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邱楠生

资料来源:      日期:2018年08月20日 22:54     浏览量:

姓名

邱楠生

性别


籍贯

福建

出生年月

1968.07

最高学历

博士

职称

教授

联系电话

010-89733340

电子邮箱

qiunsh@cup.edu.cn

联系地址

安徽省淮南市舜耕中路168号安徽理工大学 邮编:232001

邱楠生,男,福建连城县人,1968年7月生,教授,博士生导师,国家杰出青年基金获得者。1989年淮南矿业学院(现安徽理工大学)本科毕业,1991年于中国矿业大学北京研究生部获煤田地质学硕士学位,1994年于中国科学院地质研究所获构造地质学博士学位。1998.10~1999.4在美国Oklahoma State University做访问学者。1994年7月至今在中国石油大学(北京)盆地与油藏研究中心从事教学与科研工作,2012-2016担任中心主任。研究方向为沉积盆地温压场、盆地构造~热演化和油气成藏机理。发表SCI收录论文64篇(其中第一作者26篇,指导的研究生为第一作者的19篇),EI收录36篇,出版专著3部。现为《地学前缘》、《石油学报》、《Petroleum Science》和《石油科学通报》编委,中国地质学会构造地质学与地球动力学专业委员会副主任,中国地球物理学会地热专业委员会委员,地球科学学院学术委员会主任。获得教育部自然科学一等奖等省部级一等奖5项,2003年获得青年地质科技奖、2005年入选教育部“新世纪优秀人才支持计划”,2011年获国家杰出青年科学基金资助,2014年获第七届黄汲清青年地质科学技术奖。

研究领域

沉积盆地温压场,沉积盆地热体制和热历史,油气成藏史和成藏机理

主要研究项目

【1】国家自然科学基金重大项目“页岩气改造-散失途径与保存条件”子专题(2017-2021)

【2】国家“973”项目“构造热演化与页岩气的改造和保存”课题之子专题(2012-2016)

【3】中国石油勘探开发研究院杭州地质研究院项目“四川盆地震旦~古生界深层碳酸盐岩温压场研究”(2015-2016)

【4】华北油田项目“冀中坳陷重点潜山带油气成藏动力与优势运移方向”(2015-2016)

【5】 国家杰出青年科学基金项目“石油与天然气地质学”(2012-2015)

【6】国家自然基金重点项目“华北克拉通破坏的地热学响应-来自沉积盆地热历史的约束”(2012-2015)

【7】国家自然基金“塔里木盆地西北缘构造-热演化的低温热年代学约束”(2011-2013)

【8】国家自然基金“有机质自由基热演化的时间-温度效应机制研究”(2005-2007)

【9】 国家自然基金“沉积盆地中微量元素抑制或催化有机质成熟的机理” (2004-2004)

【10】国家油气重大专项“典型大型气田形成的温压场研究”专题(2009 -2015)

【11】国家油气重大专项“准噶尔盆地准中地区油气成藏动力研究”专题(2011-2015)

【12】国家“973”项目“中国西部叠合盆地多期构造过程叠加与深部古温压场重建”课题之子专题(2011-2015)

【13】国家“863”项目“天然气水合物成藏条件实验模拟技术”(2006-2010)

【14】 国家“十五”攻关子课题“济阳坳陷下第三系隐蔽油气藏成藏机理” (2000-2003)

【15】教育部重大项目 “ 中国典型海相沉积盆地热动力学与油气成藏”(2008-2011)

【16】教育部新世纪优秀人才支持计划项目“我国碳酸盐岩地区有机质高-过成熟的热演化历史及古地温恢复方法探”(2006-2008)

【17】教育部重点基金“沉积盆地古生代碳酸盐岩地区古地温恢复方法探索”(2003-2005)

【18】中石化海相前瞻性项目 “ 中国陆域海相沉积盆地烃源岩成熟度与生烃期次 ” (2007-2010)

【19】中石化“十五”重大基础研究项目“八面河油田成藏组合模式研究”(2000-2003)

【20】中石化西指项目“准噶尔盆地有效烃源岩分布特征、演化历史和油源贡献” (2004-2007)

【21】中石化 “十五”重大项目“郯庐断裂中段两侧盆地烃源岩分布及演化规律研究”(2003-2005)

【22】中石油创新基金“沉积盆地有机质镜质体反射率异常的有机-无机作用成因机理” (2003-2005)

【23】中石油创新基金“深部热力系熵与流体输运热动力学机制研究(CX2000-05)”(2000-2002)

【24】中石油“九五”项目三级课题“柴达木盆地温压场研究”(1996-1998)

【25】中海油重大项目“渤海湾地区优质烃源岩分布预测与油气资源定量评价”(2006-2010)

