Southern North China Basin,Neoproterozoic and Lower Palaeozoic,Marine,Effective gas source rock,Organic geochemistry,"/> 南华北盆地新元古界—下古生界海相烃源岩评价

天然气地球科学

• 天然气地球化学 • 上一篇    下一篇

南华北盆地新元古界—下古生界海相烃源岩评价

李振生,李建勋,王创,贾超,张交东   

  1. 1.合肥工业大学资源与环境工程学院,安徽 合肥 230009;2.中国地质科学院,北京 100037
  • 收稿日期:2017-05-22 修回日期:2017-07-15 出版日期:2017-11-10 发布日期:2017-11-10
  • 作者简介:李振生(1976-),男,河北遵化人,副研究员,博士,主要从事基础油气地质学和沉积岩石学研究.E-mail:lizs@ustc.edu.cn;lizhensh@163.com.
  • 基金资助:

    国家自然科学基金(编号:41372194,41172117);中国地质调查局地质调查项目(编号:1211302108023-1)联合资助.

Comprehensive analysis of Neoproterozoic and Lower Palaeozoicmarine source rocks in southern North China Basin

Li Zhen-sheng,Li Jian-Xun,Wang Chuang,Jia Chao,Zhang Jiao-dong
 
  

  1. 1.School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China;
    2.Chinese Academy of Geological Sciences,Beijing 100037,China
  • Received:2017-05-22 Revised:2017-07-15 Online:2017-11-10 Published:2017-11-10

摘要:

南华北盆地是我国油气勘探历史较长,但仍未取得工业性突破的地区之一,新元古界—下古生界深层油气是值得深入探索的海相天然气新地层和新领域,从有机地球化学和沉积相的角度分析新元古界—下古生界的烃源岩条件,为下一步天然气勘探决策提供地质依据。有机地球化学评价表明南华北盆地新元古界—下古生界有机质类型为腐泥型(I型),热演化程度达到高—过成熟阶段,尚有一定的生气潜力;新元古界—下古生界包括6套区域性烃源岩层,青白口系刘老碑组差烃源岩、崔庄组差—好烃源岩和寒武系马店组好—很好烃源岩、张夏—崮山组及凤山组差—中等烃源岩的有效分布区为南华北盆地南缘及东南缘的较深水陆棚或开阔台地和次深海斜坡相沉积区;青白口系张渠组—魏集组及史家组差—很好烃源岩和中奥陶统差—中等烃源岩的有效分布区为东北部较深水台地以及西南部浅海陆棚相沉积区。马店组暗色泥页岩及泥质白云岩为最优的烃源岩,张渠组—魏集组碳酸盐岩和泥页岩、崔庄组泥页岩、刘老碑组泥页岩次之,中奥陶统、张夏组—崮山组盐岩及九里桥组—九顶山组碳酸盐岩为较差的烃源岩。
 

关键词: 南华北盆地, 新元古界&mdash, 下古生界, 海相, 有效气源岩, 有机地球化学

Abstract:

Deep hydrocarbon resources in Neoproterozoic-Lower Paleozoic Erathem of southern North China Basin,which is one of the areas without industrial hydrocarbon accumulations discovered during a long history of oil and gas exploration,will be probably the new formation and domain worthy of further exploration of marine natural gas.In this paper,the comprehensive analysis of organic geochemistry and sedimentary facies of marine source rocks in Neoproterozoic and Lower Palaeozoic Erathem would provide a geological basis for decision on further natural gas exploration.It is suggested by organic geochemical evaluation that the organic matter was sapropel type(type I)with high to over mature stage of thermal evolution degree,and six sets of regional potential hydrocarbon source rocks were optimized,which is in the peak stage of natural gas generation at present.Effective hydrocarbon source rocks of Liulaobei and Cuizhuang formations of Qingbaikouan System,and Madian and Zhangxia-Gushan Formations of Cambrian System,which respectively were poor,poor-good,good-very good and poor-middle grade of source rocks,developed in southern and southeastern part of southern North China Basin which were sediments of deeper-water neritic shelf facies,open platform facies and bathyal slope facies;while that of Zhangqu-Weiji Formation of Qingbaikouan System and middle Ordovician,which respectively were poor-very good and poor-middle grade of source rocks,developed in the northeast part which were sediments of deeper-water open platform facies as well as neritic shelf facies.The best source rocks were mud shale and argillaceous dolomite of Madian Formation,the second were mud shale of Cuizhuang and Liulaobei Formations and carbonate and muddy mud shale of Zhangqu-Weiji Formation,and the poorer were carbonate of Zhangxia-Gushan Formation,middle Ordovician as well as Jiayuan-Jiudingshan Formation.
 

