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中国石油大学北京地球科学学院导师教师师资介绍简介-龚承林

本站小编 Free考研考试/2020-05-12



龚承林,男,岗位教授,博士生导师,2014年获中国石油大学(北京)博士学位(导师王英民教授)、2014年至2017年在美国德克萨斯大学奥斯汀分校从事博士后研究(导师Ronald J Steel教授)。
现任《AAPG Bulletin》副主编、《Journal of Sedimentary Research》副主编、《Petroleum Science》副主编、《古地理学报》编委和中国石油大学(北京)优秀青年。
主要从事深水沉积、层序地层和地震资料解释方面的教学与科研工作,主持国家自然科学基金项目两项,在“(1)陆架边缘三角洲—海底扇源汇系统过程和沉积物分配,(2)深水重力流沉积体系及有利储层的形成分布及(3)浊流与底流交互作用的过程响应”取得了国际一流的研究成果,以第一/通讯作者在《Geology》、《Earth-Science Reviews》、《GSA Bulletin》、《Sedimentology》、《AAPG Bulletin》、《Journal of Sedimentary Research》等高水平国际SCI刊物上发表学术论文20余篇。获教育部科技进步奖一等奖1项。
Email:chenglingong@hotmail.com电话:**
1. 团队建设与研究生培养
与美国德克萨斯大学奥斯汀分校导师Ronald J Steel教授课题组有实质的合作关系,可以为有志于从事“深水沉积学或层序地层学研究”的同学提供良好的科研平台和发展机遇。热忱欢迎有志于学术和深水沉积研究的同学加入课题组,愿同同学们一道探索深水沉积学奥秘、尽我所能愿做春泥、甘为人梯。
2. 科研项目
在研项目:
(1)国家自然科学基金面上项目,珠江峡谷末次冰期以来浊流活动对气候变化的响应尺度与反馈机制(**),2020-2023,主持
(2)国家自然科学基金青年科学基金项目,中更新世以来珠江陆架边缘三角洲-海底扇“源-汇同步”的形成机制(**),2019-2021,主持
(3)油气资源与探测国家重点实验室杰出人才培育课题,深水水道的发育、演化及其背景控制,2018-2020,主持
(4)中国石油大学(北京)优秀青年科研启动基金,深水水道的沉积动力学过程重构,2017-2021,主持
(5)中海石油(中国)研究中心课题,墨西哥海域盆地盐相关构造油气运聚机理研究,2018-2020,参与
(6)中石油大港油田课题,多类型斜坡区油气成藏机理研究,2018-2020,参与
结题项目:
(1)中海石油(中国)东海石油天然气作业公司课题,西湖凹陷杭州斜坡带古近系成藏条件及勘探方向研究,2018-2019,主持
(2)中海石油(中国)有限公司天津分公司课题,石南中段浅层油气成藏规律及动力学研究,2018-2019,参与
3. 代表性学术报告
邀请报告:
(1)GongChenglin, et al., Flow processes and sedimentation in unidirectionally migrating deep-water channels, 4th International Submarine Canyon Symposium, Shenzhen, 2018.11.5-2018.11.7 (大会报告-特邀报告)
(2)龚承林等,陆缘深水区浊流与底流交互作用的过程、响应和动力学机制,第六届全国沉积学大会,南京, 2017.10.28-2017.10.30(会议报告-特邀报告)
(3)龚承林等,陆缘深水区浊流与底流交互作用的过程、响应和动力学机制,第五届地球系统科学大会,上海,2018.7.2-2018.7.4(会议报告-特邀报告)
(4)龚承林等,深水单向迁移水道的过程响应及动力学机制,第一届“青年沉积学家论坛”, 北京,北京,2018.11.10-2018.11.10(会议报告-特邀报告)
主持会议:
(1)GongChenglin, Steel Ronald, and Lin Changsong, When and how clastic detritusare transported from shelf-edge staging areas into deep-water areas: From a source-to-sink perspective, 9th International Conference on Asian Marine Geology, Shanghai, China, 2018.10.10-2018.10.12(会议召集人)
(2)SullivanMorgan, GongChenglin, and Sweet Mike, Source to Sink, AAPG 2019 Annual Convention & Exhibition, San Antonio, USA, 2019.5.19-2019.5.22(分会场主席)
(3)GongChenglin, TallingPeter, RebescoMichele,CartignyMatthieu, HeijnenMaarten,and HuPeng, Deep-water channels: Morphology, architecture, flow processes and sedimentation, 34th IAS Meeting of Sedimentology, Roma, Italy, 2019.9.10-2019. 9.13(会议召集人)
4. 代表性学术论文(n= 21,*=通讯作者
(1)Gong, C*., Wang, Y., Zhu, W., Li, W., Xu, Q., Zhang, J., 2011. The central submarine canyon in the Qiongdongnan Basin, northwestern South China Sea: Architecture, sequence stratigraphy, and depositional processes. Marine and Petroleum Geology, v. 28, p. 1690-1702,doi: 10.1016/j.marpetgeo.2011.06.005.
