酒西盆地下白垩统赤金堡组烃源岩孢粉相特征及其石油地质意义

doi:10.7623/syxb202011007

石油学报 ›› 2020, Vol. 41 ›› Issue (11): 1376-1387,1395.DOI: 10.7623/syxb202011007

酒西盆地下白垩统赤金堡组烃源岩孢粉相特征及其石油地质意义

马博^1,2,3,4, 吉利明^1,2,3,4, 张明震^1,2, 金培红^1,2, 苑伯超⁵, 龙礼文⁶

1. 中国科学院西北生态环境资源研究院甘肃兰州 730000;
2. 甘肃省油气资源研究重点实验室甘肃兰州 730000;
3. 现代古生物学和地层学国家重点实验室(中国科学院南京地质古生物研究所) 江苏南京 210008;
4. 中国科学院大学北京 100049;
5. 中国石油玉门油田公司勘探开发研究院甘肃酒泉 735019;
6. 中国石油勘探开发研究院西北分院甘肃兰州 730020

收稿日期:2020-02-04 修回日期:2020-09-24 出版日期:2020-11-25 发布日期:2020-12-11
通讯作者: 吉利明,男,1963年1月生,1984年获武汉地质学院学士学位,2005年获中国地质大学(武汉)博士学位,现为中国科学院西北生态环境资源研究院研究员,主要从事油气地球化学与微体古生物学研究工作。Email:jilimin@lzb.ac.cn
作者简介:马博,男,1995年10月生,2017年获兰州大学地质学专业学士学位,现为中国科学院西北生态环境资源研究院矿物学、岩石学、矿床学专业博士研究生,主要从事油气地质与地球化学研究。Email:641477048@qq.com
基金资助:
国家自然科学基金项目（No.41672137）、现代古生物学和地层学国家重点实验室（中国科学院南京地质古生物研究所）基金（No.183111）和甘肃省重点实验室专项（1309RTSA041）资助。

Palynofacies characteristics of source rocks of Lower Cretaceous Chijinbao Formation in Jiuxi Basin and their petroleum geological significance

Ma Bo^1,2,3,4, Ji Liming^1,2,3,4, Zhang Mingzhen^1,2, Jin Peihong^1,2, Yuan Bochao⁵, Long Liwen⁶

1. Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Gansu Lanzhou 730000, China;
2. Gansu Key Laboratory of Petroleum Resources, Gansu Lanzhou 730000, China;
3. State Key Laboratory of Paleobiology and Stratigraphy(Nanjing Institute of Geology and Paleontology, CAS), Jiangsu Nanjing 210008, China;
4. University of Chinese Academy of Sciences, Beijing 10004
9. China;
5. Research Institute of Exploration and Development, PetroChina Yumen Oilfield Company, Gansu Jiuquan 735019, China;
6. PetroChina Research Institute of Petroleum Exploration and Development-Northwest, Gansu Lanzhou 730020, China

Received:2020-02-04 Revised:2020-09-24 Online:2020-11-25 Published:2020-12-11

摘要/Abstract

摘要：

酒西盆地是中国最早开发的陆相含油气盆地之一，下白垩统是盆地主要的烃源岩。通过对旱峡地区下白垩统赤金堡组烃源岩孢粉相进行系统研究，首次识别出木质-丝炭组合（孢粉相A）、无定形组合（孢粉相B）和无定形-木质组合（孢粉相C）3个孢粉相，分别发育在赤金堡组的下部、中部与顶部、上部。孢粉相A以丰富的木质组织和较多的丝炭为特征，孢粉相B以无定形为主要组分，含较多孢粉体和木质组织，孢粉相C以木质和无定形为主。有机质母质来源自下而上表现出从以陆源高等植物输入为主到低等水生生物为主，再到显示混源特征，最终又变为以低等水生生物为主的演化特征。赤金堡组中部及顶部孢粉相B段烃源岩有机质类型以Ⅱ₁型为主，具有较好的生油潜力；而下部和上部孢粉相A段和孢粉相C段烃源岩有机质类型以Ⅲ型为主，生油能力差。孢粉相分析揭示赤金堡组沉积期湖盆经历了断陷形成、强烈扩张、充填收缩和再次凹陷4个演化阶段，沉积环境依次为近源冲积扇—滨浅湖相、半深湖相—深湖相、扇三角洲相和局部半深湖相—深湖相。其中，沉积中期强烈凹陷阶段和末期断陷复活阶段的深水缺氧环境中发育了较好的烃源岩。

关键词: 酒西盆地, 赤金堡组, 烃源岩, 孢粉相, 母质来源, 沉积环境

Abstract:

