干酪根裂解气和原油裂解气的成因判识方法

陈世加; 付晓文; 马力宁; 陈新领; 张祥

doi:10.11781/sysydz200204364

干酪根裂解气和原油裂解气的成因判识方法

doi: 10.11781/sysydz200204364

1.
西南石油学院, 四川, 南充, 637001
2. 中国石油, 青海石油勘探开发研究院, 甘肃, 敦煌, 736302

基金项目: “九五”国家重点科技攻关项目(96-111-01-06-01);西南石油学院油气藏地质与开发工程国家重点实验项目(PLN99005)

详细信息

作者简介:
陈世加(1964- ),男(汉族),广东大埔人,博士、副教授,主要从事油气地质与地球化学方面的研究与教学工作.

中图分类号: TE122.1
计量
- 文章访问数: 804
- HTML全文浏览量: 84
- PDF下载量: 575
- 被引次数: 0
出版历程
- 收稿日期: 2001-02-19
- 修回日期: 2002-05-21
- 刊出日期: 2002-07-25

GENETIC IDENTIFICATION METHOD OF KEROGEN-CRACKED GASES AND OIL-CRACKED GASES

1.
Southwestern Petroleum Institute, Nanchong, Sichuan 637001 China
2. Qinghai Petroleum Exploration and Development Institute, Dunhuang, Gansu 736302, China

摘要

摘要: 天然气既可来源于干酪根的裂解气,也可来源于原油的裂解气。对于腐泥型有机质,绝大部分天然气是来自源岩生成的原油裂解气,只有部分来自干酪根的裂解气,因此天然气气源研究不仅要指出来自哪套源岩,还需指出它的成因,尤其是高演化地区天然气气源研究。该文以塔里木盆地海相腐泥型天然气为例,根据天然气组成ln(C₂/C₃)与(δ¹³C₂-δ¹³C₃)以及甲烷碳同位素特征判识其成因。塔北地区的干气主要为干酪根晚期裂解气,塔北英买力奥陶系及塔中石炭系的天然气主要为原油裂解气。
- 成因判识 /
- 干酪根裂解气 /
- 原油裂解气 /
- 塔里木盆地
Abstract: Natural gas is not only originated from kerogen cracking,but also from oil cracking. For type Ⅰ or Ⅱ kerogen,most of natural gas is derived from cracking of oil generated from source rock during oil generation peak, only part of natural gas is originated from kerogen cracking directly. Genetic identification of kerogen and oil-cracked gases is very important for the study of natural gas sources and area exploration evaluation, especially for high maturity areas. Natural gas genesis in the North and Central Tarim was studied according to ln(C₂/C₃) and (δ¹³ C₂-δ¹³ C₃)of gas composition. The results showed that dry gas in the North Tarim is mainly kerogen-cracked gas,and gas in the Central Tarim is mainly oil-cracked one.
- genetic identification /
- kerogen-cracked gas /
- oil-cracked gas /
- the Tarim Basin

HTML全文

参考文献(8)

[1]	Burnham A K. A simple kinetic model of petroleum formation and cracking[J]. Geochim Cosmochim Acta, 1989,43:1979-1988.
[2]	Alain A, et al. Genetic and post-genetic molecular and isotopic fractionations in natural gases[J]. Chem Geol, 1995, 126: 281-290.
[3]	黄第藩,等. 塔里木盆地东部天然气的成因类型及其成熟度判识[J].中国科学 D辑,1996,11(5):432-438.
[4]	钱志浩,陈正铺. 塔里木盆地北部天然气成因类型研究[J]. 石油实验地质,1992,14(3):217-226.
[5]	James A T. Correlation of natural gas using the carbon isotopic distribution between hydrocarbon components[J]. AAPG Bull, 1983,67(1): 1176-1193.
[6]	王涵云,杨天宇. 原油热解成气摸拟实验[J]. 天然气工业,1982,(3):28-32.
[7]	陈世加,付晓文,沈照国,等.塔里木盆地中高氮天然气的成因及其与油气运移聚集的关系[J]. 沉积学报,2000,18(4):615-618.
[8]	陈世加,付晓文, 沈照国,等.塔里木盆地塔中地区石炭系储层天然气的成因及地质意义[J].天然气工业,2001,21(1):39-41.