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| 1 | Delineation of Potential Mineral Resources RegionBased on Geo-anomaly Unit显示文摘The geological anomaly unit method (GAUM) is a new way to delineate and evaluate ore finding targets in line with the “geological anomaly ore finding theory”. Comprehensive ore finding information from geological, geochemical and geophysical data is used for quantitative measurement of the “ore forming geological anomaly unit” in this paper. The main procedures are shown as follows: (1) The geo anomalous events associated with gold mineralization are analyzed in Tongshi gold field; (2) The zonation in the concentrated heavy minerals and the stream sediment elements of ore forming geo anomaly are studied in detail; (3) The deep geological structural framework is deduced by means of the synthetic geological interpretation of gravity and magnetic information; (4) The ore controlling geo anomalies and ore anomalies are chosen as the variables of the favorable ore forming indexes that can be used for the quantitative delineation and evaluation of the potential ore forming regions. | Chen Yongqing Faculty of Earth Resources, China University of Geosciences, Wuhan 430074 The Center for Development and Research, China Geological Survey, Beijing 100083 Liu Hongguang Faculty of Earth Resources, China University of Geosciences, Wuhan 4 | 2000 | Journal of Earth Science2000，19，2： | 5 |
| 2 | COMPARISON OF SCOURS IN FRONT OF VERTICAL BREAKWATERS DUE TO REGULAR AND IRREGULAR WAVES显示文摘In this paper the scours of sand bed due to regular and irregular waves in front of vertical breakwaters, such as scouring patterns, scouring mechanisms, etc., are investigated. Thereby, the scours under the action of the two kinds of waves are compared connected. | Gao Xue ping Department of Civil and Environmental Engineering, Faculty of Engineering, Ehime University, 3 Bunkyo cho, Matsuyama 790 77, JapanKunimitsu Inouchi Center for Cooperative Research and Development, Ehime University, 3 Bunkyo cho, Mats | 2000 | Journal of Hydrodynamics2000，12，1： | 3 |
| 3 | Dynamic Settings and Interactions between Basin Subsidence and Orogeny in Zhoukou Depression and Dabie Orogenic Belt显示文摘This paper presents a study of the geo dynamic setting and the relation between orogenic uplift and basin subsidence in the inland Zhoukou depression and Dabie orogenic belt. Since the Mesozoic the evolution of Zhoukou depression can be divided into three stages: (1) foreland basin, (2) transitional stage, (3) fault depression. Formation and variations of basin were not only related to the orogenesis, but also consistent with the orogenic uplift. | Sun Jiazhen Yang Xianghua Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China Qiu Ronghua He Mingxi Exploration and Development Institute of Henan Oilfield, Nanyang 473132, China | 2000 | Journal of Earth Science2000，19，3： | 2 |
| 4 | Core elements of epilepsy diagnosis and management: expert consensus from the Leadership in Epilepsy, Advocacy, and Development (LEAD) faculty显示文摘 | Glauser TA Sankar R Co-chairs of the Leadership in Epilepsy Advocacy and Development Faculty | 2008 | Curr Med Res Opin2008，24，12： | 1 |
| 5 | Wave reflection, transmission and harmonics due to different submerged structures显示文摘Comparisons of wave reflection, transmission and harmonics due to different types of sub merged structures are investigated by a numerical method, the boundary-fitted coordinate (BFC) method. The types of submerged structures include a submerged horizontal plate, submerged breakwa ters (rectangular and trapezoidal) and a step-type structure (topography). First, the BFC method is ver ified by comparing the computed results with the experimental data, including wave surface elevations, reflected and transmitted wave heights, and amplitudes of higher harmonics, showing that the method is a reasonable one to predict wave deformations due to the submerged structures. Secondly, the wave sur face elevations and the higher harmonics over different submerged structures are compared. Thirdly, re flected and transmitted waves due to different submerged structures are investigated. | Gao Xueping1 Inouchi Kunimitsu2 Kakinuma Tadao3 (1. Hydraulics Institute, Faculty of Civil Engineering, Tianjin University, Tianjin 300072, China 2. Center for Cooperative Research and Development, Ehime University, 3 Bunkyo-cho, Matsuyama 790 - 8577, Japan 3. Nagasaki Comprehensive University, Aba-cho 536, Nagasaki 851 - 0193, Japan) | 2000 | Acta Oceanologica Sinica2000，19，2： | 1 |
