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| 1 | Sedimentology and Sequence Stratigraphy of Marine to Lacustrine Deltaic Deposits in a Craton Basin and Their Controlling Factors: Shan 2 Member–He 8 Member(Guadalupian–Lopingian, Permian), Southeast Ordos Basin, North China显示文摘The Shan 2 Member, Shan 1 Member and He 8 Member of the Mid–Late Permian Shanxi and lower Xiashihezi formations, in the southeastern Ordos Basin, together comprise ~150 m of deltaic deposits. This sequence records an overall evolution from deep marine environment to shallow lake associated with braided river, braided river delta and meandering river delta. Core description, well log interpretation, and stable isotope analysis, including carbon, oxygen and strontium, were conducted to understand the sedimentary evolution of Shan 2 to He 8 Member. The Shanxi Formation, which consists of the Shan 2 and Shan 1 members, is characterized by a tidal-influenced meandering river delta environment and a higher δ^(13)C value and ^(87)Sr?(^(86)Sr) ratio and a lower δ^(18)O value. The He 8 Member, the basal part of the Xiashihezi Formation, is featured by a braided river to braided river delta system and a lower δ^(13)C value, ^(87)Sr?(^(86)Sr) ratio, and a higher δ^(18)O value. Four third-order depositional sequences separated by five sequence boundaries are determined. Coarsening upward sequences of the Shan 2 Member–He 8 Member indicate a general regression trend, which can be correlated to global sea-level fall occurring during the Roadian–Wuchiapingian, as also evidenced by previous published zircon U–Pb results. The coal-bearing sequence(Shanxi Formation) to non-coal-bearing sequence(He 8 Member), as well as a decrease of ^(87)Sr?(^(86)Sr), suggest a trend from humid to arid climates. A combined effect of sea-level drop and a small uplift at the end of Shanxi Formation are proposed. | SHAN Xin YU Xinghe Peter CLIFT LI Yalong JIN Lina SU Dongxu DU Yonghui ZHOU Jinsong HAN Xiaoqin | 2018 | Acta Geologica Sinica(English Edition)2018，92，1： | 4 |
| 2 | Development of the East Asian monsoon: Mineralogical and sedimentologic records in the northern South China Sea since 20 Ma显示文摘 | Shiming Wan Anchun Li Peter D. Clift Jan-Berend W. Stuut | 2007 | Palaeogeography Palaeoclimatology Palaeoecology2007，，3： | 1 |
| 3 | Genchemical evolution of the Dras-Kohistan arc during collision with Eurasia:evidence from the ladakh Himalaya, India 显示文摘 | PETER D CLIFT ROBYN HANNIGAN | 2002 | The Island Arc2002，11，： | 1 |
| 4 | Erosional response of South China to rifting and monsoonal strengthening; a record from South China Sea显示文摘 | CLIFT Peter LEE Jae Il CLARK Marin1 K | 2002 | Marine Geology2002，184，： | 1 |
| 5 | Seismic reflection evidence for a dangerous grounds miniplate: No extrusion origin for the South China Sea显示文摘 | Peter Clift GhLee NaDuc | 2008 | Tectonics2008，27，： | 1 |
| 6 | Provenance discrimination of siliciclastic sediments in the middle Okinawa Trough since 30<ce:hsp sp='0.25'/>ka: Constraints from rare earth element compositions显示文摘 | Yanguang Dou Shouye Yang Zhenxia Liu Peter D. Clift Xuefa Shi Hua Yu Serge Berne | 2010 | Marine Geology2010，，1： | 1 |
| 7 | Preferential mantle lithespherie extension under the south China margin显示文摘 | Clift Peters Lin Jian | 2001 | Marine and Petroleum Geology2001，18，： | 1 |
| 8 | Evidence of low flexural rigidity and low viscosity lower continental crust during continantal break-up in the South China Sea显示文摘 | Clift Peter Lin Jian Barekhansen Udo | 2002 | Marine and Petroleum Geology2002，19，： | 1 |
| 9 | Cognitive predictors of adherence to malaria prophylaxis regimens on return from a malarious region: a prospective study 显示文摘 | Charles Abraham Stephen Clift Peter Grabowski | 1999 | Social Science & Medicine1999，48，11： | 1 |
| 10 | Ground-penetrating radar study of beach-ridge deposits in Huangqihai Lake, North China: the imprint of washover processes显示文摘在湖的盆决定沙滩山脉的起源能经常是有问题的。为胡昂基海·莱克的北方岸上的沙滩山脉的形成负责的沉积过程被使用渗透雷达(GPR ) 的地面调查。400 MHz GPR 天线被用来完成 0.04-0.08 m 的高垂直的分辨率。雷达地层学然后用地震地层学的原则被决定。雷达外形(RF ) 被分析思考,以及思考结束模式的内部配置和连续性决定。识别 RF 掉进三个组(倾向,水平、不规则) 。使倾向的组由显示使倾向了的 RF 组成思考。水平组由 RF 组成展出主要水平的思考。在不规则的组,思考典型地是弱的。有思考与的 RF 轻轻地,向陆地,在岸正常侧面的剧降作为 washover 表存款被解释。有陡峭地向陆地蘸、使 washover 脑叶成鳞状的思考的 RF 作为被解释。当冲洗没能进入水的重要身体,沉积完全在相对弄平的地形学上发生时, Washover 表发展。当冲洗进入地形学向陆地陡峭地在蘸的一个区域时, Washover 脑叶开发发生,并且沉积发生在 washover 表或以前的 washover 脑叶的表面上。当从垂直地并且旁边地叠的 washover 表和 washover 脑叶完全被形成,沙滩山脉存款被解释。他们被波浪主导的过程和沿岸的水流补充的第二等的冲洗过程形成。 | Xin SHAN Xinghe YU Peter D. CLIFT Chengpeng TAN Shunli LI Zhixing WANG Dongxu SU | 2016 | Frontiers of Earth Science2016，10，1： | 0 |
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