石油与天然气地质 ›› 1986, Vol. 7 ›› Issue (3): 256-260.doi: 10.11743/ogg19860309
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周兴太
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Zhou Xingtai
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摘要:
在利用δ13C 值判断天然气的成因类型时,必须考虑具体地质情况。华北地区的天然气:若δ13C1值小于-55‰,既可能是生物气,也可能是煤田气;若δ13C1值在-35‰至-45‰之间,则属沙河街组生成的气的可能性较大;若δ13C1值大于-40‰,则有属石炭二叠纪煤系气的可能。
Abstract:
A preliminary approach is made on the genetic types of the gases in North China based on the carbon isotope data and geological data.It is suggested that natural gas with δ13C-value less than -55‰ is generally biogenic gas or gasgenerated from coal seam;the one with δ13C-value ranging from -35‰ to 45‰is generally derived from humic-saproplic kerogens of the Tertiary;while theone whose δ13C-value is greater than -40‰ is mainly generated from coal mea-sures(including coal seams and carbonaceous shales)of the Permo-Carboni-ferous.
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链接本文: http://ogg.pepris.com/CN/10.11743/ogg19860309
http://ogg.pepris.com/CN/Y1986/V7/I3/256