天然气地球科学
高级检索
作者投稿 专家审稿 编辑办公

天然气地球科学

• 天然气地球化学 • 上一篇    下一篇

南华北盆地豫西地区C—P烃源岩地球化学特征

吴伟，王雨涵，曹高社，黄雪峰，刘惟庆   

  1. 河南理工大学，河南 焦作 454000
  • 收稿日期:2014-03-01 修回日期:2014-07-23 出版日期:2015-01-10 发布日期:2015-01-10
  • 作者简介:吴伟(1979-)，男，河南温县人，副教授，博士，主要从事沉积盆地分析与油气勘探研究. E-mail：wei@hpu.edu.cn.
  • 基金资助:

    国家自然科学基金(编号：41102059)；油气资源与探测国家重点实验室(编号：PRP/open-1109)；河南省教育厅自然科学基金(编号：12B170005)联合资助.

The Geochemical Characteristics of The Carboniferous and Permian Source Rocks in the Western Henan,the southern North China Basin

WU Wei，WANG Yu-han，CAO Gao-she，HUANG Xue-feng，LIU Wei-qing   

  1. Henan Polytechnic University,Jiaozuo 454000,China
  • Received:2014-03-01 Revised:2014-07-23 Online:2015-01-10 Published:2015-01-10

PDF (PC)

537

摘要：

针对南华北盆地上古生界油气勘探难题，在油气地质理论的指导下，进行大量踏勘和岩心观察，利用实验室烃源岩有机显微组分鉴定、残余TOC测定、热解分析和镜质组反射率测定等方法，对豫西地区C—P烃源岩进行了有机地球化学特征分析，以期解决豫西地区煤系地层厚度大但尚无油气藏发现的问题。研究发现：烃源岩类型包括炭质泥岩、生物碎屑灰岩、煤岩和暗色泥岩等烃源岩，分别受控于该区的沉积环境演化，地层从下向上表现为1个规模较大的海进—海退旋回，太原组沉积中期为最大海侵时期，对应的烃源岩应为原始条件下最好的烃源岩|烃源岩有机质类型主要以Ⅲ型干酪根为主，生烃潜量极低，远低于良好烃源岩标准，依据残余有机指标评价为差烃源岩或非烃源岩|烃源岩生烃潜量低且倒挂的现象主要由过高热演化程度、大量断裂发育以及不同岩性的CH4吸附能力差异导致。对于整个豫西地区油气勘探而言，保存条件极好或者受区域热事件影响较低的地区可能为潜在的有利区。

关键词: 热演化程度, 烃源岩评价, 豫西地区, 南华北盆地

Abstract:

The purpose of the paper is to solve the problem about the hydrocarbon source rock recognition of Western Henan,the southern North China basin.Based on an extensive survey and observation of drilling cores,organic maceral identification,determination of residual  TOC,thermal analysis and vitrinite reflectance determination of hydrocarbon source rocks were used in the analysis of organic geochemistry feature of the Carboniferous and Permian source rocks in Western Henan.The study found that source rock,including carbonaceous mudstone,bioclastic limestone,coal,and dark mudstone,were influenced by the evolution of sedimentary environment.The best hydrocarbon source rocks originally should be the bioclastic limestone of Taiyuan Formation which deposited in the maximum transgression of the huge Transgressive-regressive cycles.However,the source rocks with type Ⅲ organic matter  and low hydrocarbon generation potential,mainly should be evaluated as poor source rocks or non-hydrocarbon source rock.The inversion phenomenon of low hydrocarbon generation potential was due to high thermal evolution,large amount of fracture development and the difference of CH4 adsorption capacity of different lithology.In Western Henan,the area where has excellent preservation conditions and affected by the regional thermal event slightly should be the favorable exploration area.

Key words: The degree of thermal evolution, Evaluation of hydrocarbon source rocks, Western Henan, The southern North China Basin

中图分类号: 

