|本期目录/Table of Contents|

[1]沈朴,金强,张玉明,等.潍北凹陷孔店组天然气成因类型及分布规律[J].地球科学与环境学报,2010,32(03):252-256.
 SHEN Pu,JIN Qiang,ZHANG Yu-ming,et al.Genetic Type and Distribution Rule of Natural Gas of Kongdian Formation in Weibei Sag[J].Journal of Earth Sciences and Environment,2010,32(03):252-256.
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第32卷
期数:
2010年第03期
页码:
252-256
栏目:
基础地质与矿产地质
出版日期:
2010-09-20

文章信息/Info

Title:
Genetic Type and Distribution Rule of Natural Gas of Kongdian Formation in Weibei Sag
文章编号:
1672-6561(2010)03-0252-05
作者:
沈朴1金强1张玉明2张善文12王力3程付启2
(1.中国石油大学 地球资源与信息学院,山东 东营 257061; 2.中国石油化工股份有限公司 胜利油田分公司, 山东 东营 257000; 3.中国石油天然气集团公司冀东油田分公司 勘探开发研究院,河北 唐山 063004)
Author(s):
SHEN Pu1 JIN Qiang1 ZHANG Yu-ming2 ZHANG Shan-wen12 WANG Li3 CHENG Fu-qi2
(1.School of Geo-resources and Information, China University of Petroleum, Dongying 257061, Shandong, China; 2.Shengli Oilfield Company, China Petroleum and Chemical Corporation, Dongying 257000, Shandong, China; 3.Institute of Exploration and Development, Jidong Oilfield Company, China National Petroleum Corporation,Tangshan 063004, Hebei, China)
关键词:
天然气地球化学成因类型分布规律孔店组潍北凹陷
Keywords:
natural gas geochemistry genetic type distribution rule Kongdian Formation Weibei Sag
分类号:
TE122;P618.13
DOI:
-
文献标志码:
A
摘要:
根据天然气组分以及碳同位素和轻烃特征等资料,运用天然气成因理论并结合天然气成因类型判识图版和成藏条件,探讨了潍北凹陷孔店组天然气成因类型及分布规律。结果表明:潍北凹陷天然气CH4体积分数大,重烃体积分数小,非烃组分极少;南部斜坡带的疃4井天然气属生物气;灶户鼻状构造带南部产出的天然气为混有生物气的油型伴生气;灶户鼻状构造带中部地区属典型的油型伴生气;北部洼陷区的东部和南缘产出的天然气具有煤型气,并有油型气混入;以昌1井为代表的北部深洼陷区是煤型气发育的有利地区。总之,潍北凹陷天然气可以划分为生物气、混有生物气的油型伴生气、典型的油型伴生气、混有油型气的煤型气、典型的煤型气等5种成因类型;孔店组天然气类型多样、分布复杂,这些与该区的烃源岩类型、成熟度等因素有关。
Abstract:
Based on natural gas composition, carbon isotope and light hydrocarbon data, genetic type and distribution rule of natural gas of Kongdian Formation in Weibei Sag were discussed with the theory and discriminant diagram of natural gas genetic type and reservoir condition. The results showed that volume contents of CH4, heavy hydrocarbon and nonhydrocarbon were high, low and extremely low for natural gas in Weibei Sag, respectively; natural gas from well Tuan-4 in southern clinoform zone was biogas; natural gas in the southern of Duhu nose tectonic zone was oil type associated gas with biogas; natural gas in the middle of Duhu nose tectonic zone was typical oil type associated gas; natural gas in southern rim and eastern of northern subsag was coal type gas with oil type gas; northern deep subsag was the prospecting area for coal type gas. In general, natural gas in Weibei Sag could be divided into five genetic types, which were biogas, oil type associated gas with biogas, typical oil type associated gas, coal type gas with oil type gas, typical coal type gas; types of natural gas in Kongdian Formation were numerous, distribution was complex, the reasons could be related to hydrocarbon source rock and maturation.

参考文献/References:

[1] 杨显成,李文涛,刘 华,等.精细研究,精心勘探,努力开创天然气和外围地区勘探新局面[R].山东东营:中国石油化工股份有限公司胜利油田分公司地质科学研究院,2007.
[2] 汪泽成,李晓清,程有义,等.潍北盆地天然气分布规律[J].石油实验地质,2002,24(2):130-135.
[3] 李晓清.潍北走滑盆地形成演化与含油气系统[D].北京:中国科学院研究生院,2002.
[4] 宋一涛,廖永胜,王 忠.潍北凹陷孔店组烃源岩评价及油源分析[J].石油与天然气地质,2005,26(6):487-493.
[5] 邱楠生,蔡进功,李善鹏,等.昌潍拗陷潍北凹陷热历史和油气成藏期次[J].地质科学,2003,38(3):413-424.
[6] 程有义,李晓清,汪泽成,等.潍北拉分盆地形成演化及其对成油气条件的控制[J].石油勘探与开发,2004,31(6):32-35.
[7] 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.
[8] 戴金星.天然气碳氢同位素特征和各类天然气鉴别[C]∥戴金星.天然气地质和地球化学论文集(卷二).北京:石油工业出版社,2000:190-228.
[9] 宋 岩,徐永昌.天然气成因类型及其鉴别[J].石油勘探与开发,2005,32(4):24-29.
[10] 宋 岩,陈孟晋,秦胜飞,等.中国天然气地质理论进展[J].石油勘探与开发,2004,31(1):8-11.
[11] Berner U,Faber E.Empirical Carbon Isotope/maturity Relationships for Gases from Algal Kerogens and Terrigenous Organic Matter,Based on Dry,Open-system Pyrolysis[J].Organic Geochemistry,1996,24(10/11):947-955.
[12] 侯读杰,张林晔.实用油气地球化学图鉴[M].北京:石油工业出版社,2003.
[13] 胡惕麟,戈葆雄,张义纲,等.源岩吸附烃和天然气轻烃指纹参数的开发和应用[J].石油实验地质,1990,12(4):375-394.
[14] Snowdon L R,Powell T G.Immature Oil and Condensate; Modification of Hydrocarbon Generation Model for Terrestrial Organic Matter[J].AAPG Bulletin,1982,66(6):775-788.
[15] 张义纲,陈焕疆.论生物气的生成和聚集[J].石油与天然气地质,1983,4(2):160-170.
[16] 陈 英,戴金星,戚厚发.关于生物气研究中几个理论及方法问题的研究[J].石油实验地质,1994,16(3):209-219.
[17] 薛 会,张金川,刘丽芳,等.天然气机理类型及其分布[J].地球科学与环境学报,2006,28(2):53-57.
[18] 戴金星.中国煤成气研究二十年的重大进展[J].石油勘探与开发,1999,26(3):1-10.
[19] 戴金星,夏新宇,秦胜飞,等.中国有机烷烃气碳同位素系列倒转的成因[J].石油与天然气地质,2003,24(1):1-6.

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备注/Memo

备注/Memo:
收稿日期:2009-10-15
基金项目: 国家重点基础研究发展计划项目(2001CB209102)
作者简介: 沈 朴(1984-),男,安徽六安人,工学博士研究生,从事石油地质研究。E-mail:shenpuhdpucn@sina.com
更新日期/Last Update: 2010-09-20