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The components and carbon isotope of the gases in inclusions in reservoir layers of Upper Paleozoic gas pools in the Ordos Basin,China
Authors:JingKui Mi  JinXing Dai  ShuiChang Zhang  WenZheng Zhang  Se Gong  XianQing Li
Affiliation:1.Research Institute of Petroleum Exploration and Development,PetroChina,Beijing,China;2.Exploration and Development Research Institute of PetroChina Changqing Oilfield Company,Xi’an,China;3.Key Laboratory of Coal Resources, Ministry of Education,China University of Miningand Technology,Beijing,China
Abstract: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.
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