发表的主要论文

[1] Qiu N S, Zuo Y H, Xu W,   et al., Meso-Cenozoic lithosphere thinning in the eastern North China Craton:   evidence from thermal history of the Bohai Bay Basin, North China. Journal of   Geology, 2016,142: 195-219. [SCI]

[2] Nansheng Qiu,Yinhui Zuo,   Wei Xu, Jian Chang, Meso-Cenzoic thermal structure of the lithosphere in the   Bohai Bay Basin, eastern North China Craton. Geological Journal, 2016,   51:794-804. [SCI]

[3] Liu Y F, Qiu N S, Xie Z   Y, et al., Overpressure compartments in the Central Paleo-Uplift, Sichuan   Basin, Southwest China. AAPG Bulletin, 2016,100(5):867-888[SCI]

[4] Chang J, Li J W, Qiu N S,   Song X Y, Li H L. Multiple cooling episodes in Central Tarim (Northwest   China) revealed by apatite fission track analysis and vitrinite reflectance   data. International Journal of Earth Science, 2016,105(4):1257-1272.[SCI]

[5]Liu Y F, Qiu N S, Chang J,   et al., Distribution and evolution for the Upper Triassic overpressures in   the central of Sichuan Basin, SW China. Journal of Petroleum Science and   Engineering, 2016, 1116-1129. Doi :10.1016/j.petrol2016.08.016

[6]Zhu C Q, Hu S B, Qiu N S,   et al., Geothermal constraints on Emeishan mantle plume magmatism:   paleotemperature reconstruction of the Sichuan Basin, SW China. International   Journal of Earth Science, 2016, DOI: 10.1007/s00531-016-1404-2.

[7]Xu W, Qiu N S, Wang Y. Evolution   of Meso-Cenozoic lithospheric thermal-rheological structure in the Jiyang   sub-basin, Bohai Bay Basin, eastern North China Craton. International Journal   Earth Sciences,2016, Doi :10.10007 /s00531-016-1360-x

[8]Chang J, Qiu N S and Xu W.   Thermal regime of the Tarim Basin, Northwest China: A review. International   Geology Review, 2017,59(1) :49-61.

[9]Xu W, Qiu N S, Heat flow   and destabilized Cratons: a comparative study of the North China, Siberian   and Wyoming Cratons. International Geology Review,2016, doi:10.1080/00206814.   2016.1240050

[10] Li Z, Qiu N S, Chang J,   Yang X M., Precambrian evolution of the Tarim Block and its tectonic affinity   to other major continental blocks in China: New clues from U-Pb geochronology   and Lu-Hf isotopes of detrital zircons. Precambrian Research, 2015, 270:1-21.   [SCI]

[11] Cai C E, Liu Z, Qiu N S,   He J L, Xu S H. Hydrocarbon accumulation in the northwest Chaluhe Fault   Depression, Yitong Basin, North China. Australian Journal of Earth Sciences,   2015, 62:4, 513-527. [SCI]

[12]Qiu N S, Xu W, Zuo Y H,   Chang J. Meso-Cenozoic thermal regime in the Bohai Bay Basin, eastern North   China Craton. International Geology review, 2015, 57(3):271-289[SCI]

[13]Zuo Y H, Qiu N S, Hao Q   Q, et al., Geothermal regime and source rock thermal evolution in the Chagan   sag, Inner Mongolia, northern China. Marine and Petroleum Geology,   2015,59:245-267. [SCI]

[14]Qiu N S, Zuo Y H, Chang   J, Li W Z. Geothermal evidence of Mesozoic and Cenozoic lithospheric thinning   in the eastern North China craton: constraints from the thermal history of   the Jiyang sub-basin, Bohai Bay Basin. Gondwana Research, 2014,   26(3-4):1079-1092. [SCI]

[15]Yu Y X, Tang L J, Yang W   J, Huang T Z, Qiu N Sand Li W G. Salt structures and hydrocarbon   accumulations in the Tarim Basin, northwest China. AAPG Bulletin, 2014,   98(1):135-159[SCI,EI].

[16]Chang J, Roderick B, Yuan   W M, Li W Z, Que Y Q, Qiu N S. Mesozoic cooling history of the “Bachu   Uplift”in the Tarim Basin, China : constraints from zircon fission-track   thermochronology. Radiation Measurements,2014,67:5-14

[17]Qiu N S, Chang J, Zuo Y   H, Wang J Y, Li H L. Thermal evolution and Lower Paleozoic source rocks   maturation in the Tarim Basin, Northwest China. AAPG   Bulletin,2012,96(5):789-821[SCI,EI]

