鄂尔多斯盆地北缘书记沟中元古界长城系烃源岩地质特征

冯娟萍; 姚韦卓; 欧阳征健; 李文厚

doi:10.16152/j.cnki.xdxbzr.2024-06-002

您当前的位置：

首页 >

文章列表页 >

鄂尔多斯盆地北缘书记沟中元古界长城系烃源岩地质特征

鄂尔多斯盆地岩相古地理与沉积演化 | 更新时间：2024-12-16

- 鄂尔多斯盆地北缘书记沟中元古界长城系烃源岩地质特征
- Geological characteristics of source rocks of Mesoproterozoic Changchengian System in Shujigou area of the northern margin of Ordos Basin
- 西北大学学报（自然科学版） 2024年54卷第6期页码：950-960
- 作者机构：
  
  1.西安科技大学　地质与环境学院，陕西　西安　 710054
  2.煤炭绿色开采地质研究所，陕西　西安　 710054
  3.兰州城市学院　培黎石油工程学院，甘肃　兰州　 730070
  4.西北大学　地质学系，陕西　西安　 710069
- 作者简介：
  
  冯娟萍，女，博士，副教授，从事沉积学和石油地质学研究，fengjuanping@163.com。
  欧阳征健，男，博士，副教授，从事构造地质学研究，ouyangzhengjian@126.com
- 基金信息：
  
  国家自然科学基金青年项目(41502107)
- DOI：10.16152/j.cnki.xdxbzr.2024-06-002
  中图分类号： P618.13
- 纸质出版日期：2024-12-25，
  
  收稿日期：2024-07-15，
- 稿件说明：
移动端阅览
冯娟萍, 姚韦卓, 欧阳征健, 等. 鄂尔多斯盆地北缘书记沟中元古界长城系烃源岩地质特征[J]. 西北大学学报（自然科学版）, 2024,54(6):950-960.

FENG JUANPING, YAO WEIZHUO, OUYANG ZHENGJIAN, et al. Geological characteristics of source rocks of Mesoproterozoic Changchengian System in Shujigou area of the northern margin of Ordos Basin. [J]. Journal of northwest university (natural science edition), 2024, 54(6): 950-960.
冯娟萍, 姚韦卓, 欧阳征健, 等. 鄂尔多斯盆地北缘书记沟中元古界长城系烃源岩地质特征[J]. 西北大学学报（自然科学版）, 2024,54(6):950-960. DOI： 10.16152/j.cnki.xdxbzr.2024-06-002.

FENG JUANPING, YAO WEIZHUO, OUYANG ZHENGJIAN, et al. Geological characteristics of source rocks of Mesoproterozoic Changchengian System in Shujigou area of the northern margin of Ordos Basin. [J]. Journal of northwest university (natural science edition), 2024, 54(6): 950-960. DOI： 10.16152/j.cnki.xdxbzr.2024-06-002.

摘要

是否发育有效烃源岩是鄂尔多斯盆地中元古界成藏的关键。采用野外地质考察、显微薄片鉴定和地球化学分析等研究方法，对鄂尔多斯盆地北缘书记沟中元古界长城系阿古鲁沟组烃源岩地质特征展开研究。研究表明，阿古鲁沟组烃源岩为黑色含粉砂质泥质碳质板岩及黑色含电气石云母碳质千枚岩，原岩为黑色含砂页岩。烃源岩有机碳含量高，为0.34%～9.56%，平均值为3.3%；有机质类型以I型和Ⅱ1型为主；

变化范围为3.57%～4.68%，平均值为4.09%；

max

值为404～562 ℃，处于以生成干气为主的过成熟阶段。稀土元素配分模式为轻稀土微富集、轻重稀土分异不明显的略微右倾型；δCe值为0.74～0.92，表现出Ce负异常；δEu变化范围比较大，为0.95～4.83，指示阿古鲁沟组烃源岩当时沉积时处于还原-氧化过渡环境。稀土元素、微量元素含量指示阿古鲁沟组烃源岩形成于滨浅海-台后盆地沉积环境。当时，气候温暖潮湿，间或出现短暂偏干热气候变化，水体具有一定深度，能量较小，为与北侧广海沟通有限的较闭