Key words: Southern North China Basin')">

中图分类号: 

  • TE122.1+15


[1]Zhao Junfeng,Liu Chiyang,He Zhengguang,et al.Thermal evolution degree and its hydrocarbon geological implications of the main strata series in the southern north China craton[J].Petroleum Geology & Experiment,2010,32(2):101-107.[赵俊峰,刘池洋,何争光,等.南华北地区主要层系热演化特征及其油气地质意义[J].石油实验地质,2010,32(2):101-107.]
[2]He Mingxi,Du Jianbo,Wang Rongxin,et al.The study of exploration prospect of marine natural gas in the Neoproterozoic-Lower Paleozoic on the south margin of the north China platform[J].Petroleum Geology & Experiment,2009,31(2):154-159.[何明喜,杜建波,王荣新,等.华北南缘新元古界—下古生界海相天然气前景初探[J].石油实验地质,2009,31(2):154-159.]
[3]Liang Bing,Liu Hongyu.Sedimentary basin evolution and geological elements of unconventional oil and gas reservoirs in Fuyang area,Anhui Province[J].Journal of Palaeogeography,2014,16(2):179-192.[梁兵,刘宏宇.安徽阜阳地区沉积盆地演化与非常规油气藏的地质要素构成[J].古地理学报,2014,16(2):179-192.]
[4]Wei Xiaoliang,Zhang Jinchuan,Dang Wei,et al.Characteristics and gas-bearing property of transitional shale in Well Mouye 1[J].Science Technology and Engineering,2016,16(26):42-50.[魏晓亮,张金川,党伟,等.牟页1井海陆过渡相页岩发育特征及其含气性[J].科学技术与工程,2016,16(26):42-50.]
[5]Ling Fan,Zhu Yuzhen,Zhou Minglei,et al.Shale gas potential assessment of Changshan Uplift area in southern North China Basin by using wide field electromagnetic method[J].Geophysical and Geochemical Exploration,2017,41(2):369-376.[凌帆,朱裕振,周明磊,等.广域电磁法在南华北盆地长山隆起页岩气资源潜力评价中的应用[J].物探与化探,2017,41(2):369-376.]
[6]Huang Wenming,Liu Shugen,Xu Guosheng,et al.Characteristics of paleo oil pools from Sinian to Lower Paleozoic in southeastern margin of Sichuan Basin[J].Geological Review,201,57(2):285-299.[黄文明,刘树根,徐国盛,等.四川盆地东南缘震旦系—古生界古油藏特征[J].地质论评,201,57(2):285-299.]
[7]Dai Jinxing.Pool-forming periods and gas sources of Weiyuan Gasfield[J].Petroleum Geology & Experiment,200,25(5):473-479.[戴金星.威远气田成藏期及气源[J].石油实验地质,200,25(5):473-480.]
[8]Cai C,Li K,Anlai M,et al.Distinguishing Cambrian from Upper Ordovician source rocks:Evidence from sulfur isotopes and biomarkers in the Tarim Basin[J].Organic Geochemistry,2009,40(7):755-768.
[9]Ma Y,Zhang S,Guo T,et al.Petroleum geology of the Puguang sour gas field in the Sichuan Basin,SW China[J].Marine and Petroleum Geology,2008,25(4/5):357-370.
[10]Wu L,Liao Y,Fang Y,et al.The study on the source of the oil seeps and bitumens in the Tianjingshan structure of the northern Longmen Mountain structure of Sichuan Basin,China[J].Marine and Petroleum Geology,201,37(1):147-161.
[11]Yu B,Dong H,Widom E,et al.Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin,Northwest China:Lmplications for depositional setting and tectonic history[J].Journal of Asian Earth Sciences,2009,34(3):418-436.
[12]Wang Tieguan,Han Keyou.On Meso-Neoproterozoic primary petroleum resources[J].Acta Pertolei Sinica,201,32(1):1-7.[王铁冠,韩克猷.论中—新元古界的原生油气资源[J].石油学报,201,32(1):1-7.]