The Jiuxi Basin is one of the earliest developed continental petroliferous basins in China, dominated by Lower Cretaceous source rocks. Through the systematic research on the palynofacies of source rocks of Lower Cretaceous Chijinbao Formation in Hanxia area, three types of palynofacies were initially identified in this study, i.e., the woody tissue-fusain assemblage (palynofacies A), amorphous assemblage (palynofacies B)and amorphous-wood tissue assemblage (palynofacies C), developed in the lower, middle and top parts of the Chijinbao Formation, respectively. Palynofacies A is characterized by abundant woody tissue and high content of fusain. Palynofacies B is mainly composed of amorphous material, containing much sporinite and woody tissue. Palynofacies C mainly contains woody tissue and amorphous material. From bottom to top, the source of parent material for organic matter shows the evolution from the dominant terrestrial higher plant input to the dominant lower hydrobiont, and then the mixed source characteristics; finally, it is dominant by the lower hydrobiont again. The organic matter of source rocks of the palynofacies B section in the middle and top parts of Chijinbao Formation is dominated by type Ⅱ₁, indicating good oil-generating potential; while that of the palynofacies A section and palynofacies C section in the lower and upper parts is dominated by type Ⅲ, showing poor oil-generating ability. The palynofacies analysis reveals that the lake basin underwent four evolutionary stages during the depositional stage of Chijinbao Formation:formation of fault depression, strong expansion, filling and contraction, and re-sagging. The depositional environment was shown as near-source alluvial fan facies-shore shallow lake facies, semi-deep lake facies-deep lake facies, fan delta facies and local semi-deep lake facies-deep lake facies successively. Among them, good source rocks developed in the deep water anoxic environment during the strong subsidence stage and the resurrection stage of fault depression respectively in the middle and final sedimentary stage.

Key words: Jiuxi Basin, Chijinbao Formation, source rock, palynofacies, organic matter source, sedimentary environment

中图分类号:

TE122.1

马博, 吉利明, 张明震, 金培红, 苑伯超, 龙礼文. 酒西盆地下白垩统赤金堡组烃源岩孢粉相特征及其石油地质意义[J]. 石油学报, 2020, 41(11): 1376-1387,1395.

Ma Bo, Ji Liming, Zhang Mingzhen, Jin Peihong, Yuan Bochao, Long Liwen. Palynofacies characteristics of source rocks of Lower Cretaceous Chijinbao Formation in Jiuxi Basin and their petroleum geological significance[J]. Acta Petrolei Sinica, 2020, 41(11): 1376-1387,1395.