(2)Gong, C*., Wang, Y., Peng, X., Li, W., Qiu, Y., Xu, S., 2012. Sediment waves on the South China Sea Slope off southwestern Taiwan: Implications for the intrusion of the Northern Pacific Deep Water into the South China Sea. Marine and Petroleum Geology, v. 32, p. 95-109, doi:10.1016/j.marpetgeo.2011.12.005.
(3)Gong, C., Wang, Y., Zhu, W., Li, W., Xu, Q., 2013. Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea. AAPG Bulletin, v. 97, p. 285-308, DOI:10.1306/9.
(4)Gong, C*., Wang, Y., Hodgson, D.M., Zhu, W., Li, W., Xu, Q., Li, D., 2014. Origin and anatomy of two different types of mass-transport complexes: A 3D seismic case study from the northern South China Sea margin. Marine and Petroleum Geology, v. 54, p. 198–215, doi: org/10.1016/j.marpetgeo.2014.03.006.
(5)Gong, C*., Wang, Y., Steel, R.J., Olariu, C., Xu, Q., Liu, X., Zhao, Q., 2015. Growth styles of shelf-margin clinoforms: Prediction of sand- and sediment-budget partitioning into and across the shelf. Journal of Sedimentary Research, v. 85, p. 209–229, DOI: http://dx.doi.org/10.2110/jsr.2015.10 (研究亮点).
(6)Gong, C., Wang, Y., Pyles, D.R., Steel, R.J., Xu, S., Xu, Q., Li, D., 2015. Shelf-edge trajectories and stratal stacking patterns: Their sequence-stratigraphic significance and relation to stylesof deep-water sedimentation and amount of deep-water sandstone. AAPG Bulletin, v. 99, p. 1211–1243, doi:10.1306/.
(7)Gong, C*., Wang, Y., Xu, S*., Pickering, K.T., Peng, X., Li, W., Yan, Q., 2015. The northeastern South China Sea margin created by the combined action of down-slope and along-slope processes: Processes, products and implications for exploration and paleoceanography. Marine and Petroleum Geology, v. 64, p. 233–249, 10.1016/j.marpetgeo.2015.01.016.
(8)Gong, C*., Wang, Y., Steel, R.J., Peakall, J., Zhao, X., Sun, Q., 2016. Flow processes and sedimentation in unidirectionally migrating deep-water channels: From a 3D seismic perspective. Sedimentology, v. 63, p. 645–661,doi: 10.1111/sed.12233.
(9)Gong, C*., Steel, R.J., Wang, Y., Lin, C., Olariu, C., 2016. Shelf-margin architecture variability and its role in source-to-sink sediment budget partitioning. Earth-Science Reviews,v. 154, p. 72–101, 10.1016/j.earscirev.2015.12.003 (IF = 9.452, 15 citations).
