威远气田成藏期及气源

戴金星

doi:10.11781/sysydz200305473

威远气田成藏期及气源

doi: 10.11781/sysydz200305473

戴金星

中国石油, 勘探开发研究院, 北京, 100083

详细信息

作者简介:
戴金星(1935- ),男(汉族),浙江温州人,中国科学院院士,主要从事天然气地质和地球化学方面的研究.

中图分类号: TE122.3
计量
- 文章访问数: 1036
- HTML全文浏览量: 120
- PDF下载量: 626
- 被引次数: 0
出版历程
- 收稿日期: 2003-07-03
- 修回日期: 2003-07-31
- 刊出日期: 2003-09-25

POOL-FORMING PERIODS AND GAS SOURCES OF WEIYUAN GASFIELD

DAI Jin-xing

Research Institute of Petroleum Exploration and Development, CNPC, Beijing 100083, China

摘要

摘要: 威远气田不仅是中国储集层最老(震旦系灯影组)和烃源岩最老(寒武系九老洞组)的大气田,而且也是世界上地质时代最古老的气藏之一。尽管该气田的储集层和烃源岩时代很早,但它的天然气聚集成藏很晚,是在喜马拉雅期。关于气田的气源研究有多种认识:一种认为是无机成因,因为气藏中的He和Ar含量高,⁴⁰Ar/³⁶Ar平均高达7 000,故认为包括烃气在内的天然气可能是来自地球深部;另一种认为是有机成因气。关于后者又有3种观点:a)灯影组气藏是该组含藻白云岩自生自储的裂解气;b)气源来自或主要来自灯影组气藏的盖层九老洞组;c)灯影组气藏是来自灯影组白云岩和九老洞泥页岩的混合气。作者根据灯影组气藏中δ¹³C₁<δ¹³C₂,δ¹³C₁<-31‰,确定烷烃气是有机成因的;灯影组有机碳平均值仅为0.12%,难成为有效烃源岩,而九老洞组有机碳平均值为0.97%,故烷烃气应来自后者。由于气藏中R/Ra为0.021及0.022,说明氦是壳源无机成因;同时震旦系白云岩含铀、钍矿物低,而九老洞组则较高,故气藏中的He也主要由九老洞组铀、钍衰变来。由此得出灯影组天然气主要来自九老洞组的有机成因气。
- 气源 /
- 气藏类型 /
- 成藏模式 /
- 威远气田
Abstract: Weiyuan gasfield is not only the great gasfield with the oldest reservoirs (the Sinian Dengying Formation) and the oldest source rocks (the Cambrian Jiulaodong Formation) in China but also one of the gas pools with the oldest geologic ages in the world.Though the ages of reservoirs and source rocks in this gasfield were very old, the natural gas in it accumulated and pool-formed very late, in the Himalayan period.There are various opinions concerning the gas origin of the field.One is inorganic origin, which believes the natural gas including hydrocarbon gases maybe come from the deep of the Earth because of the high He and Ar contents in gas pools and the high mean ⁴⁰Ar/³⁶Ar value of up to 7 000.The other is organic origin, which is divided into three viewpoints: a) the gas pools in the Dengying Formation are cracking gases from its own algal dolomite; b)the gas sources mainly come from the caprocks of the Dengying gas pools, that is, the Jiulaodong Formation; c)the gas pools of the Dengying Formation are mixed gases from the Dengying dolomite and the Jiulaodong argillutite.According to δ¹³C₁ < δ¹³C₂ and δ¹³C₁ < -31‰ in the gas pools of the Dengying Formation, it is concluded that the hydrocarbon gases are organic origin.The Dengying Formation has the average TOC value of only 0.12%, so is difficult to become effective source rocks;and the Jiulaodong Formation has the average TOC value of 0.97%, so the hydrocarbon gases should come from it.The R/Ra values of 0.021 and 0.022 in gas pools suggest the crust-source inorganic origin of helium.It the meantime, as the uranium and thorium mineral contents are low in the Sinian dolomite and higher in the Jiulaodong Formation, the helium in gas pools also mainly comes from the uranium and thorium decay of the Jiulaodong Formation.As a result, the natural gas in the Dengying Formation is mainly organic origin gases from the Jiulaodong Formation.
- gas source /
- the type of gas /
- pools pools-forming pattern /
- Weiyuan gasfield

HTML全文

参考文献(19)

[1]	徐永昌,沈平,李玉成. 中国最古老的气藏——四川威远震旦纪气藏[J]. 沉积学报,1989,7(4):1-11.
[2]	包茨.天然气地质学[M]. 北京:科学出版社,1988.361-365.
[3]	戴金星. 天然气在我国未来的能源中占有重要地位[J]. 科技导报,1989,(3):42-44.
[4]	王先彬. 地球深部来源的天然气[J]. 科学通报,1982,27(17):1069-1071.
[5]	瞿光明. 中国石油地质志(卷10)[M]. 北京:石油工业出版社,1989.419-424.
[6]	康竹林,傅诚德,崔涉芬,等. 中国大中型气田概论[M]. 北京:石油工业出版社,2000.67-90,115-122,137-141,146-154,163-177,197-200,204-206,218-221,226-231,238-247,252-257,276-293.
[7]	戴金星,裴锡古,戚厚发. 中国天然气地质学(卷二)[M]. 北京:石油工业出版社,1996.10-15.
[8]	戴金星,宋岩,戚厚发,等. 四川威远气田多源气藏的成因分析[A].天然气地质研究论文集编委会.天然气地质研究论文集[C]. 北京:石油工业出版社,1989.74-80.
[9]	陈文正. 再论四川盆地威远震旦系气藏的气源[J]. 天然气工业,1992,12(6):28-32.
[10]	戴金星. 加强天然气地学研究, 勘探更多大气田[J]. 天然气地球科学,2003,14(1):3-14.
[11]	沈平,徐永昌,王先彬,等. 气源岩和天然气地球化学特征及成气机理研究[M]. 兰州:甘肃科学技术出版社,1991.186-192.
[12]	沈平,王先彬,徐永昌. 天然气同位素组成及气源对比[J]. 石油勘探与开发,1982,(6):34-38.
[13]	戴鸿呜,王顺玉,王海清,等. 四川盆地寒武系-震旦系含气系统成藏特征及有利勘探区块[J]. 石油勘探与开发,1999,26(5):16-20.
[14]	戴金星,王廷栋,戴鸿呜,等. 中国碳酸盐岩大型气田的气源[J]. 海相油气地质. 2000,5(1-2):143-144.
[15]	戴金星. 天然气碳氢同位素特征和各类天然气鉴别[J]. 天然气地球科学,1993,4(2,3).
[16]	Krooss B M, Leythaeuser D, Lillack H. Nitrogen-rich natural gases, qualitative and quantitative aspects of natural gas accumulation in rservoirs[J]. Erdol and Kohle-Erdgas-Petrochemie, 1993, 46(7-8):271-276.
[17]	Littke R, Krooss B, Idic E, et al. Molecular nitrogen in natural gas accumulations: generation from sedimentary organic matter at high temperatures[J]. AAPG Bulletion, 1995,79(3):410-430..
[18]	戴金星,裴锡古,戚厚发. 中国天然气地质学(卷一)[M]. 北京:石油工业出版社,1992.114-116.
[19]	戴金星,李先奇,宋岩. 论中国东部和大陆架二氧化碳气田(藏)及其气的成因类型[A].戴金星,等.天然气地质研究新进展[M]. 北京:石油工业出版社,1997.183-203.