参考文献

[1] 陈建平,陈建军,倪云燕,等.酒泉盆地酒西坳陷油气成藏控制因素与有利勘探方向[J].石油学报,2019,40(11):1311-1330.
CHEN Jianping,CHEN Jianjun,NI Yunyan,et al.Controlling factors of petroleum accumulation and favorable exploration area in the Jiuxi depression,Jiuquan Basin[J].Acta Petrolei Sinica,2019,40(11):1311-1330.
[2] 陈建平,魏军,倪云燕,等.酒泉盆地酒西坳陷主力烃源岩分布及对油气勘探的启示[J].石油学报,2018,39(11):1223-1240.
CHEN Jianping,WEI Jun,NI Yunyan,et al.Determination of main source rocks in the Jiuxi depression of Jiuquan Basin and its implications for oil and gas exploration[J].Acta Petrolei Sinica,2018,39(11):1223-1240.
[3] 陈建军.酒西坳陷的生烃条件与油气源研究[D].成都:西南石油学院,2004.
CHEN Jianjun.Research on the conditions of hydrocarbon-generating and the correlation of oil and source rock from the Jiuxi depression[D].Chengdu:Southwest Petroleum University,2004.
[4] 陈建军,程克明,熊英,等.酒西坳陷下白垩统藻纹层灰岩生烃特征[J].石油勘探与开发,2005,32(6):61-65.
CHEN Jianjun,CHENG Keming,XIONG Ying,et al.Hydrocarbon generation of laminar algal limestone of lower Cretaceous in the Jiuxi depression,NW China[J].Petroleum Exploration and Development,2005,32(6):61-65.
[5] 涂建琪,陈建平,张大江,等.湖相碳酸盐岩烃源岩有机显微组分分类及其岩石学特征——以酒西盆地为例[J].岩石学报,2012,28(3):917-926.
TU Jianqi,CHEN Jianping,ZHANG Dajiang,et al.A petrographic classification of macerals in lacustrine carbonate source rocks and their organic petrological characteristics:a case study on Jiuxi Basin,NW China[J]. Acta Petrologica Sinica,2012,28(3):917-926.
[6] 王崇孝,马国福,周在华.酒泉盆地中、新生代构造演化及沉积充填特征[J].石油勘探与开发,2005,32(1):33-36.
WANG Chongxiao,MA Guofu,ZHOU Zaihua.Structure evolution and sedimentary filling of Jiuquan Basin in Mesozoic-Cenozoic period,NW China[J].Petroleum Exploration and Development,2005,32(1):33-36.
[7] 潘良云,谢结来,李明杰,等.酒泉盆地白垩纪-新生代区域构造演化与油气勘探[J].石油与天然气地质,2006,27(1):62-69.
PAN Liangyun,XIE Jielai,LI Mingjie,et al.Cretaceous-Cenozoic regional tectonic evolution in Jiuquan Basin and petroleum exploration[J].Oil & Gas Geology,2006,27(1):62-69.
[8] 王晓丰,张志诚,郭召杰,等.酒西盆地早白垩世沉积特征及原型盆地恢复[J].石油与天然气地质,2008,29(3):303-311.
WANG Xiaofeng,ZHANG Zhicheng,GUO Zhaojie,et al.Sedimentary characteristics of the Lower Cretaceous and reconstruction of the prototype basin in the Jiuxi Basin[J].Oil & Gas Geology,2008,29(3):303-311.
[9] 薛沛霖,旷红伟,柳永清,等.甘肃酒泉西部地区下白垩统下沟组-中沟组沉积相特征与早白垩世盆地演化[J].地质通报,2013,32(2/3):476-487.
XUE Peilin,KUANG Hongwei,LIU Yongqing,et al.Sedimentary facies of the early cretaceous Xiagou Formation and Zhonggou Formation and basin evolution in western Jiuquan,Gansu Province[J].Geological Bulletin of China,2013,32(2/3):476-487.
[10] 王涛,刘淑文,隗合明,等.热水沉积矿床研究的现状与趋势[J].地球科学与环境学报,2004,26(4):6-10.
WANG Tao,LIU Shuwen,WEI Heming,et al.Resent situations and trend of studies on the hydrothermal sedimentary deposit[J].Journal of Earth Sciences and Environment,2004,26(4):6-10.
[11] 彭楠,旷红伟,柳永清.北祁连-酒西地区早白垩世盆地沉积特征与古地理演化[J].地学前缘,2011,18(4):77-87.
PENG Nan,KUANG Hongwei,LIU Yongqing.Sedimentary evolution and palaeogeography of the Early Cretaceous basins from the northern Qilian Mountains to Jiuxi areas[J].Earth Science Frontiers,2011,18(4):77-87.
[12] 杨经绥,孟繁聪,张建新,等.重新认识阿尔金断裂东段红柳峡火山岩的时代及构造意义[J].中国科学:D辑,2001,31(S1):83-89.
YANG Jingsui,MENG Fancong,ZHANG Jianxin,et al.Recognition of the geologic age of volcanic rock distributed in the eastern end of Hongliuxia Fault and its tectonic significance[J].Science China Earth Sciences,2001,31(S1):83-89.
[13] 陈建平,陈建军,张立平,等.酒西盆地油气形成与勘探方向新认识(一)-基本石油地质条件及生油潜力[J].石油勘探与开发,2001,28(1):19-22.
CHEN Jianping,CHEN Jianjun,ZHANG Liping,et al.New opinions on oil and gas generation and exploration in Jiuxi Basin (I)-Basic petroleum and geological condition and oil-generating potential[J].Petroleum Exploration and Development,2001,28(1):19-22.
[14] 文华国,郑荣才,叶泰然,等.酒西盆地青西凹陷下白垩统沉积特征与有利勘探区预测[J].沉积与特提斯地质,2005,25(4):71-77.
