1988
DOI: 10.1016/0009-2541(88)90110-6
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Composition and stable-isotope geochemistry of natural gases from Kansas, Midcontinent, U.S.A.

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Cited by 97 publications
(40 citation statements)
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“…While Ballentine and Sherwood Lollar (2002) stated that gases with 4 He > 0.1% nearly always contain high nitrogen contents, the Australian natural gases generally show a weak positive correlation between 4 He and nitrogen and poor correlation within individual basins (Fig. 11), which does not support an overall strong correspondence between nitrogen and crustal, radiogenic helium nor the concept for a dominant deep metasedimentary or crystalline origin for the associated nitrogen (Jenden et al 1988a(Jenden et al , 1988b. Additionally, the stronger positive linear correlation between R/Ra and 3 He/N 2 (Fig.…”
Section: Nitrogenmentioning
confidence: 92%
“…While Ballentine and Sherwood Lollar (2002) stated that gases with 4 He > 0.1% nearly always contain high nitrogen contents, the Australian natural gases generally show a weak positive correlation between 4 He and nitrogen and poor correlation within individual basins (Fig. 11), which does not support an overall strong correspondence between nitrogen and crustal, radiogenic helium nor the concept for a dominant deep metasedimentary or crystalline origin for the associated nitrogen (Jenden et al 1988a(Jenden et al , 1988b. Additionally, the stronger positive linear correlation between R/Ra and 3 He/N 2 (Fig.…”
Section: Nitrogenmentioning
confidence: 92%
“…The Puguang and Maoba gas fields are located in the Xuanhan-Daxian area in NE Sichuan Basin, having multiple high-quality source rocks, effective cover rocks and James, 1990;Rooney et al, 1995;Tilley and Muehlenbachs, 2006;Jenden et al, 1988).…”
Section: Gas-source Relationshipmentioning
confidence: 99%
“…These Feixianguan-Changxing gases and the Jianglingjiang gases share a common source, most likely in the Upper Permian Longtan Formation. Type III, Sacramento Basin (Jenden et al 1988) T y p e II D e la w a r e / v a l v e r d e b a s in ( R o o n e y e t a l, 1 9 9 5 ) / P r e -c r e ta c e o u s g a s , W C S B ( J a m e s , 1 9 9 0 : T il le y e t a l, 2 0 0 6 ) T y p e II I, N ig e r D e lt a ( R o o n e y e t a l. Other Feixianguan-Changxing gases with low δ 13 C 2 values are distributed below the line of type II kerogen in Figure 6 and far away from the maturity trend line in Figure 7. Because the middle tectonostratigraphic section in the Xuanhan-Daxian region has experienced intensive faulting and folding, the deep seated faults may have provided conduits for fluid migration from several source rocks in different formations, and thus make it possible for multiple source rocks to charge the Feixianguan-Changxing reservoirs in the Puguang and Maoba fields.…”
Section: Comparative Study Of Gases From Different Stratigraphic Intementioning
confidence: 99%
“…It plays an important role in the process of oil/gas generation. Meanwhile, the information about the hydrogen isotopic composition of natural gas is of specific significance [1][2][3][4][5][6], and hydrogen isotopic analysis is one of the most important approaches to studying the process of hydrocarbon generation, the variation trend following hydrocarbon generation, and oil/gas-source correlation [7][8][9][10][11][12][13]. Unsophisticated H isotope analytical technology has long hampered the study and development of hydrogen isotope geochemistry.…”
mentioning
confidence: 99%