(10)Gong, C*., Steel, R.J., Wang, Y., Lin, C., Olariu, C., 2016. Grain size and transport regime at shelf edge as fundamental controls on delivery of shelf-edge sands to deepwater. Earth-Science Reviews,v. 157, p. 32–60.
(11)Li, S., Gong, C*., 2016. Flow dynamics and sedimentation of lateral accretion packages in sinuous deep-water channels: A 3D seismic case study from the northwestern South China Sea margin. Journal of Asian Earth Sciences,v. 124, p. 233–246, doi.org/10.1016/j.jseaes.2016.05.008.
(12)Gong, C*., Wang, Y., Zheng, R., Hernandez-Molina, F.J., Li, Y., Stow, D., Xu, Q., Brackenridge, R.E., 2016. Middle Miocene reworked turbidites in the Baiyun Sag of the Pearl River Mouth Basin, northern South China Sea margin: Processes, genesis, and implications.Journal of Asian Earth Sciences,v. 128, p. 119–129, doi.org/10.1016/j.jseaes.2016.06.025.
(13)Gong, C*., Peakall, J., Wang, Y., Wells, M.G., Xu, J., 2017. Flow processes and sedimentation in contourite channels on the northwestern South China Sea margin: A joint 3D seismic and oceanographic perspective. Marine Geology,v. 393, p. 176–193, doi.org/10.1016/j.margeo.2016.11.002).
(14)Gong, C*., Chen, L., West, L.,2017.Asymmetrical, inversely graded, upstream-migrating cyclic steps inmarine settings: Late Miocene-early Pliocene Fish Creek-Vallecito Basin,southern California. SedimentaryGeology,v. 360, p. 35–46, doi.org/10.1016/j.sedgeo.2017.09.002.
(15)Gong, C*., Blum, M.D., Wang, Y., Lin, C., Qiang, X., 2018.Can climatic signals be discerned in the deepwatersink?: An answer from the Pearl River sediment-routing system.GSA Bulletin,v. 130, p. 661–677, doi.org /10.1130 /B31578.1.
(16)Li, L., Gong, C*., Steel, R.J., 2018. Bankfull discharge as a key control on submarine channel morphology and architecture: Case study from the Rio Muni Basin, West Africa. Marine Geology,v. 401, p. 66–80, doi.org/10.1130/G40204.1.
(17)Li, L., Gong, C*., 2018. Gradual transition from net erosional to net depositional cyclic steps along the submarine distributary channel thalweg in the Rio Muni Basin: A Joint 3-D seismic and numerical approach. Journal of Geophysical Research: Earth Surface,v. 123, p. 2087–2106, doi.org/10.1130/G40204.1.
(18)Gong, C*., Wang, Y., Rebesco, M., Salon, S., Steel, R.J., 2018. How do turbidity flows interact with contour currents in unidirectionally migrating deep-water channels? Geology,v. 46, p. 551–554, doi.org/10.1016/j.margeo.2018.04.010.
(19)Gong, C., Steel, R.J., Sweet, M.L., Wang, Y., Li, S., Xu, Q., 2019. Shelf-edge delta overreach at the shelf break can guarantee the delivery of terrestrial sediments to deep water at all sea-level stands. AAPG Bulletin,v. 103, p. 65–90.
(20)Gong, C*., Sztanó, O., Steel, R.J.,Xian, B., Galloway, W., Bada, G., Qiang, X., 2019.Critical differences in sediment delivery and partitioning between marine and lacustrine basins.GSA Bulletin,v. 131, p. 766–781.
(21)Gong, C*., Qi, K., Ma, Y., Li, D., Feng, N., Xu, H., accepted.Tight coupling between the cyclicity of deep-water systems and rising/flat shelf-edge pairs along the submarine segment of Qiongdongnan sediment-routing system.Journal of Sedimentary Research.


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