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《Chinese Journal of Geophysics》 2003-05
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DISTRIBUTION CHARACTERISTICS OF GEOTEMPERATURE FIELD IN JIYANG DEPRESSION,SHANDONG,NORTH CHINA

GONG YULING 1,2 WANG LIANGSHU 1 LIU SHAOWEN 1 GUO LINGZHI 1 CAI JINGONG 3 1 Department of Earth Sciences, Nanjing University, Nanjing 210093, China 2 Department of Exploration and Information Technology, East China Institute of Technology, Fuzhou 344000, China 3 Geological Science Institute of Shengli Oilfield, Dongying 257015, China  
Based on the analysis of geotemperature data derived from 703 exploration wells in the Jiyang depression of the Shengli oilfield, Shandong, North China, in combination with corresponding geothermal calculations, we present the geothermal field distribution characteristics of this region, which include the plane contour plots of geothermal gradient present day, geotemperature at depths 3km, 4km and 5km, respectively, as well as the top surface of lower Tertiary Es_ 4 formation of Jiyang depression. The results show that the average geothermal gradient present day of the whole Jiyang depression is about 35.5℃/km, the corresponding gradients of its four main sags, i.e. Zhanhua, Dongying, Chezhen and Huimin, are 36.1℃/km, 35.5℃/km, 35.4℃/km, and 34.6℃/km, respectively. While in the Weibei sag, outer flank of the Jiyang depression, it is 35.5℃/km. The distribution of geothermal gradient and geotemperature in the Jiyang depression is mainly governed by its tectonic framework of alternating uplifts and depressions areas. This distribution is also correlated with the basement depth. It is characteristiced by higher temperature in uplifts and lower one in depressions. In addition, those regions of relatively high geothermal gradient are consistent with those of Cenozoic volcanic rocks distribution. The pattern of basement depth of the Jiyang depression, which is also the distributionof uplifts and depressions, is controlled by the lithospheric extension during basin formation. This geodynamic process also accounts for the distribution of volcanic rocks in this region, consequently, the geothermal field characteristics of the Jiyang depression is governed by its tectonic evolution process. In addition, our results also indicate that most of the Es_ 4 formation in the Jiyang depression is still within liquid window of oil and gas.
【Fund】: 国家基础研究发展规划项目 (G19990 43 3 0 2 );; 胜利油田科技攻关项目资助
【CateGory Index】: P544.4
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9 CHEN Wu-zhen1 CHEN Hong-han 1,2 LI Wen-tao3 FENG Yong2 GONG Xue1 XIONG Wan-lin 1(1.Department of Petroleum Geology,Faculty of Earth Resources,China University of Geosciences,Wuhan 430074; 2.Lanzhou Center for Oil and Gas Resources,Institute of Geology and Geophysics,CAS,Lanzhou 730000; 3.Institute of Geological Science Research,Shengli Oilfield,SINOPEC,Dongying,Shandong 257015);Study on Differentiation of Secondary Hydrocarbon Generation for the Carboniferous-Permian Source Rocks in the Eastern Linqing Depression[J];Acta Sedimentologica Sinica;2012-01
10 LEI Chao1,REN Jianye1,WU Meilian2,QI Peng1 and HU Desheng1(1.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074,Hubei,China;2.Institute of Petroleum Exploration and Development,Tarim Oilfield,Kuerle 841000,Xinjiang,China);THE QUANTIFICATIONAL ANALYSIS OF DEVELOPMENT AND EVOLVEMENT OF GUXI NEGATIVE INVERSION FAULT AND ITS SIGNIFICANCE IN PETROLEUM GEOLOGY IN JIYANG DEPRESSION[J];Geotectonica Et Metallogenia;2008-04
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1 JIA Hong-yi~(1,2),YANG Chang-chun~1,YU Jian-guo~2,WANG Jin-duo~2 (1.Institute of Geology and Geophysics,CAS,Beijing 100029,China; 2.Geophysical Research Institute of Shengli Oil field Ltd.Co.,Dongying 257022,China);Structural transition and hydrocarbon accumulation during early eocene in Dongying sag of the Jiyang depression[A];[C];2008
2 LI Zong-Xing~(1,2),ZHAO Ping~(1*),SUN Zhan-Xue~3,YUAN Yu-Song~4,ZHAO Yong-Qing~5 1 Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics, Chinese Academy of Sciences,Beijing 100029,China 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China 3 East China College of Technology,Fuzhou,Jiangxi 344000,China 4 Exploration and Production Research Institute,SINOPEC,Beijing 100083,China 5 Exploration Department of South Company of Prospecting,SINOPEC,Chengdu 610041,China;A study on maturity evolution of Lower Silurian marine hydrocarbon source rocks and thermal history in the southern Jianghan basin[A];[C];2011
3 JIA Hong-yi1, 2, YANG Chang-chun1, YU Jian-guo2, WANG Jin-duo2(1. Institute of Geology and Geophysics, CAS, Beijing 100029, China;2.Geophysical Research Institute of Shengli Oilfield Ltd. Co., Dongying 257022, China);Structural transition and hydrocarbon accumulation during early eocene in Dongying sag of the Jiyang depression[A];[C];2007
4 Li Jiawei Qiu Nansheng Chang Jian;Apatite Fission Track Response to Tectono-thermal Evolution of the Tazhong Area in Tarim Basin,China[A];[C];2011
5 WANG Jiyang~1,HU Shengbiao~1,PANG Zhonghe~1,HE Lijuan~1,ZHAO Ping~1,ZHU Chuanqing~1,RAO Song~(1,2), TANG Xiaoyin~(1,2),KONG Yanlong~(1,2),LUO Lu~(1,2),LI Weiwei~(1,2) 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.University of Chinese Academy of Sciences,Beijing 100049,China;Estimate of Geothermal Resources Potential for Hot Dry Rock in the Continental Area of China[A];[C];2013
6 WANG Jiyang~1,HU Shengbiao~1,PANG Zhonghe~1,HE Lijuan~1,ZHAO Ping~1,ZHU Chuanqing~1,RAO Song~(1,2), TANG Xiaoyin~(1,2),KONG Yanlong~(1,2),LUO Lu~(1,2),LI Weiwei~(1,2) 1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China 2.University of Chinese Academy of Sciences,Beijing 100049,China;Estimate of Geothermal Resources Potential for Hot Dry Rock in the Continental Area of China[A];[C];2013
7 LI ZongXing~(1,2),XU Ming~(2,3*),ZHAO Ping~1,SUN ZhanXue~4 & ZHU ChuanQing~(2,3) 1 Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 2 Graduate University of Chinese Academy of Sciences,Beijing 100049,China; 3 State Key Laboratory of Lithospheric Evolution,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China; 4 East China Institute of Technology,Fuzhou 344000,China;Geothermal regime and hydrocarbon kitchen evolution in the Jianghan Basin[A];[C];2014
8 WangXin;JiangYoulu;Liu Hua;Wang Xiaorui;School of Geosciences in China University of Petroleum;;Characteristics of tectonic evolution and its control action on source rock in Jiyang Depression[A];[C];2015
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