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鄂尔多斯盆地富县地区延长组原油生物标志物特征及油源对比

  • 骆垠山 ,
  • 张哨楠 ,
  • 罗小明 ,
  • 邓南涛 ,
  • 王力
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  • 1. 成都理工大学油气藏地质及开发工程国家重点实验室, 成都 610059;
    2. 西南石油大学资源与环境学院, 成都 610500;
    3. 中国石油天然气集团公司青海油田分公司采油二厂开发室, 海西 816400;
    4. 陕西延长石油(集团)有限责任公司研究院, 西安 710075
骆垠山,博士研究生,研究方向为石油地质,电子信箱:dengnt2009@vip.qq.com

收稿日期: 2015-01-15

  修回日期: 2015-09-06

  网络出版日期: 2016-02-04

基金资助

国家科技重大专项(2011ZX05002-001-003)

Biomarker characteristics and oil-source correlation of the Yanchang crude oil in Fuxian area, Ordos Basin

  • LUO Yinshan ,
  • ZHANG Shaonan ,
  • LUO Xiaoming ,
  • DENG Nantao ,
  • WANG Li
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  • 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;
    2. College of Resources and Environmental Sciences, Southwest Petroleum University, Chengdu 610500, China;
    3. Development Section Office of Second Oil Production Plant in Qinghai Oilfield, PetroChina, Haixi 816400, China;
    4. Research Institute of Shaanxi Yanchang Petroleum (Group) Co., Ltd., Xi'an 710075, China

Received date: 2015-01-15

  Revised date: 2015-09-06

  Online published: 2016-02-04

摘要

系统采集鄂尔多斯盆地南部中生界的烃源岩、富县地区延长组原油及油砂样品,对它们的饱和烃馏分进行GC-MS 分析,通过对生物标志物组成特征的研究探讨富县地区延长组原油的来源。结果表明:根据Pr/Ph,8β(H)-补身烷和C30重排藿烷相对含量,鄂尔多斯盆地南部中生界烃源岩可划分为A1、A2、A3、A4、B 类,富县地区延长组原油可划分为Ⅰ、Ⅱ、Ⅲ类,目前发现的原油主要是第Ⅰ类;第Ⅰ类原油来自A1类烃源岩(深湖相沉积相带的长7 油页岩),第Ⅱ类原油来自A2类烃源岩(深湖-半深湖沉积相带的长7 暗色泥岩),第Ⅲ类原油来自A3类烃源岩(半深湖沉积相带的长7 暗色泥岩)。

本文引用格式

骆垠山 , 张哨楠 , 罗小明 , 邓南涛 , 王力 . 鄂尔多斯盆地富县地区延长组原油生物标志物特征及油源对比[J]. 科技导报, 2016 , 34(2) : 129 -134 . DOI: 10.3981/j.issn.1000-7857.2016.2.020

Abstract

Samples of the Mesozoic source rock, crude oil and oil-bearing sands from Fuxian area in the southern Ordos Basin were collected systematically. Gas chromatography-mass spectrometry (GC-MS) was performed on the saturated hydrocarbon fractions extracted from these samples for discussing their biomarker characteristics and crude oil origin. The results show that on the basis of biomarker source parameter distribution, the Mesozoic source rock can be divided into five types (type A1、A2、A3、A4 and B), and the crude oil can be grouped into three types (I, II and III). Type I crude oil is derived from type A1 source rock (Chang 7 oil shale deposited in a reducing, deep lacustrine facies environment). Type II crude oil is sourced from type A2 source rock (Chang 7 dark mudstone deposited in subreducing to reducing, deep or semi-deep lacustrine facies environments). Type III crude oil is sourced from type A3 source rock (Chang 7 dark mudstone deposited in a sub-reducing to reducing, semi-deep lacustrine facies environment).