塞贫氧-厌氧、咸水-微咸水还原环境，这种条件非常有利于烃源岩的形成。

Abstract

The development of effective source rocks is the key to Mesoproterozoic hydrocarbon accumulation in Ordos area. In this paper

the geological characteristics of the Agulugou Formation source rocks in Shujigou area were studied by means of field geological investigation

microscopic section identification and geochemical analysis. Researches show that the source rocks of Agulugou Formation are carbonaceous slate and phyllite

and the original rocks are black sand-bearing shale. The contents of organic carbon in the source rocks are high

and the value ranges from 0.34% to 9.56%

with an average of 3.3%. The types of organic matter are I and II1 kerogen. The value of

ranges from 3.57% to 4.68%

and the

max

value is from 404 ℃ to 562 ℃. These results show that the thermal evolution of source rocks is high

and is in the over-mature stage. The distribution pattern of rare earth elements is a slightly right-leaning pattern with slight enrichment of LREE and no obvious differentiation of LREE and HREE. The δCe values range from 0.74 to 0.92

showing a negative Ce anomaly

and the δEu range is relatively large

ranging from 0.95 to 4.83

that indicates that the deposit of the source rocks formed in a transitional environment from reduction to oxidation. The content of trace elements indicates that the Agulugou Formation deposited in a back-plateform basin with a water depth of less than 250 m

and the sedimentary facies were fluvial-shore sands

shallow water carbonaceous-argillaceous deposits of the barrier island. Combined with the above research

it shows that the Mesoproterozoic source rocks in the study area are mainly good-excellent source rocks formed in the reduction-oxidation environment

and the hydrocarbon generation geological conditions are favorable.

关键词

书记沟中元古界烃源岩地质特征地球化学

Keywords

Shujigou areaMesoproterozoicsource rocksgeological characteristicsgeochemistry

references

HUNT J M. Generation of gas and oil from coal and other terrestrial organic matter[J]. Organic Geochemistry, 1991, 17(6): 673-680.

KLEMME H D, ULIMSHEK G F. Effective petroleum source rocks of the world: Stratigraphic distribution and controlling factors[J]. AAPG Bulletin, 1991, 75(12): 1809-1851.

王铁冠, 韩克猷. 论中-新元古界的原生油气资源[J]. 石油学报, 2011, 32(1): 1-7.

WANG T G, HAN K Y. On Meso-Neoproterozoic primary petroleum resources[J]. Acta Petrolei Sinica, 2011, 32(1): 1-7.

DICKAS A B. Worldwide distribution of Precambrian hydrocarbon deposits[J]. Geoscience Wisconsin, 1986, 11: 8-13.

KUZNETSOV V G. Riphean hydrocarbon reservoirs of the Yurubchen-Tokhom zone, Lena-Tunguska Province, NE Russia[J]. Journal of Petroleum Geology, 1997, 20(4): 459-474.

MURRAY G E, KACZOR M J, MCARTHUR R E. Indigenous Precambrian petroleum revisited[J]. AAPG Bulletin, 1980, 64(10): 1681-1700.

童晓光, 徐树宝. 世界石油勘探开发图集(独联体地区分册)[M]. 北京: 石油工业出版社, 2004.

GAHUSHKTN Y I, YAKOVLEV G E, KUPRIN V F. Catagenesis of Riphean and Vendian deposits in western Bashkoetostan and realization of the hydrocarbon potential their organic matter: Numerical estimates[J]. Geochemistry International, 2004, 42(1): 61-76.

O’DELL M, LAMERS E. Subsurface uncertainty management and development optimization in the harweel cluster, South Oman[J]. SPE Reservoir Evaluation and Engineering, 2005, 8(2): 164-168.

刘淑萱. 深层油气藏储集层与相态预测[M]. 北京: 石油工业出版社, 1992.

杜汝霖. 燕山地区震旦亚界及其矿产[J]. 河北地质学院学报, 1978, 2: 5-15.

DU R L. Mineral resources of Sinian in Yanshan area[J]. Journal of Hebei Geology College, 1978, 2: 5-15.