[13]Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation,distribution,resource potential and discovery of the Sinian-Cambrian giant gas field,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):278-293.[邹才能,杜金虎,徐春春,等.四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.]
[14]Wei Guoqi,Du Jinhu,Xu Chunchun,et al.Characteristics and accumulation modes of large gas reservoirs in Sinian-Cambrian of Gaoshiti-Moxi region,Sichuan Basin[J].Acta Petrolei Sinica,2015,36(1):1-12.[魏国齐,杜金虎,徐春春,等.四川盆地高石梯—磨溪地区震旦系—寒武系大型气藏特征与聚集模式[J].石油学报,2015,36(1):1-12.]
[15]Zheng Ping,Shi Yuhua,Zou Chunyan,et al.Natural gas sources in the Dengying and Longwangmiao Formations in the Gaoshiti-Maoxi area,Sichuan Basin[J].Natural Gas Industry,2014,34(3):50-54.[郑平,施雨华,邹春艳,等.高石梯—磨溪地区灯影组、龙王庙组天然气气源分析[J].天然气工业,2014,34(3):50-54.]
[16]Wang Pengwan,Chen Ziliao,He Xunyun,et al.Accumulation of Lower Cambrian Niutitang shale gasand prediction of potential area in Qiannan Sag[J].Natural Gas Geoscience,201,22(3):518-524.[王鹏万,陈子炓,贺训云,等.黔南坳陷下寒武统页岩气成藏条件与有利区带评价[J].天然气地球科学,201,22(3):518-524.]
[17]Han Shuangbiao,Zhang Jinchuan,Li Yuxi,et al.The optimum selecting of shale gas well location for geological investigation in Niutitang Formation in Lower Cambrian,northern Guizhou area[J].Natural Gas Geoscience,201,24(1):182-187.[韩双彪,张金川,李玉喜,等.黔北地区下寒武统牛蹄塘组页岩气地质调查井位优选[J].天然气地球科学,201,24(1):182-187.]
[18]Luo Chao,Liu Shugen,Sun Wei,et al.Basic characteristics of shale gas in the Lower Cambrian Niutitang Formation in the Upper Yangtze Region:Taking Nangao section in Danzhaias an example[J].Natural Gas Geoscience,2014,25(3):453-470.[罗超,刘树根,孙玮,等.上扬子区下寒武统牛蹄塘组页岩气基本特征研究——以贵州丹寨南皋剖面为例[J].天然气地球科学,2014,25(3):453-470.]
[19]Dong Dazhong,Wang Yuman,Li Xinjing,et al.Breakthrough and prospect of shale gas exploration and development in China[J].Natural Gas Industry,2016,36(1):19-32.[董大忠,王玉满,李新景,等.中国页岩气勘探开发新突破及发展前景思考[J].天然气工业,2016,36(1):19-32.]
[20]Dai Jingxing,Liu Deliang,Cao Gaoshe,et al.Cambrian Source Rock in the South Margin of the North China Basin[M].Beijing:Petroleum Industry Press,2005.[戴金星,刘德良,曹高社,等.华北盆地南缘寒武系烃源岩[M].北京:石油工业出版社,2005.]
[21]Dai Jinxing,Liu Deliang,Cao Gaoshe.Discovery of marine muddy hydrocarbon source rocks in the southern margin of the north China block and its siginficance for gas exploration[J].Geological Review,200,49(3):322-329.[戴金星,刘德良,曹高社.华北陆块南部下寒武统海相泥质烃源岩的发现对天然气勘探的意义[J].地质论评,200,49(3):322-329.]
[22]Chen Qilin,Bai Yunlai,Liao Jianbo,et al.Distribution characteristics and exploring significance of Cambrian source rock in the deep of Ordos Basin,China[J].Natural Gas Geoscience,2015,26(3):397-407.[陈启林,白云来,廖建波,等.鄂尔多斯盆地深层寒武系烃源岩展布特征及其勘探意义[J].天然气地球科学,2015,26(3):397-407.]