参考文献

[1] 张文正, 杨华, 杨奕华, 等. 鄂尔多斯盆地长7优质烃源岩的岩石学、 元素地球化学特征及发育环境[J]. 地球化学, 2008, 37(1): 59-64. Zhang Wenzheng, Yang hua, Yang Yihua, et al. Petrology and element geochemistry and development environment of Yanchang Formation Chang-7 high quality source rocks in Ordos Basin[J]. Geochimica, 2008, 37(1) :59-64.
[2] 张文正, 杨华, 李剑锋, 等. 论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用——强生排烃特征及机理分析[J]. 石油勘探与开发, 2006, 33(3): 289-293. Zhang Wenzheng, Yang Hua, Li Jianfeng, et al. Leading effect of highclass source rock of Chang 7 in Ordos Basin on enrichment of low per-meability oil-gas accumulation:hydrocarbon generation and expulsion mechanism Petroleum[J]. Exploration and Development, 2006, 33(3): 289-293.
[3] 杨华, 张文正. 论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用: 地质地球化学特征[J]. 地球化学, 2005, 34(2): 147-154. Yang Hua, Zhang Wenzheng. Leading effect of the seventh member high-quality source rock of Yanchang formation in Ordos Basin during the enrichment of low-penetrating oil-gas accumulation: geology and geochemistry[J]. Geochimica, 2005, 34(2): 147-154.
[4] 张文正, 杨华, 李善鹏. 鄂尔多斯盆地长9-1湖相优质烃源岩成藏意义[J]. 石油勘探与开发, 2008, 35(5): 557-562. Zhang Wenzheng, Yang Hua, Li Shanpeng. Hydrocarbon accumulation significance of Chang_9~1 high-quality lacustrine source rocks of Yan-chang formation, Ordos Basin[J]. Petroleum Exploration and Develop-ment, 2008, 35(5): 557-562.
[5] 段毅, 吴保祥, 张辉, 等. 鄂尔多斯盆地西峰油田原油地球化学特征及其成因[J]. 地质学报, 2006, 80(2): 301-310. Duan Yi, Wu Baoxiang, Zhang Hui, et al. Geochemistry and genesis of crude oils of the Xifeng Oilfield in the Ordos Basin[J]. Acta Geologica Sinica, 2006, 80(2): 301-310.
[6] 郭艳琴, 李文厚, 陈全红, 等. 鄂尔多斯盆地安塞-富县地区延长组-延安组原油地球化学特征及油源对比[J]. 石油与天然气地质, 2006, 27(2): 218-224. Guo Yanqin, Li Wenhou, Chen Quanhong, et al. Geochemical behaviors of oil and oil-source correlation in Yanchang Yan' an formations in An-sai-Fuxian area, Ordos Basin[J]. Oil & Gas Geology, 2006, 27(2): 218-224.
[7] 张晓丽, 段毅, 何金先, 等. 鄂尔多斯盆地华庆地区三叠系延长组长8 油层组油气成藏条件分析[J]. 地质科技情报, 2013, 32(4): 127-132. Zhang Xiaoli, Duan Yi, He Jinxian, et al. Analysis of reservoir forming conditions of chang8 formation in Huaqing Area, Ordos Basin[J]. Geo-logical Science and Technology Information, 2013, 32(4): 127-132.
[8] 张云霞, 陈纯芳, 宋艳波. 鄂尔多斯盆地南部中生界烃源岩特征及油源对比[J]. 石油实验地质, 2012, 34(2): 173-177. Zhang Yunxia, Chen Chunfang, Song Yanbo. Features of mesozoic source rocks and oil-source correlation in southern Ordos Basin[J]. Pe-troleum Geology & Experiment, 2012, 34(2): 173-177.
[9] Moldowan J M, Fago F J, Carlson R M K, et al. Rearranged hopanes in sediments and petroleum[J]. Geochimica et Cosmochimica Acta, 1991, 55(2): 3333-3353.
[10] Philip R P, Gilbert T D. Biomarker distribution in oils predominantly derived from terrigenous source material[M]//Leythaeuser D, Rullkotter J. Advances in Organic Geochemistry 1985. Oxford: Pergamon Press, 1986: 73-84.
[11] Farrimond P, Teln S N. Three series of rearranged hopanes in Toar-cian sediments (northern Italy)[J]. Organic Geochemistry, 1996, 25(3-4): 165-177.
[12] 朱扬明, 钟荣春, 蔡勋育, 等. 川中侏罗系原油重排藿烷类化合物的组成及成因探讨[J]. 地球化学, 2007, 36(3): 253-260. Zhu Yangming, Zhong Rongchun, Cai Xunyu, et al. Composition and origin approach of rearranged hopanes in Jurassic oils of cen tral Sich-uan Basin[J]. Geochimica, 2007, 36(3): 253-260.
[13] 张文正, 杨华, 候林慧, 等. 鄂尔多斯盆地延长组不同烃源岩17α (H)-重排藿烷的分布及其地质意义[J]. 中国科学: 地球科学, 2009, 52(7): 965-974. Zhang Wenzheng, Yang Hua, Hou Linhui, et al. Distribution and geo-logical significance of 17α(H)-diahopanes from different hydrocarbon source rocks of Yanchang formation in Ordos Basin[J]. Science in Chi-na: Earth Sciences, 2009, 52(7): 965-974.
[14] 李相博, 刘显阳, 周世新, 等. 鄂尔多斯盆地延长组下组合油气来源及成藏模式[J]. 石油勘探与开发, 2012, 39(2): 172-180. Li Xiangbo, Liu Xianyang, Zhou Shixin, et al. Hydrocarbon origin and reservoir forming model of the Lower Yanchang Formation, Ordos Ba-sin[J]. Petroleum Exploration and Development, 2012, 39(2): 172-180.
[15] 邓南涛, 张枝焕, 鲍志东, 等. 鄂尔多斯盆地南部延长组有效烃源岩地球化学特征及识别标志[J]. 中国石油大学学报: 自然科学版, 2013, 37(2): 135-145. Deng Nantao, Zhang Zhihuan, Bao Zhidong, et al. Geochemical fea-tures and identification characteristics for efficient source rocks of the Yanchang formation in southern Ordos Basin[J]. Journal of China Uni-versity of Petroleum: Edition of Natural Science, 2013, 37(2): 135-145.
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