张长根, 熊继辉. 燕山西段震旦亚界油气生成问题探讨[J]. 华东石油大学学报(自然科学版), 1979(1): 88-102.

ZHANG C G, XIONG J H. Discussion on hydrocarbon-generation of Sinian in the western Yanshan area[J]. Journal of China University of Petroleum (Edition of Natural Science), 1979(1): 88-102.

黄醒汉, 张一伟. 燕山西段震旦亚界、下古生界含油性[J]. 华东石油大学学报(自然科学版), 1979(1): 103-114.

HUANG X H, ZHANG Y W. Oil-bearing property of Sinian suberatherm and Lower Paleozoic in the western Yanshan area[J]. Journal of China University of Petroleum (Edition of Natural Science), 1979, 1: 103-114.

王铁冠. 燕山地区震旦亚界油苗的原生性及其石油地质意义[J]. 石油勘探与开发, 1980(2): 34-52.

WANG T G. The primary property of Sinian suberathem oil seepages and its petroleum geological significance[J]. Petroleum Exploration and Developmemt, 1980(2): 34-52.

王铁冠. 论燕山地区震旦亚界油苗的原生性[M]. 北京: 科学出版社, 1984.

高耀斌, 郝石生, 卢学军, 等. 燕山地区中-上元古界油苗及其油源研究[J]. 石油大学学报(自然科学版), 1991, 15(1): 1-8.

GAO Y B, HAO S S, LU X J, et al. Study on oil source of the middle-upper Proterozoic layer in Yanshan area[J]. Journal of the University of Petroleum, 1991, 15(1): 1-8.

陈践发, 孙省利. 华北新元古界下马岭组富有机质层段的地球化学特征及成因初探[J]. 天然气地球科学, 2004, 15(2): 110-114.

CHEN J F, SUN S L. Preliminary study of geochemical characteristics and formation of organic matter rich stratigraphy of Xiamaling Formation of later Proterozoic in north China[J]. Natural Gas Geoscience, 2004, 15(2): 110-114.

高德臻, 李龙, 魏荣珠. 内蒙古固阳福顺店一带渣尔泰山群褶皱构造研究[J]. 地球科学, 2000, 25(3): 247-252.

GAO D Z, LI L, WEI R Z. Fold structure of Zhaertaishan group in Fushundain, Guyang County, Inner Mongolia[J]. Earth Science, 2000, 25(3): 247-252.

郭彦如, 赵振宇, 张月巧, 等. 鄂尔多斯盆地海相烃源岩系发育特征与勘探新领域[J]. 石油学报, 2016, 37(8): 939-951.

GUO Y R, ZHAO Z Y, ZHANG Y Q, et al. Development characteristics and new exploration areas of marine source rocks in Ordos Basin[J]. Acta Petrolei Sinica, 2016, 37(8): 939-951.

冯娟萍, 丁雪峰, 欧阳征健. 鄂尔多斯盆地南缘中元古界长城系烃源岩地球化学特征[J]. 西安科技大学学报, 2015, 35(6): 749-754.

FENG J P, DING X F, OUYANG Z J. Geochemical characteristics of Mesoproterozoic Erathem Changchengian System source rocks in the south margins of Ordos Basin[J]. Journal of Xi'an University of Science and Technology, 2015, 35(6): 749-754.

冯娟萍, 欧阳征健, 范萌萌. 鄂尔多斯盆地北缘固阳县北中元古界长城系烃源岩地质特征及意义[J]. 地质科学, 2020, 55(4): 1044-1055.

FENG J P, OUYANG Z J, FAN M M. Geological characteristics and significance of source rocks of Mesoproterozoic Changchengian System in north of Guyang County of the northern margin of Ordos Basin[J]. Chinese Journal of Geology, 2020, 55(4): 1044-1055.

冯娟萍, 欧阳征健, 周义军, 等鄂尔多斯地区中元古界“拗拉槽”的重新厘定[J]. 西北大学学报(自然科学版), 2018, 48(4): 587-592.

