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A Study of the Migration and Accumulation Efficiency and the Genesis of Hydrocarbon Natural Gas in the Xujiaweizi Fault Depression
Author(s) -
Jijun LI,
Shuangfang LU,
Haitao XUE,
Qiuli HUO,
Qingxia XU
Publication year - 2008
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/j.1755-6724.2008.tb00613.x
Subject(s) - natural gas , hydrocarbon , isotopes of carbon , coal , pyrolysis , source rock , kerogen , caprock , carbon fibers , alkane , chemistry , geology , propane , isotope fractionation , mineralogy , fractionation , environmental chemistry , petroleum engineering , total organic carbon , paleontology , organic chemistry , materials science , structural basin , composite number , composite material
In order to investigate the migration and accumulation efficiency of hydrocarbon natural gas in the Xujiaweizi fault depression, and to provide new evidence for the classification of its genesis, a source rock pyrolysis experiment in a closed system was designed and carried out. Based on this, kinetic models for describing gas generation from organic matter and carbon isotope fractionation during this process were established, calibrated and then extrapolated to geologic conditions by combining the thermal history data of the Xushen‐1 Well. The results indicate that the coal measures in the Xujiaweizi fault depression are typical “high‐efficiency gas sources”, the natural gas generated from them has a high migration and accumulation efficiency, and consequently a large‐scale natural gas accumulation occurred in the area. The highly/over matured coal measures in the Xujiaweizi fault depression generate coaliferous gas with a high δ 13 C 1 value (> −20%) at the late stage, making the carbon isotope composition of organic alkane gases abnormally heavy. In addition, the mixing and dissipation through the caprock of natural gas can result in the negative carbon isotope sequence (δ 13 C 1 >δ 13 C 2 >δ 13 C 3 >δ 13 C 4 ) of organic alkane gases, and the dissipation can also lead to the abnormally heavy carbon isotope composition of organic alkane gases. As for the discovery of inorganic nonhydrocarbon gas reservoirs, it can only serve as an accessorial evidence rather than a direct evidence that the hydrocarbon gas is inorganic. As a result, it needs stronger evidence to classify the hydrocarbon natural gas in the Xujiaweizi fault depression as inorganic gas.