[23]He Mingxi,Wang Min,Qiu Ronghua,et al.Polyphased Superposition Basins and Oil-Gas Resource in the Southern North China Block[M].Beijing:Geological Publishing House,2012.[何明喜,王敏,邱荣华,等.南华北多期复合叠合盆地与油气[M].北京:地质出版社,2012.]
[24]He Zhiliang,Xu Xuhui,Dai Shaowu et al.Evolution and Petroleum Prospect of East Qinling and Dabie Orogenic Belt and Both Sides of Basins[M].Wuhan:China University of Geosciences Press,2013.[何治亮,许旭辉,戴少武,等.东秦岭—大别造山带及两侧盆地演化与油气勘探[M].武汉:中国地质大学出版社,2013.]
[25]Tao Shizhen,Liu Deliang,Li Changwei,et al.Exploration frontiers of unexplored shale layer in new district,North China block:Source rock and its gas system of Madian Formation of Lower Cambrian in the southern part of North China block(SNCB)[J].Natural Gas Geoscience,2014,25(11):1767-1780.[陶士振,刘德良,李昌伟,等.华北陆块新区新层页岩气潜在勘探新领域——南华北下寒武统马店组烃源岩及其含气系统[J].天然气地球科学,2014,25(11):1767-1780.]
[26]Yang D B,Xu W L,Xu Y G,et al.U-Pb ages and Hf isotope data from detrital zircons in the Neoproterozoic sandstones of northern Jiangsu and southern Liaoning Provinces,China:Lmplications for the Late Precambrian evolution of the southeastern North China Craton[J].Precambrian Research,2012,(216-219)(9):162-176.
[27]Liu Yongqing,Gao Linzhi,Liu Yanxue,et al.Zircon U-Pb dating for the Earliest Neoproterozoic mafic magmatism in the southern margin of the North China Block[J].Chinese Science Bulletin,2006,51(19):2375-2382.[柳永清,高林志,刘燕学,等.徐淮地区新元古代初期镁铁质岩浆事件的锆石U-Pb 定年[J].科学通报,2005,50(22):2514-2521.]
[28]Gao L Z,Zhang C H,Liu P J,et al.Reclassification of the Meso-and Neoproterozoic chronostratigraphy of North China by SHRIMP Zircon ages[J].Acta Geologica Sinica-English Edition,2009,83(6):1074-1084.
[29]Wang Qinghai,Yang Debin,Xu Wenliang.Neoproterozoic basic magmatism in the southeast margin of North China Craton:Evidence from whole-rock geochemistry,U-Pb and Hf isotopic study of zircons from diabase swarms in the Xuzhou-Huaibei area of China[J].Science China:Earth Sciences,201,55(9):1461-1479.[王清海,杨德彬,许文良.华北陆块东南缘新元古代基性岩浆活动——徐淮地区辉绿岩床群岩石地球化学、年代学和Hf同位素证据[J].中国科学:地球科学,201,41(6):796-815.]
[30]Hu Guohui,Zhao Taiping,Zhou Yanyan,et al.Meso-Neoproterozoic sedimentary formation in the southern margin of the North China Craton and its geological implications[J].Acta Petrologica Sinica,201,29(7):2491-2507.[胡国辉,赵太平,周艳艳,等.华北克拉通南缘中—新元古代沉积地层对比研究及其地质意义[J].岩石学报,201,29(7):2491-2507.]
[31]Zhang H F,Zhang J,Zhang G W,et al.Detrital zircon U-Pb,Lu-Hf,and O isotopes of the Wufoshan Group:Implications for episodic crustal growth and reworking of the southern North China craton[J].Precambrian Research,2016,273:112-128.
[32]He Y,Zhao G,Sun M,et al.SHRIMP and LA-ICP-MS zircon geochronology of the Xiong’er volcanic rocks:Implications for the Paleo-Mesoproterozoic evolution of the southern margin of the North China Craton[J].Precambrian Research,2009,168(3/4):213-222.
