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| 1 | Primary migration and secondary alteration of the Upper Paleozoic gas reservoir in Ordos Basin,China―Application of fluid inclusion gases显示文摘The composition of fluid inclusions(FI)often represents the initial geochemical characteristics of palaeo-fluid in reservoir rock.Influence on composition and carbon isotopic composition of gas during primary migration,reservoir-forming and subsequent secondary alterations are discussed through comparing fluid inclusion gas with coal-formed gas and natural gas in present gas reservoirs in the Ordos Basin.The results show that primary migration of gas has significant effect on the molecular but not on the carbon isotopic composition of methane.Migration and diffusion fractionation took place during the secondary migration of gas in Upper Paleozoic gas reservoir according to carbon isotopic composition of methane in FIs.Composition and carbon isotopic composition of natural gas were nearly unchanged after the gas reservoir forming through comparing the FI gases with the natural gas in present gas reservoir. | GONG Se 1,2 ,PENG PingAn 1 ,SHUAI YanHua 3 ,DAI JinXing 3 &ZHANG WenZheng 4 1 Guangzhou Institute of Geochemistry,the Chinese Academy of Sciences,Guangzhou 510640,China 2 Common Wealth Scientific and Research Organization,Petroleum Resources,PO Box 136,North Ryde,New South Wales,1670,Australia 3 Research Institute of Petroleum Exploration and Development,PetroChina,Beijing 100083,China 4 Research Institute of Exploration and Development,Changqing Petroleum Corporation,Xi’an 710021,China | 2008 | Science China Earth Sciences2008，51，S1： | 3 |
| 2 | Ex vivo expanded murine bone marrow cells with a multiple cytokine cocktail retain long-term hematopoietic reconstitution potentials显示文摘 | Yang Q Gong SE Li K | 2005 | Med Sci Monit2005，11，6： | 1 |
| 3 | Simulation experiments on secondary thermal stress of biodegraded bituminous sandstones显示文摘Secondary variation of reservoir is a hot problem in petroleum geochemistry field. Several kinds of secondary variations have taken place after the formation of bituminous sandstones in the Tarim Basin including biodegra-dation, washing, dissipation and secondary thermal stress. Biodegraded bituminous sandstones were used in the experiment. Pyrolysis experiment has been performed in a closed system, simulating secondary thermal stress with continual burial of Silurian bituminous sandstones which may cause the changes in molecular compositions, carbon isotope and physical properties of bituminous sandstones. The results are as follows: (i) Gases are mainly product during the experiment and carbon isotope of gas is lighter. (ii) Yield of C6+ hydrocarbon is relative smaller, and yielded oil is mainly light oil. (iii) Chromatogram character of biodegraded oil-sand is similar to that of saturated hydrocarbon in extracts from present-day bituminous sandstones, (iv) Porosity of bituminous sandstones gradually | GONG Se PENG Ping’an LU Yuhong XIAO Zhongyao JIA Wanglu WANG Zhenqi YU Chiling LIU Dehan LU Jialan LIU Jinzhong | 2004 | Chinese Science Bulletin2004，49，S1： | 1 |
| 4 | Petroleum charge history in the Lunnan Low Uplift, Tarim Basin, China – Evidence from oil-bearing fluid inclusions显示文摘 | Se Gong Simon C. George Herbert Volk Keyu Liu Ping’an Peng | 2007 | Organic Geochemistry2007，，8： | 1 |
| 5 | Innovative fluorescence spectroscopic techniques for rapidly characterising oil inclusions显示文摘 | Liu Keyu George SC Lu Xuesong Gong Se Tian Hua Gui Lili | 2014 | Organic Geochemistry2014，72，： | 1 |
| 6 | Associations of dietary folate, Vitamins B6 and B12 and methianine intake with risk of breast cancer among African American and European American women 显示文摘 | Gong Z Ambrosone CB McCann SE | 2014 | Int J Cancer2014，134，6： | 1 |
| 7 | Cloning and developmental expression of a family of pleurocidin-like antimicrobial peptides from winter flounder,Pleuronecter americanus(walbaum)显示文摘 | Douglas SE Gallant JW Gong Z | 2001 | Dev Comp Immunol2001，25，2： | 1 |
| 8 | The components and carbon isotope of the gases in inclusions in reservoir layers of Upper Paleozoic gas pools in the Ordos Basin,China显示文摘The components and carbon isotope of gases in inclusions are one of the most important geochemical indexes for gas pools.The analysis results of the components and carbon isotope of gases from inclusions in reservoir layers of Upper Palaeozoic gas pools in the Ordos Basin show that most inclusions grown in reservoir sandstone are primary inclusions.There is only a little difference about the components and carbon isotope between the well gases and the secondary inclusions gases.This indicated that the epigenetic change of gas pools is little.This difference between the well gases and the secondary inclusions gases is caused by two reasons:(i)The well gases come from several disconnected sand bodies buried in a segment of depth,while the inclusion gases come from a point of depth.(ii)The secondary inclusions trapped the gases generated in the former stage of source rock gas generation,and the well gases are the mixed gases generated in all the stages.It is irresponsible to reconstruct the palaeo-temperature and palaeo-pressure under which the gas pool formed using carbon dioxide inclusions. | MI JingKui 1 ,DAI JinXing 1 ,ZHANG ShuiChang 1 ,ZHANG WenZheng 2 ,GONG Se 1 &LI XianQing 3 1 Research Institute of Petroleum Exploration and Development,PetroChina,Beijing 100083,China 2 Exploration and Development Research Institute of PetroChina Changqing Oilfield Company,Xi’an 710021,China 3 Key Laboratory of Coal Resources,Ministry of Education,China University of Miningand Technology,Beijing 100083,China | 2008 | Science China Earth Sciences2008，51，S1： | 1 |
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