conodonts and Its Biostratigraphy at the Guan Ziba Section,Wangcang,Sichuan Basin,SongXianTeng/Chinese Geology University (Beijing),0/65
- Study on the Triassic-jurassic Tectonic Evolution of the Middle Great Xing’an Range,LiShiChao/Chinese Academy of Geological Sciences,1/367
- Study on Lower Triassic Stratigraphy of High Resolution Geochemistry for Chaohu Section, Anhui Province:Implication for Paleo-environment,ChenJianBo/China University of Geosciences,0/105
- In-situ Shrimp Oxygen Isotopic Study on Conodonts from the Permian/Triassic Boundary of Wenbudangsang Section, Tibet,ZhouLiQin/Chengdu University of Technology,1/100
- Sandstone Grain Size Analysis and Environmental Significance of Lower Triassic Kanglu Formation Gangmari Region, Tibet,ZhangShuaiJun/Chinese Geology University (Beijing),0/13
- Studies on Geological Characteristics and Forming Age of Southern Xiangjia Mountain Granitic Pluton at East Section of East Kunlun Orogenic Belt,WangXueLiang/Chang'an University,1/65
- "Anachronistic Facies" in the Early Triassic Recovery Time,ZhaoXiaoMing/China University of Geosciences,0/49
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