[18]Qiu N S, Chang J, Li W Z,   Yun L, Li H L. New evidence on the Neogene uplift of South Tianshan:   Constraints from the (U-Th)/He and AFT ages of borehole samples of the Tarim   basin and implications for hydrocarbon generation. International J. of Earth   Sciences, 2012, 101(6): 1625-1643[SCI]

[19]Qiu N S, Li H L, Xu E S,   Qin J Z, Zheng L J. Temperature and time effects on free radical   concentration in organic matters: evidence from laboratory pyrolysis   experimental and geological samples. Energy Exploration and Exploitation,   2012, 30(2):311-329 [SCI, EI]

[20] Chang J, Qiu N S, Li J   W. Tectono-thermal evolution of the northwestern Tarim Basin in China:   Constrains from zircon and apatite (U-Th)/He thermochronology. J. of Asian   Earth Sciences, 2012, 61:187-198. [SCI]

[21]Chang J, Qiu N S. Closure   temperature of (U-Th)/He system in apatite obtained from natural drillhole   samples in the Tarim basin and its geological significance. Chinese Science   Bulletin, 2012,57(26): 3482-3490. [SCI, EI]

[22]Tian Y T, Qiu N S, Barry   P K, et al., Detrital zircon (U-Th)/He thermochronometry of the Mesozoic Daba   Shan foreland basin, central China: evidence from timing of post-orogenic   denudation. Tectonophysics, 2012,(570-571):65-77 [SCI]

[23] Zuo Y H, Qiu N S, Zhang   Y, et al., Geothermal regime and hydrocarbon Kitchen evolution of the   offshore Bohai Bay Basin, North China. AAPG Bulletin, 2011,   95(5):749-769[SCI,EI]

[24]Qiu N S, Jiang G, Mei Q   H, et al., The Paleozoic tectonothermal evolution of the Bachu Uplift of the   Tarim Basin, NW China: constraints from (U-Th)/He ages, apatite fission track   and vitrinite reflectance data.J. of Asian Earth Sciences, 2011,   41(6):551-563 [SCI]

[25]Qiu N S, Zuo H Y, Zhou X   H, Li C C. Geothermal regime of the Bohai Offshore Area, Bohai Bay Basin,   North China. Energy Exploration & Exploitation, 2010, 28(5):327-350   [SCI,EI]

[26]Qiu N S, Wang J Y, Mei Q   H, et al., Constraints of (U-Th)/He ages on early Paleozoic tectonothermal   evolution of the Tarim Basin, China. Science China: Earth Sciences, 2010,   53(7): 964-976.[SCI,EI]

[27]邱楠生, Reiners P,梅庆华,姜光,等,   (U-Th)/He年龄在沉积盆地构造-热演化研究中的应用-以塔里木盆地KQ1井为例(中英文对照).地球物理学报,2009,52(7):1825-1835 [SCI].

[28]Qiu N S, Zhang Z H, Xu E   S. Geothermal regime and Jurassic source rocks maturity in the Junggar Basin,   Northwest China. J. of Asian Earth Science, 2008, 31(4-6):464-478[SCI]

[29]Qiu N S, Li H L, Jin Z J,   Zhu Y K. Temperature and time effect on the concentrations of free radicals   in coal: evidence from laboratory pyrolysis experiments. International J. of   Coal Geology, 2007, 69(3): 220-228. [SCI,EI]

[30]邱楠生,苏向光,李兆影,张杰,柳忠泉,李政,张林晔. 郯庐断裂中段两侧坳陷新生代构造-热演化历史研究(中英文对照). 地球物理学报, 2007,50(5):1497-1507 [SCI]

[31]Qiu N S, Zha M, Wang X L,   Yang H B. Tectono-thermal evolution of the Junggar Basin, Northwest China:   Constraints from Ro and apatite fission track modeling. Petroleum   Geosciences, 2005, 11(4):361-372.[SCI]

[32]邱楠生,胡圣标和何丽娟,沉积盆地热体制研究的理论和应用.石油工业出版社, 2004,240pp.

[33]Qiu N S. Geothermal   regime in the Qaidam basin, northeast Qinghai-Tibet Plateau. Geological   Magazine, 2003, 140(6):707-719 [SCI]

[34]Qiu N S, Kang Y S, Jin Z   J. Temperature and pressure field in the Tertiary succession of the Western   Qaidam Basin, Northeast Qinghai-Tibet Plateau, China. Marine and Petroleum   Geology,2003, 20(5):493-507[SCI,EI]

[35]Qiu N S. Tectono-thermal   Evolution of the Qaidam Basin, China-evidence from Ro and Apatite fission   track data. Petroleum Geosciences, 2002, 8(3):279-285 [SCI]

[36]Qiu N S, Wang J Y. The   use of free radicals of organic matter to determine paleogeo- temperature   gradient. Organic Geochemistry, 1998, 28(1/2):77-86[SCI,EI]



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