[33]Zhao Taiping,Zhou Meifu,Jin Chengwei,et al.Discussionon age of the Xiong’er Group in southern margin of North China Craton[J].Chinese Journal of Geology,200,36(3):326-334.[赵太平,周美夫,金成伟,等.华北陆块南缘熊耳群形成时代讨论[J].地质科学,200,36(3):326-334.]
[34]Cui M,Zhang B,Zhang L.U-Pb dating of baddeleyite and zircon from the Shizhaigou diorite in the southern margin of North China Craton:Constrains on the timing and tectonic setting of the Paleoproterozoic Xiong’er group[J].Gondwana Research,201,20(1):184-193.
[35]Zhao Taiping,Zhai Mingguo,Xia Bin,et al.Zircon U-Pb SHRIMP dating for the volcanic rocks of the Xiong’er Group:Constraints on the initial formation age of the cover of the north China Craton[J].Chinese Science Bulletin,2004,49(23):2495-2502.[赵太平,翟明国,夏斌,等.熊耳群火山岩锆石 SHRIMP 年代学研究:对华北克拉通盖层发育初始时间的制约[J].科学通报,2004,49(22):2342-2349.]
[36]Gao L Z,Liu P J,Yin C Y,et al.Detrital Zircon Dating of Meso-and Neoproterozoic rocks in north china and its implications[J].Acta Geologica Sinica-English Edition,201,85(2):271-282.
[37]Hu G,Zhao T,Zhou Y.Depositional age,provenance and tectonic setting of the proterozoic Ruyang Group,southern margin of the north China Craton[J].Precambrian Research,2014,246:296-318.
[38]Li Meng,Wang Chao,Wang Zhaofei.Depositional age and geological implications of the Ruyang Group in the southwestern margin of the North China Craton:Evidence from detrital zircon U-Pb ages[J].Chinese Journal of Geology,201,48(4):1115-1139.[李猛,王超,王钊飞.华北克拉通西南缘汝阳群沉积时代及其地质意义—来自碎屑锆石 U-Pb 年龄的证据[J].地质科学,201,48(4):1115-1139.]
[39]Su Wenbo,Li Huaikun,Xu Li,et al.Luoyu and Ruyang Group at the south margin of the North China Craton(NCC)should belong in the Mesoproterozoic Changchengian System:Direct constraints from the LA-MC-ICPMS U-Pb age of the tuffite in the Luoyukou Formation,Ruzhou,Henan,China[J].Geological Survey and Research,201,35(2):96-108.[苏文博,李怀坤,徐莉,等.华北克拉通南缘洛峪群—汝阳群属于中元古界长城系——河南汝州洛峪口组层凝灰岩锆石 LA-MC-ICPMS U-Pb 年龄的直接约束[J].地质调查与研究,201,35(2):96-108.]
[40]Zhu X Y,Chen F K,Li S Q,et al.Crustal evolution of the North Qinling terrain of the Qinling Orogen,China:Evidence from detrital zircon U-Pb ages and Hf isotopic composition[J].Gondwana Research,201,20(1):194-204.
[41]Yan Guohan,Ma Fang,Cai Jianhui,et al.SHRIMP U-Pb Zircon ages of the trachyte in the Dahongkou Formation,Luanchuan Group,southern margin of the North China Craton[C]//National Symposium on Petrology and Geodynamics.Beijing,2010:289-290.[阎国翰,马芳,蔡剑辉,等.华北克拉通南缘栾川群大洪口组碱性粗面岩锆石SHRIMP U-Pb年龄及其意义[C]//2010年全国岩石学与地球动力学研讨会.北京,2010:289-290.]
[42]Wang X L,Jiang S Y,Dai B Z,et al.Age,geochemistry and tectonic setting of the Neoproterozoic(ca 830 Ma)gabbros on the southern margin of the North China Craton[J].Precambrian Research,201,190(1-4):35-47.