FENG J P, OUYANG Z J, ZHOU Y J, et al. Revision of the Mesoproterozoic Aulacogen in Ordos Area[J]. Journal of Northwest University (Natural Science Edition), 2018, 48(4): 587-592.

康明, 岳长成, 刘孝峰, 等. 内蒙古渣尔泰地区中生代火山岩地球化学特征及构造环境分析[J]. 岩石学报, 2017, 33(6): 1685-1704.

KANG M, YUE C C, LIU X F, et al. Geochemical characteristics and tectonic setting for Mesozoic volcanoic rocks in the Zhaertai area, Inner Mongolia[J]. Acta Petrologica Sinica, 2017, 33(6): 1686-1704.

内蒙古自治区地质矿产局. 内蒙古自治区岩石地层[M]. 武汉: 中国地质大学出版社, 1996.

谭林, 朱坤玉, 周盛德, 等. 内蒙古渣尔泰山群岩相古地理[M]. 北京: 地质出版社, 1991.

潘永胜, 胡建中, 陈志勇, 等. 内蒙古固阳地区渣尔泰山群层序地层学研究[J]. 内蒙古地质, 2001(3): 1-10.

PAN Y S, HU J Z, CHEN Z Y, et al. The study on the sequence stratigraphy of Zhaertaishan group in Guyang Area, Inner Mongolia[J]. Geology of Inner Mongolia, 2001(3): 1-10.

PETERS K E. Guideline of evaluating petroleum source rock using programmed pyrolysis[J]. AAPG Bulletin, 1986, 70(3): 318-329.

JARVIE D M. Total organic carbon (TOC) analysis[M]//ROBERT K. Source and migration processes and evaluation techniques. Tulsa: AAPG, 1991: 113-118.

NICHOLLS G D. Trace elements in sediments: An assessment of their possible utility as depth indicators[J]. Marine Geology, 1967, 5: 539-555.

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 W Z, YANG H, YANG Y H, et al. Petrology and element geochemistry and development environment of Yanchang Formation Chang 7 high quality source rocks in Ordos Basin[J]. Geochemica, 2008, 37(1): 59-64.

陶树, 汤达祯, 周传祎, 等. 川东南—黔中及其周边地区下组合烃源岩元素地球化学特征及沉积环境意义[J]. 中国地质, 2009, 36(2): 397-403.

TAO S, TANG D Z, ZHOU C Y, et al. Element geochemical characteristics of the lower assemblage hydrocarbon source rocks in southeast Sichuan-central Guizhou (Chuandongnan-Qianzhong) region and its periphery areas and their implications to sedimentary environments[J]. Geology in China, 2009, 36(2): 397-403.

付金华, 李士祥, 徐黎明, 等. 鄂尔多斯盆地三叠系延长组长7段古环境恢复及意义[J]. 石油勘探与开发, 2018, 45(6): 936-946.

FU J H, LI S X, XU L M, et al. Paleo-sedimentary environment restoration and its significance of Chang 7 member of triassic Yanchang Formation in Ordos Basin, NW China[J]. Petroleum exploration and development, 2018, 45(6): 936-946.

CAMPBELL A C, PALMER M R, KLINKHAMMER G P, et al. The chemistry of hot springs on the Mid-Atlantic Ridge[J]. Nature, 1988, 335: 514-519.

腾格尔, 刘文汇, 徐永昌, 等. 海相地层无机参数与烃源岩发育环境的相关研究：以鄂尔多斯盆地为例[J]. 石油与天然气地质, 2005, 26(4): 411-421.

TENGER , LIU W H, XU Y C, et al. Study on relation between inorganic parameters in marine deposits and developmental environment of hydrocarbon source rocks: Taking Ordos Basin as an example[J]. Oil and Gas Geology, 2005, 26(4): 411-421.

EMERSON S R, HUESTED S S. Ocean anoxia and the concentrations of molybdenum and vanadium in seawater[J]. Marine Chemistry, 1991, 34, 177-196.

WIGNALL P B. Black shales (Oxford Monographs on Geology and Geophysics)[M]. Oxford: Oxford University Press, 1994.