WEN Huaguo,ZHENG Rongcai,YE Tairan,et al.Sedimentary characteristics of Lower Cretaceous strata and prediction of the favourable exploration areas in the Qingxi depression,Jiuxi Basin,Gansu[J].Sedimentary Geology and Tethyan Geology,2005,25(4):71-77.
[15] 薛沛霖.祁连山北部早白垩世沉积盆地演化——以酒西盆地为例[D].荆州:长江大学,2013.
XUE Peilin.The early cretaceous basin evolution of northern Qilian Mountain-an example from Jiuxi Basin[D].Jingzhou:Yangtze University,2013.
[16] 叶得泉,钟筱春,石宝珩.中国北方含油气区白垩系[M].北京:石油工业出版社,1990.
YE Dequan,ZHONG Xiaochun,SHI Baohang.The Cretaceous stratigraphy of petroliferous region in North China[M].Beijing:Petroleum Industry Press,1990.
[17] 邓胜徽,卢远征.甘肃酒泉盆地早白垩世植物化石及其古气候意义[J].地质学报,2008,82(1):104-114.
DENG Shenghui,LU Yuanzheng.Fossil plants from Lower Cretaceous of the Jiuquan Basin,Gansu,Northwest China and their palaeoclimatic implications[J].Acta Geologica Sinica,2008,82(1):104-114.
[18] 郑荣才,王成善,朱利东,等.酒西盆地首例湖相"白烟型"喷流岩——热水沉积白云岩的发现及其意义[J].成都理工大学学报:自然科学版,2003,30(1):1-8.
ZHENG Rongcai,WANG Chengshan,ZHU Lidong,et al.Discovery of the first example of "white smoke type" of exhalative rock (hydrothermal sedimentary dolostone)in Jiuxi Basin and its significance[J].Journal of Chengdu University of Technology:Science & Technology Edition,2003,30(1):1-8.
[19] 郑荣才,文华国,范铭涛,等.酒西盆地下沟组湖相白烟型喷流岩岩石学特征[J].岩石学报,2006,22(12):3027-3038.
ZHENG Rongcai,WEN Huaguo,FAN Mingtao,et al.Lithological characteristics of sublacustrine white smoke type exhalative rock of the Xiagou Formation in Jiuxi Basin[J].Acta Petrologica Sinica,2006,22(12):3027-3038.
[20] 文华国,郑荣才,QING Hairuo,等.酒泉盆地青西凹陷下沟组湖相热水沉积岩流体包裹体特征[J].地质学报,2010,84(1):106-116.
WEN Huaguo,ZHENG Rongcai,QING Hairuo,et al.Characteristics of fluid inclusions in the lacustrine hydrothermal sedimentary rock from the Xiagou Formation,Lower Cretaceous in Qingxi sag,Jiuquan Basin[J].Acta Geologica Sinica,2010,84(1):106-116.
[21] WEN Huaguo,ZHENG Rongcai,QING Hairuo,et al.Primary dolostone related to the Cretaceous lacustrine hydrothermal sedimentation in Qingxi sag,Jiuquan Basin on the northern Tibetan Plateau[J].Science China:Earth Sciences,2013,56(12):2080-2093.
[22] 李明杰.酒泉盆地构造特征与油气勘探[D].北京:中国地质大学,2006.
LI Mingjie.Structure character and petroleum exploration of Jiuquan Basin[D].Beijing:China University of Geosciences,2006.
[23] 国家标准化管理委员会.GB/T 19144-2010沉积岩中干酪根分离方法[S].北京:中国标准出版社,2010.
[24] 国家能源局.SY/T 5125-2014,透射光-荧光干酪根显微组分鉴定及类型划分方法[S].北京:石油工业出版社,2015.
[25] TYSON R V.Sedimentary organic matter:organic facies and palynofacies[M].London:Chapman and Hall,1995.
[26] COMBAZ A.Les kérogènes vus au microscope[M]//DURAND B.Kerogen:Insoluble Organic Matter from Sedimentary Rocks.Paris:Editions Technip,1980:55-112.
[27] 李建国,BATTEN D J.孢粉相:原理及方法[J].古生物学报,2005,44(1):138-156.
LI Jianguo,BATTEN D J.Palynofacies:principles and methods[J].Acta Palaeontologica Sinica,2005,44(1):138-156.
[28] MASRAN T C,POCOCK S A J.The classification of plant-derived particulate organic matter in sedimentary rocks[C]//BROOKS J.Organic Maturation Studies and Fossil Fuel Exploration.London:Academic Press,1981:145-175.
[29] BOUSSAFIR M,GELIN F,LALLIER-VERGÈS E,et al.Electron microscopy and pyrolysis of kerogens from the Kimmeridge Clay Formation,UK:Source organisms,preservation processes,and origin of microcycles[J].Geochimica et Cosmochimica Acta,1995,59(18):3731-3747.
[30] TEWARI R,AWATAR R,PANDITA S K,et al.The Permian-Triassic palynological transition in the Guryul Ravine section,Kashmir,India:implications for Tethyan-Gondwanan correlations[J].Earth-Science Reviews,2015,149:53-66.
[31] ERCEGOVAC M,KOSTI? A.Organic facies and palynofacies:nomenclature,classification and applicability for petroleum source rock evaluation[J].International Journal of Coal Geology,2006,68(1/2):70-78.