| 6 | Depositional Sequences of Yitong Graben (Eastern China) and Its Response to Transform-Extensional Processes显示文摘INTRODUCTIONTheTancheng-Lujiangfaultbeltisthelargeststrike-slipfaultbeltinEastChina.Thisfaultbelthasundergoneacom-plicatedgeo... | Lu Yongchao Ren Jianye Li Sitian Chen Ping Ye Hongpo Faculty of Earth Resources, China University of Geosciences, Wuhan 430074 Cui Xuezhou Li Bencai Institute of Exploration and Development of Jilin Oil Field, Fuyu 131200 | 1999 | Journal of Earth Science1999，18，2： | 1 |
| 7 | Development of Diapirs and Accumulation of Natural Gases in Yinggehai Basin显示文摘Overpressure developed throughout most of the Yinggehai basin. The burial depth to top overpressure varied from about 1 600 m to 4 500 m, with the shallowest top overpressure occurring in the depocenter. The main cause of the overpressure was disequilibrium compaction resulting from rapid sedimentation of fine grained sediments. The overpressure was strengthened by the retention of fluids including gases due to lack of faults before diapir development. The diapirism in the Yinggehai basin was a combined result of the strong overpressure and the tensile stress field caused by the right lateral slip of the boundary fault. The diapirism, a product of the movement of overpressured fluids and plastic shales, shaped the vertical conduits from source to traps that would be absent without overpressured fluid release. Natural gas accumulation in traps in the diapir structure zones was also intermittent, which can be inferred from the inter reservoir compositional heterogeneity, transient thermal effect of fluid flow and migration fractionation. | Gong Zaisheng China National Offshore Oil Corporation, Beijing 100029 Yang Jiaming Institute of Petroleum Exploration and Development, China National Offshore Oil Corporation, Gaobeidian 074010 Hu Jianwu Hao Fang Faculty of Earth Resources, | 2001 | Journal of China University of Geosciences2001，12，2： | 1 |
| 8 | Extensional Tectonic System of Erlian Fault Basin Groupand Its Deep Background显示文摘INTRODUCTIONInhighlyextendedregions(β>1.5-2)suchastheBasinandRangeProvinceandpasivemargins,extensionaltectonicsystemischaract... | Ren Jianye Li Sitian Faculty of Earth Resources, China University of Geosciences, Wuhan 430074 Jiao Guihao Exploration and Development Research Institute, Huabei Oil Administration Bureau, Renqiu 062552 Chen Ping Faculty of Business Administratio | 1998 | Journal of Earth Science1998，17，3： | 1 |
| 9 | Depositional Responding to Tectonic Evolution of East China Sea Shelf Basin显示文摘DepositionalRespondingtoTectonicEvolutionofEastChinaSeaShelfBasin*LuYongchaoWuFadongXieXinongChenPingFacultyofEarthResources,... | Lu Yongchao Wu Fadong Xie Xinong Chen PingFaculty of Earth Resources, China University of Geosciences, Wuhan 430074 Zhou Ping Li Peilian Xu WeilingShanghai Institute of Offshore Petroleum Exploration and Development, MGMR, Shanghai 200120 | 1997 | Journal of Earth Science1997，16，1： | 1 |
| 10 | Complex petroleum accumulating process and accumulation series in the buried-hill trend in the rift basin:An example of Xinglongtai structure trend,Liaohe subbasin显示文摘The buried-hill trend is a typical style of the petroliferous structure in the faulted basin of eastern China. The Xinglongtai structure trend in the Liaohe subbasin,Bohai Bay Basin is a buried faulted-hill trend resulting from the periodic faulting of the Tai’an-Dawa faults. The structure was cut by various faults,which are interlinked and constitute the conduits for petroleum migration. Petroleum accumulated in the Tertiary sandstones and pre-Tertiary basement of metamorphosed rocks through the migration pathways of the fault system. Petroleum in the structure was derived from different hydrocarbon kitchens to form a hybrid field complex. Petroleum charged the structure from different directions and accumulated in various reservoirs through different pathways in different times. The accumulations in the buried hill trend of Xingongtai are composed of two types of traps in the two stratigraphic systems: traps in the Tertiary sandstones were formed by the fault blocks and by the pinchout of the sandstone,and traps in the pre-Tertiary basement of metamorphosed rocks were formed by fissures in the inner part of the buried hills and by the unconformity near the surface of the buried hills. | GAO XianZhi1,PANG XiongQi1,LI XiaoGuang2,CHEN ZhenYan2,SHAN JunFeng2,LIU Feng1,ZOU ZhiWen1 & Li WeiLian1 1 Faculty of Resources and Information Technology,China University of Petroleum,Beijing 102249,China 2 Exploration and Development Institute of Liaohe Oilfield,Petrochina Liaohe Oil Company,Panjin 124010,China | 2008 | Science China Earth Sciences2008，51，S2： | 0 |
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