KIMURA H, WATANABE Y. Ocean anoxia at the Precambrian-Cambrian boundary[J]. Geology, 2001, 29(11): 995-998.

HATCH J R, LEVENTHAL J S. Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (missourian) stark shale member of the dennis limestone, Wabaunsee County, Kansas, USA[J]. Chemical Geology, 1992, 99(1/3): 65-82.

JONES B J, MANNING D A C. Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J]. Chemical Geology, 1994, 111(1/4): 111-129.

RIMMER S M. Geochemical paleoredox indicators in Devonian-Mississippian black shales, Central Appalachian Basin (USA)[J]. Chemical Geology, 2004, 206(3/4): 373-391.

邓小亮, 林良彪, 余瑜, 等. 川西北剑阁地区栖霞组地球化学及古环境意义[J]. 成都理工大学学报(自然科学版), 2020, 47(2): 198-209.

DENG X L, LIN L B, YU Y, et al. Geochemical characteristics and palaeo environmental significance of Qixia Formation in Jiange, Sichuan, China[J]. Journal of Chengdu University of Technology (Science and Technology Edition), 2020, 47(2): 198-209.

MYERS K J, WIGNALL P B. Understanding Jurassic organic-rich mudrocks, new concepts using Gamma-ray spectrometry and palaeoecology: Examples from the Kimmeridge clay of Dorset and the Jet rock of Yorkshire[M]//LEGGETTJ K, ZUFFA G G. Marine clastic sedimentology. Dordrecht: Springer, 1987: 172-189.

WIGNALL P B, TWITCHETT R J. Oceanic anoxia and the end Permian mass extinction[J]. Science, 1996, 272(5265): 1155-1158.

腾格尔, 刘文汇, 徐永昌, 等. 无机地球化学参数与有效烃源岩发育环境的相关研究[J]. 地球科学进展, 2005, 20(2): 193-200.

TENGER , LIU W H, XU Y C, et al. Correlative study on parameters of inorganic geochemistry and hydrocarbon source rocks formative environment[J]. Advances in Earth Science, 2005, 20(2): 193-200.

LERMAN A, IMBODEN D, GAT J. Physics and chemistry of lakes[M]. Berlin: Springer, 1995.

ZERFASS H, LAVINA E L, SCHULTZ C L, et al. Sequence stratigraphy of continental Triassic strata of southernmost Brazil: A contribution to southwestern Gondwana palaeogeography and palaeoclimate[J]. Sedimentary Geology, 2003, 161(1/2): 85-105.

JANZ H, VENNEMANN T W, TORSTEN W, et al. Isotopic composition (O, C, Sr, and Nd) and trace element ratios (Sr/Ca, Mg/Ca) of Miocene marine and brackish ostracods from north Alpine Foreland deposits (Germany and Austria) as indicators for palaeoclimate[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 225(1/4): 216-247.

冯娟萍, 欧阳征健, 李文厚. 鄂尔多斯地区中新元古代构造沉积演化研究[J]. 西北大学学报(自然科学版), 2020, 50(4): 634-643.

FENG J P, OUYANG Z J, LI W H. Tectonic and depositional evolution of Meso-Neo Proterozoic in Ordos Area[J]. Journal of Northwest University (Natural Science Edition), 2020, 50(4): 634-643.

乔秀夫, 姚培毅, 王成述, 等. 内蒙古渣尔泰群层序地层及构造环境[J]. 地质学报, 1991, 1: 1-16.

QIAO X F, YAO P Y, WANG C S, et al. Sequence stratigraphy and tectonic environment of the Chaertai Group, Inner Mongolia[J]. Acta Geologica Sinica, 1991, 1: 1-16.

浏览量

下载量

CSCD

文章被引用时，请邮件提醒。

提交

工具集

关联资源

浅埋煤层烧变岩地球化学与变质矿物相特征

土壤硒和重金属元素分布规律及污染评价——以陕西紫阳为例

冀西南中元古界长城系赵家庄组叠层砂质MISS组合的发现及意义

鄂尔多斯盆地南部延长组长7段致密油成藏条件与富集主控因素

鄂尔多斯地区中元古界“拗拉槽”的重新厘定