(Research Instit ute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China)
Received date: 2005-12-05
Revised date: 2005-12-31
Online published: 2006-02-20
The abiogenic gas resource can be classified as major abiogenic gas and minor abiogenic gas,based on the commercial resource and the proportion of natural gas components.In the major abiogenic gas resource,the abiogenic gases(CO_2 and CH_4) take the most part of natural gas,even whole.Whereas,the abiogenic gases concentration(He)in the minor abiogenic gas resource is low,or extreme low. Most of the major abiogenic gas accumulations which have the high concentration of CO_2 and gaseous hydrocarbons are discovered.
DAI Jin-xing . Characteristic of Abiogenic Gas Resource and Resource Perspective[J]. Natural Gas Geoscience, 2006 , 17(1) : 1 -6 . DOI: 10.11764/j.issn.1672-1926.2006.01.1
[1]戴金星,桂明义,黄自林,等.楚雄盆地中东部禄丰-楚雄一带的二氧 化碳气及其成因[J].地球化学,1986,(1):42-49.
[2] 戴金星.云南省腾冲县硫磺塘天然气的碳同位素组成特征和成因[J].科学通 报,1988,(15):1168-1170.
[3] 戴金星,文亨范,宋岩.五大连池地幔成因的天然气[J].石油实验地质,19 92,(2):200-203.
[4] DAI JINXING, SONG YAN, DAI CHUNSEN, et al. Ge- ochemist ry and accumulation of carbon dioxide gases in China[J]. AAPG Bulletin, 1996, 80(10):1615-1626.
[5] 戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重 要进展[J].天然气地球科学,2005,16(2):127-142.
[6] DAI JINXING, YANG SHUFENG, CHEN HANLIN, et al. Geochemistry and occurrence of abiogenic gas accumulations in the Chinese sedimentary basins[J ]. Organic Geochemistry, 2005,36:1664-1688.
[7] MUFFLER F J P, WHITE D E. Origin of CO-2 in the Salton Sea geoth ermal system, southeastern California USA[C]//XXIII, International Geological Congress,1968:185-194.
[8] BROOKS J M. Deep methane maxima in the Northwest Cari- bbea n Sea: possible seepage along the Jamica ridge[J]. Science,1979,206 :1069-1071.
[9] WELHAM J, CRAIG H. Methane and hydrogen in East Pa- cific r ise hydrothermal fluids[J]. Geophys Res Lett,1979, 6(11):829-831.
[10] 郭占谦,王先彬.松辽盆地非生物成因气的探讨[J].中国科学(B辑),1994,24(3 ):303-309.
[11] 郭占谦,刘文龙,王先彬.松辽盆地非生物成因气的成藏特征[J].中国科学(D辑) ,1977,27(2):143-148.
[12] 霍秋立,杨步增,付丽.松辽盆地北部昌德东气藏天然气成因[J].石油勘探与开 发,1998,25(4):17-19.
[13]杜建国.中国天然气中高浓度CO-2成因[J].天然气地球科学,1991,2(5) :199-202.
[14] 何家雄,刘全稳.南海北部大陆架边缘盆地CO-2成因及运聚规律分析与预测[J]. 天然气地球科学,2004,15(1):1-8.
[15] 戴金星,李剑,丁巍伟,等.中国储量千亿立方米以上气田天然气地球化学特征[J ].石油勘探开发,2005,32(4):16-23.
[16] 王先彬,徐胜,陈践发,等.腾冲火山温泉气体组分和氦同位素组成特征[J].科 学通报,1993,38(9):814-817.
[17]李庆忠.打破思想禁锢,重新审视生油理论[J].新疆石油地质,2003,24( 1):75-83.
[18] 徐永昌,沈平,陶明信,等.幔源氦的工业储集和郯庐大断裂带[J].科学通报,1 990,35(12):932-935.
[19] 何家雄,夏斌,刘宝明,等.中国东部及近海陆架盆地CO-2成因及运聚规律与 控制因素研究[J].石油勘探与开发,2005,32(4):42-49.
[20]PARASCHIV D. Variation of non-hydrocarbon constituent of natural gas in different Romanian areas[C]//10th World Petroleum Congress,1979.
[21] Я[KG-*2]КУ[KG-*2]ЧЕНИ В П. Интенсивное газо накопление в недрах[M]. М:Наука, 1984.
[22] 陈荣书.天然气地质学[M].武汉:中国地质大学出版社,1989:264-265.
[23] 戴金星,宋岩,戴春森,等.中国东部无机成因气及其气藏形成条件[M].北京: 科学出版社,1995:107-131,201-202.
[24] 何家雄,胡忠良,麦文,等.综合开发利用南海莺-琼盆地CO-2资源促进中海油跨 越式发展[J].天然气地球科学,2004,15(4):401-405.
[25][KG*8/9]徐永昌,刘文汇,沈平,等.辽河盆地天然气的形成与演化[M].北京:科 学出版社,1993:60-69,134-137.
[26] 冯子辉,霍秋立,王雪.松辽盆地北部氦气成藏特征研究[J].天然气工业,2001 ,21(5):27-30.
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