[43]Gao Wei,Zhang Chuanheng,Wang Ziqiang.The discovery of large-scale acanthomorphic acritarch assemblage on the southern margin of North China old land and an analysis of its paleogeographic environment[J].Geology in China,201,38(5):1232-1243.[高维,张传恒,王自强.华北古陆南缘豫西新元古代大型疑源类及古地理环境分析[J].中国地质,201,38(5):1232-1243.]
[44]Yin Chongyu,Gao Linzhi,Liu Pengju,et al.Biostratigraphic Sequence and Stratigraphic Division of Neoproterozoic in China[M].Beijing:Science Press,2015.[尹崇玉,高林志,刘鹏举,等.中国新元古代生物地层序列与年代地层划分[M].北京:科学出版社,2015.]
[45]Gao Linzhi,Yin Chongyu,Wang Ziqiang.New view of the Neoproterozoic strata on the southern margin of the North China platform[J].Geological Bulletin of China,200,21(3):130-135.[高林志,尹崇玉,王自强.华北地台南缘新元古代地层的新认识[J].地质通报,200,21(3):130-135.]
[46]Su Wenbo.Revision of the Mesoproterozoic chronostratigraphic subdivision both of North China and Yangtze Cratons and the relevant issues[J].Earth Science Frontiers,2016,23(6):156-185.[苏文博.华北及扬子克拉通中元古代年代地层格架厘定及相关问题探讨[J].地学前缘,2016,23(6):156-185.]
[47]Zhou Hongrui,Wang Ziqiang.Feature and tectono-paleogeography evolution of the southern margin of the North China continent in Mesoproterozoic and Neoproterozoic Era[J].Geoscience,1999,13(3):261-267.[周洪瑞,王自强.华北大陆南缘中、新元古代大陆边缘性质及构造古地理演化[J].现代地质,1999,13(3):261-267.]
[48]Zhai M,Hu B,Zhao T,et al.Late Paleoproterozoic-Neoproterozoic multi-rifting events in the North China Craton and their geological significance:A study advance and review[J].Tectonophysics,2015,662:153-166.
[49]Xu Huazheng,Zhou Xinke,Gao Jinhui.Sedimentary characteristics and petroliferous condition of Lower Paleozoic inland sea in south-middle North China Basin[J].Acta Petrolei Sinica,2005,26(5):10-15,23.[许化政,周新科,高金慧.华北盆地中南部早古生代沉积特征及油气成藏条件[J].石油学报,2005,26(5):10-15,23.]
[50]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.]
[51]Hao Yiwei,Luo Mansheng,Xu Zenglian,et al.Division of sedimentary basins and its tectonic evolution in North China from Neoproterozoic to Mesozoic[J].Earth Science,2014,39(8):1230-1242.[郝奕玮,骆满生,徐增连,等.华北陆块新元古代-中生代沉积盆地划分及其构造演化[J].地球科学,2014,39(8):1230-1242.]
[52]Cao Gaoshe,Song Mingshui,Liu Deliang,et al.Sedimentary environment and geochemical characteristics of hydrocarbon source rocks in the Cambrian base of the Hefei Basin[J].Petroleum Geology & Experiment,200,24(3):273-278.[曹高社,宋明水,刘德良,等.合肥盆地寒武系底部烃源岩沉积环境和地球化学特征[J].石油实验地质,200,24(3):273-278.]
[53]Cao Gaoshe,Zhang Shanwen,Liu Zhongquan,et al.Discovery of breakup uncomnformity at the top of Lower Sinian in the south margin of North China block:The geological implication[J].Acta Sedimentologica Sinica,2005,22(4):621-627.[曹高社,张善文,柳忠泉,等.华北陆块南缘下震旦统顶部裂离不整合的发现及其地质意义[J].沉积学报,2005,22(4):621-627.]
[54]Zhu Youhai,Ma Lifang.Division and correlation of lower Cambrian and its sedimentary evolution in North China[J].Geological Review,2008,54(6):731-740.[祝有海,马丽芳.华北地区下寒武统的划分对比及其沉积演化[J].地质论评,2008,54(6):731-740.]
