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- W2371128138 abstract "Natural gas in Hetianhe Gas Field is mainly sourced from the secondary cracking of liquid hydrocarbon early generated from the Cambrian source rock.In order to investigate the migration and accumulation efficiency and to determine the source area of natural gas,the simulation experiments of hydrocarbon generation from the pyrolysis of source rock in an open system and gas generation from the cracking of crude oil in a closed system were carried out.Based on the experiments,the chemical kinetics models for describing hydrocarbon generation from organic matters and carbon isotope fractionation during methane generation from oil cracking were established,calibrated and then applied to two potential source areas including Bachu Arch and Southwest Depression.The application indicated that both potential source areas have a characteristic of generating aboundant gas in a short period,which is propitious for decreasing gas dissipation during migration and accumulation process.However,two tectonic movements had destroyed the hydrocarbon generated early in Bachu Arch.On the contrary,the tectonic evolvement of Maigaiti Slope dipping to the north and then to the south resulted in the late-generated natural gas in Southwest Depression,because the source rock in this area was at a high tectonic position at early time,which made hydrocarbon accumulate at the high tectonic position of the ancient Maigaiti Slope with a stable tectonic setting before the Himalayan orogeny instead of in the Mazhatage fracture zone located at a low position,avoiding two great tectonic movements.As a result,the natural gas in Hetianhe Gas Field was mainly from the Southwest Depression." @default.
- W2371128138 created "2016-06-24" @default.
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- W2371128138 date "2009-01-01" @default.
- W2371128138 modified "2023-09-25" @default.
- W2371128138 title "A study on the migration and accumulation efficiency and the source area of natural gas in Hetianhe Gas Field of Tarim Basin" @default.
- W2371128138 hasPublicationYear "2009" @default.
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