[32] TABǎRǎ D,PACTON M,MAKOU M,et al.Palynofacies and geochemical analysis of Oligo-Miocene bituminous rocks from the Moldavidian Domain (Eastern Carpathians,Romania):implications for petroleum exploration[J].Review of Palaeobotany and Palynology,2015,216:101-122.
[33] BATTEN D J.Palynofacies and petroleum potential[C]//JANSONIUS J,MCGREGOR D C.Palynology:Principles and Applications.Dallas:AASP Foundation,1996,3:1065-1084.
[34] 白玮晨.鄂尔多斯盆地东南部长7段孢粉相研究[D].徐州:中国矿业大学,2016.
BAI Weichen.Research on palynofacies of Chang 7 oil-bearing formation in the southeast of Ordos Basin[D].Xuzhou:China University of Mining and Technology,2016.
[35] ZHANG Mingzhen,JI Liming,WU Yuandong,et al.Palynofacies and geochemical analysis of the Triassic Yanchang Formation,Ordos Basin:Implications for hydrocarbon generation potential and the paleoenvironment of continental source rocks[J].International Journal of Coal Geology,2015,152:159-176.
[36] PACTON M,GORIN G E,VASCONCELOS C.Amorphous organic matter-Experimental data on formation and the role of microbes[J].Review of Palaeobotany and Palynology,2011,166(3/4):253-267.
[37] 陈建平,陈建军,倪云燕,等.酒泉盆地酒西坳陷原油油源[J].石油学报,2019,40(7):761-776.
CHEN Jianping,CHEN Jianjun,NI Yunyan,et al.The origin and source of crude oils in the Jiuxi depression,Jiuquan Basin[J].Acta Petrolei Sinica,2019,40(7):761-776.
[38] 马安来,马晓娟,李贤庆,等.有机岩石学在油气勘探中的应用[J].中国煤田地质,2005,17(2):11-15.
MA Anlai,MA Xiaojuan,LI Xianqing,et al.The application of organic petrology on oil and gas exploration[J].Coal Geology of China,2005,17(2):11-15.
[39] 李贤庆,王铁冠,钟宁宁,等.未熟-低熟烃源岩的有机岩石学研究的若干进展[J].地学前缘,2000,7(3):103-110.
LI Xianqing,WANG Tieguan,ZHONG Ningning,et al.Some advances in organic petrology studies on immature source rocks[J].Earth Science Frontiers,2000,7(3):103-110.
[40] S TAPLIN F L.Interpretation of thermal history from color of particulate organic matter-A review[J].Palynology,1977,1(1):9-18.
[41] BATTEN D J.Use of transmitted light microscopy of sedimentary organic matter for evaluation of hydrocarbon source potential[C]//Proceedings of the 4th International Palynological Conference,Lucknow (1976-1977).1980,2:589-594.
[42] COLLINS A.The 1-10 Spore Colour Index (SCI)Scale:a universally applicable colour maturation scale,based on graded,picked palynomorphs[J].Mededelingen Rijks Geologische Dienst,1990,45:39-47.
[43] ALAUG A S,BATTEN D J,AHMED A F.Organic geochemistry,palynofacies and petroleum potential of the Mukalla Formation (Late Cretaceous),Block 16,eastern Yemen[J].Marine and Petroleum Geology,2013,46:67-91.
[44] 朱神照.孢粉化石色变与有机质的演化[J].石油勘探与开发,1983,10(5):7-13.
ZHU Shenzhao.The colour alternation of sporo-pollen fossil and the evolution of organic matters[J].Petroleum Exploration and Development,1983,10(5):7-13.
[45] 任拥军,徐志尧,李福来,等.北部湾盆地乌石凹陷东部地区流沙港组烃源岩孢粉相特征及其意义[J].中国石油大学学报:自然科学版,2016,40(2):34-42.
REN Yongjun,XU Zhiyao,LI Fulai,et al.Palynofacies of source rocks of Liushagang Formation in East Wushi depression,Beibuwan Basin and its significance[J].Journal of China University of Petroleum:Edition of Natural Science,2016,40(2):34-42.
[46] 张淼,陈清华,徐金鲤.东营凹陷沙河街组四段孢粉相特征及其生烃潜力[J].中国石油大学学报:自然科学版,2011,35(6):28-35.
ZHANG Miao,CHEN Qinghua,XU Jinli.Characteristics of palynofacies and its hydrocarbon generation potential of Member 4 of Shahejie Formation in Dongying depression[J].Journal of China University of Petroleum:Edition of Natural Science, 2011,35(6):28-35.

酒西盆地下白垩统赤金堡组烃源岩孢粉相特征及其石油地质意义

Palynofacies characteristics of source rocks of Lower Cretaceous Chijinbao Formation in Jiuxi Basin and their petroleum geological significance

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