[55]Zhao Chenlin,Li Rufeng,Zhou Jinsong.Petroleum Geology and Sedimentology of the Meso-and Neo-proterozoic in North China[M].Beijing:Geologieal Publishing House,1997.[赵澄林,李儒峰,周劲松.华北中新元古界油气地质与沉积学[M].北京:地质出版社,1997.]
[56]Zhang Jiaodong,Liu Deliang,Huang Kaiquan,et al.Discussion on the hydrocarbon source rock characters of the Liulaobei Formation on the fringes of the Hefei Basin[J].Petroleum Geology & Expeximent,2004,26(5):474-478.[张交东,刘德良,黄开权,等.合肥盆地盆缘刘老碑组烃源岩特征探讨[J].石油实验地质,2004,26(5):474-478.]
[57]Li Zhensheng,Liu Deliang,Wu Xiaoqi,et al.Hydrocarbon-generating potentials of the Neoproterozoic in Xuhuai area,the east part of southern North China[J].Chinese Journal of Geology,201,47(1):154-168.[李振生,刘德良,吴小奇,等.南华北东部徐淮地区新元古界生烃潜力分析[J].地质科学,201,47(1):154-168.]
[58]Wu Liyan,Gu Xinzhang.The application of pyrolysis technique in source rock research[J].Acta Petrolei Sinica,1986,7(2):13-19.[邬立言,顾信章.热解技术在我国生油岩研究中的应用[J].石油学报,1986,7(2):13-19.]
[59]Li Xin,Shang Hongqun,Li Jihong,et al.A review of indicators of thermal evolution of source rocks[J].Xinjiang Petroleum Geology,2007,28(3):379-384.[李鑫,尚鸿群,李继宏,等.烃源岩热演化指标研究现状[J].新疆石油地质,2007,28(3):379-384.]
[60]Qin Jianzhong.Hydrocarbon Source Rocks in China[M].Beijing:Science Press,2005.[秦建中.中国烃源岩[M].北京:科学出版社,2005.]
[61]Zhang Jiaodong,Wang Dengwen,Liu Deliang,et al.A discussion on the basement time in the deep drill Ancan-1,Hefei Basin,southern margin of the North China plate[J].Geological Review,2008,54(4):433-438.[张交东,王登稳,刘德良,等.合肥盆地安参1超深井钻遇的基底时代问题讨论[J].地质论评,2008,54(4):433-438.]
[62]Liu Dehan,Shi Jiyang.Discussion on high evolution carbonate hydrocarbon source rocks unconventional evaluation method[J].Petroleum Exploration and Development,1994,21(3):113-115.[刘德汉,史继扬.高演化碳酸盐烃源岩非常规评价方法探讨[J].石油勘探与开发,1994,21(3):113-115.]
[63]Wang Feiyu,Chen Jing yi,Gao Gang,et al.Reflectance of macroalgae-derived vitrinite-like macerals:An organic maturity indicator for pre-Devonian marine strata[J].Petroleum Exploration and Development,2010,37(2):250-256.[王飞宇,陈敬轶,高岗,等.源于宏观藻类的镜状体反射率——前泥盆纪海相地层成熟度标尺[J].石油勘探与开发,2010,37(2):250-256.]
[64]Liao Yongsheng.Some issues about evaluation on high-over matured gas source rocks[J].Petroleum Exploration and Development,2005,32(4):147-152.[廖永胜.高—过成熟气源岩评价的若干问题[J].石油勘探与开发,2005,32(4):147-152.]
[65]Huo Zhipeng,Pang Xiongqi,Zhang Baoshou,et al.Evidences on effective carbonate source rock of low organic matter abundance and it’s lower limit of TOC[J].Geological Review,201,59(6):1165-1176.[霍志鹏,庞雄奇,张宝收,等.低丰度碳酸盐岩有效烃源岩存在的证据及其TOC下限[J].地质论评,201,59(6):1165-1176.]
[66]Liao Jianbo,Chen Qilin,Li Zhiyong,et al.Discovery and significance of hydrocarbonsource rocks in the Lower Cambrian at the southern margin of Ordos Basin[J].Journal of China University of Mining & Technology,2016,45(3):527-534.[廖建波,陈启林,李智勇,等.鄂尔多斯南缘下寒武统烃源岩的发现与意义[J].中国矿业大学学报,2016,45(3):527-534.]