  • TE122.1+13
［1］Yu Hezhong,Lv Fuliang,Guo Qingxin,et al.Proto-sediment basin types and tectonic evolution in the southern edge of north China Plate[J].Petroleum Geology & Experiment,2005,27(2):111-117.［余和中,吕福亮,郭庆新,等.华北板块南缘原型沉积盆地类型与构造演化[J].石油实验地质,2005,27(2):111-117.］
［2］Xu Hanlin,Zhao Zongju,Lv Fuliang,et al.Tectonic evolution of the Nanhuabei area and analysis about its petroleum potential[J].Geotectonica et Metallogenia,2004,28(4):450-463.［徐汉林,赵宗举,吕福亮,等.南华北地区的构造演化与含油气性[J].大地构造与成矿学,2004,28(4):450-463.］
［3］Lin Xiaoyun,Chen Qianlan,Li Jing.Distribution and geochemical characteristics of permian source rocks in the Southern North China[J].Marine Geology Frontiers,2011,27(4):21-26.［林小云,陈倩岚,李静.南华北地区二叠系烃源岩分布及地球化学特征[J].海洋地质前沿,2011,27(4):21-26.］
［4］Xu Hongjie,Huang Zeguang.The Meso-Cenozoic basinal evolution and hydrocarbon accumulation in the middle and southern part of Southern North China[J].Petroleum Geology & Experiment,2007,29(6):541-544.［徐宏节,黄泽光.南华北中南部中新生代盆地演化与油气成藏分析[J].石油实验地质,2007,29(6):541-544.］
［5］Chen Xinjun,Hu Zongquan,Li Shujun.Later hydrocarbon generation potential of Upper Paleozoic source rock in Southern North China[J].Natural Gas Geoscience,2011,22(4):610-617.［陈新军,胡宗全,李淑筠.华北南部地区上古生界晚期生烃潜力研究[J].天然气地球科学,2011,22(4):610-617.］
［6］Tenger,Gao Changlin,Hu Kai,et al.High quality source rocks of Lower Combination in the Northern Upper-Yangtze area and their hydrocarbon potential[J].Natural Gas Geoscience,2007,18(2):254-259.［腾格尔,高长林,胡凯,等.上扬子北缘下组合优质烃源岩分布及生烃潜力评价[J].天然气地球科学,2007,18(2):254-259.］
［7］Zhai Changbo,Huang Zeguang,Lin Liangbiao.Structure and petroleum analysis of the Tanzhuang-Shenqiu Sag in the south of North China Basin[J].Petroleum Geology & Experiment,2005,27(4):353-359.［翟常博,黄泽光,林良彪.南华北盆地中部凹陷结构分析及油气意义[J].石油实验地质,2005,27(4):353-359.］
［8］Qin Yong,Jin Fali,Quan Biao,et al.Characteristics and mechanism of the Late Mesozoic palaeogeothermal field in Jiaozuo-Jiyuan,Henan,China[J].Coal Geology & Exploration,1993,21(3):16-22.［秦勇,金法礼,权彪,等.焦作一济源地区晚中生代古地热场特征及成因[J].煤田地质与勘探,1993,21(3):16-22.］
［9］Zhao Junfeng,Liu Chiyang,Liu Yongtao,et al.Reconstruction of thermal evolutionary history of the Upper Paleozoic in the Southern North China[J].Oil & Gas Geology,2011,32(1):64-74.［赵俊峰,刘池洋,刘永涛,等.南华北地区上古生界热演化史恢复[J].石油与天然气地质，2011,32(1):64-74.］
［10］Cheng Zhe,Xu Xuhui,Wang Rongxin,et al.Reasons for abnormal thermal evolution of source rocks in Upper Paleozoic,Southern North China[J].Petroleum Geology & Experiment,2011,33(2):142-147.［程喆,徐旭辉,王荣新,等.南华北地区上古生界烃源岩异常热演化因素探讨[J].石油实验地质,2011,33(2):142-147.］
［11］Diao Yujie,Wei Jiuchuan,Li Zengxue,et al.Late Carboniferous-Early Permian sequence stratigraphy and plaeogeography in the Southern North China Basin[J].Journal of Stratigraphy,2011,35(1):88-94.［刁玉杰,魏久传,李增学,等.南华北盆地晚石炭世—早二叠世层序地层学及古地理研究[J].地层学杂志,2011,35(1):88-94.］
［12］Liang Jiwei,Xie Dongning,He Mingxi,et al.Structural style of the Southern North China Basin[J].Petroleum Geology & Experiment,2006,28(5):414-417.［梁积伟,解东宁,何明喜,等.华北盆地南部构造样式分析[J].石油实验地质,2006,28(5):414-417.］
［13］Li Baofang,Li Zhen,Fu Zeming,et al.The depositional filling,coal accumulation characteristics and tectonic evolution of the Late Paleozoic epeiric sea in the south of North China[J].Earth Science:Journal of China University of Geosciences,1989,14(4):367-378.［李宝芳,李祯,付泽明,等.华北南部晚古生代陆表海的沉积充填,聚煤特征和构造演化[J].地球科学,1989,14(4):367-378.］
［14］Wang Zongli,Luo Qiang,Zhao Feng,et al.Favorable pooling conditions of Carboniferous-Permian Formation in Luyi Depression of southern Huabei Basin[J].Natural Gas Geoscience,2005,16(2):194-199.［王宗礼,罗强,赵锋,等.南华北地区鹿邑凹陷石炭—二叠系有利成藏条件分析[J].天然气地球科学,2005,16(2):194-199.］
［15］Zhang Xiaohao,Zhou Dingwu,Zhao Weibo.Research of tectonics style and oil and gas exploration in the western Henan[J].Journal of Northwest University:Natural Science Edition,2007,37(4):647-652.［张小浩,周鼎武,赵伟波.豫西地区构造样式与油气勘探的探究[J].西北大学学报:自然科学版,2007,37(4):647-652.］
［16］Wang Guoshou,Pei Hongzhen,Zhou Zhuoming,et al.Sedimentary characteristics of middle and Lower Permian Series in the western Henan[J].Natural Gas Industry,2003,23(6):24-27.［王果寿,裴红振,周卓明,等.豫西地区中、下二叠统沉积特征[J].天然气工业,2003,23(6):24-27.］
［17］Jiang Youlu,Cha Ming.Geology and Exploration of Oil and Natural Gas［M］.Beijing:Petroleum Industry Press,2006:50-57.［蒋有录,查明.石油天然气地质与勘探［M］.北京:石油工业出版社,2006:50-57.］
［18］Zhou Li.Tectonics Sedimentation and Hydrocarbon Source Rocks Evolution of Late Carboniferous-Middle Permian［D］.Xi′an:Northwest University,2005.［周丽.南华北盆地晚石炭世-中二叠世构造沉积演化与烃源岩评价［D］.西安：西北大学,2005.］
［19］Xu Xianghua,Chen Xinjun,Lei Ming,et al.Exploration prospects of the Carboniferous and Permian in the Southern North China[J].Petroleum Geology & Experiment,2011,33(2):148-153.［徐向华,陈新军,雷鸣,等.华北南部地区石炭—二叠系勘探前景分析[J].石油试验地质,2011,33(2):148-153.］
［20］Xu Huazheng,Hu Zongquan,Zhou Xinke,et al.Lower Paleozoic hydrocarbon-generation history in the mid-south of North China Basin[J].Acta Petrolei Sinica,2005,26(1):31-37.［许化政,胡宗全,周新科,等.华北盆地中南部下古生界的生烃史[J].石油学报,2005,26(1):31-37.］
［21］Yan Fatang,Yao Hefa.Recovery of paleo-temperature and thermal evolution history of Jiyuan Depression,the Southern North China Basin[J].Petroleum Geology and Recovery Efficiency,2006,13(5):28-34.［闫法堂,姚合法.南华北盆地济源凹陷古地温及热演化史恢复[J].油气地质与采收率,2006,13(5):28-34.］
 
[1] 杨亚南，周世新，李靖，李成成，李源遽，马瑜，陈克非. 鄂尔多斯盆地南缘延长组烃源岩地球化学特征及油源对比[J]. 天然气地球科学, 2017, 28(4): 550-565.
[2] 李振生，李建勋，王创，贾超，张交东. 南华北盆地新元古界—下古生界海相烃源岩评价[J]. 天然气地球科学, 2017, 28(11): 1699-1713.
[3] 张交东，曾秋楠，周新桂，刘旭锋，张宏达，王玉芳，毕彩芹，曹建康，杜建波，于明德，张扬，常大宇，王付斌，苗慧心. 南华北盆地太康隆起西部新区上古生界天然气成藏条件与钻探发现[J]. 天然气地球科学, 2017, 28(11): 1637-1649.
[4] 曾艳涛，文志刚，宋换新. 乍得Bongor盆地西部凹陷K组烃源岩地球化学特征研究[J]. 天然气地球科学, 2012, 23(6): 1121-1126.
[5] 顾礼敬, 徐守余, 苏劲, 赵杰, 韩芮. 利用地震资料预测和评价烃源岩[J]. 天然气地球科学, 2011, 22(3): 554-560.
[6] 唐友军, 文志刚, 张超漠, 李军, 朱翠山. 银根—额济纳旗盆地天草凹陷天2井烃源岩生烃潜力评价[J]. 天然气地球科学, 2008, 19(4): 530-536.
[7] 何国源, 谭彦虎, 关平, 李元奎, 张文涛, 杜彬彬. 柴达木盆地西部北区第三系油源研究[J]. 天然气地球科学, 2008, 19(4): 509-518.
[8] 田福清. 二连盆地巴音都兰凹陷烃源岩评价及油源研究[J]. 天然气地球科学, 2008, 19(4): 541-543.
[9] 杨学英，包德宪，丁涛，鲁东升，蔡宁 . 利用井中油气化探资料和孢粉热变指数、有机质类型对松南盆地DB-6井烃源岩综合评价[J]. 天然气地球科学, 2005, 16(1): 73-77.
[10] 李梅;包建平;汪海;张秋茶;郑多明;卢玉红;黄龙藏;. 库车前陆盆地烃源岩和烃类成熟度及其地质意义[J]. 天然气地球科学, 2004, 15(4): 367-378.
[11] 王杰;陈践发. 华北中上元古界烃源岩沉积环境及生烃潜力研究[J]. 天然气地球科学, 2001, 12(3): 27-33.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!