[1] 龙胜祥,冯动军,李凤霞,杜伟. 四川盆地南部深层海相页岩气勘探开发前景[J]. 天然气地球科学, 2018, 29(4): 443-451.
[2] 申宝剑,秦建中,腾格尔,潘安阳,仰云峰,边立曾. 中国南方海相烃源岩中细菌状化石识别[J]. 天然气地球科学, 2018, 29(4): 510-517.
[3] 沈安江,付小东,张友,郑兴平,刘伟,邵冠铭,曹彦清. 塔里木盆地塔东地区震旦系—下古生界碳酸盐岩油气生储条件与勘探领域[J]. 天然气地球科学, 2018, 29(1): 1-16.
[4] 朱彤,俞凌杰,王烽. 四川盆地海相、湖相页岩气形成条件对比及开发策略[J]. 天然气地球科学, 2017, 28(4): 633-641.
[5] 刘培,于水明,王福国,陶文芳,张庆,许新明,胡坤. 珠江口盆地恩平凹陷海相泥岩盖层有效性评价及应用[J]. 天然气地球科学, 2017, 28(3): 452-459.
[6] 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.
[7] 吴小奇,陈迎宾,赵国伟,杜小伟,曾华盛,王萍,王彦青,胡烨. 四川盆地川西坳陷新场气田上三叠统须家河组五段烃源岩评价[J]. 天然气地球科学, 2017, 28(11): 1714-1722.
[8] 董大忠,王玉满,黄旭楠,张晨晨,管全中,黄金亮,王淑芳,李新景. 中国页岩气地质特征、资源评价方法及关键参数[J]. 天然气地球科学, 2016, 27(9): 1583-1601.
[9] 王玉满,李新景,董大忠,张晨晨,王淑芳,黄金亮,管全中. 海相页岩裂缝孔隙发育机制及地质意义[J]. 天然气地球科学, 2016, 27(9): 1602-1610.
[10] 刘伟,黄擎宇,王坤,石书缘. 深埋藏阶段白云岩化作用及其对储层的影响——以塔里木盆地下古生界白云岩为例[J]. 天然气地球科学, 2016, 27(5): 772-779.
[11] 刘洪林,王红岩,孙莎莎,吝文. 南方海相页岩气超压特征及主要选区指标研究[J]. 天然气地球科学, 2016, 27(3): 417-422.
[12] 管全中,董大忠,王淑芳,黄金亮,王玉满,张晨. 海相和陆相页岩储层微观结构差异性分析[J]. 天然气地球科学, 2016, 27(3): 524-531.
[13] 刘丹,冯子齐,刘洋,彭威龙,韩文学. 鄂尔多斯盆地中东部下古生界奥陶系自生自储气地球化学特征[J]. 天然气地球科学, 2016, 27(10): 1892-1903.
[14] 张道锋,刘新社,高星,崔子岳,闫小雄. 鄂尔多斯盆地西部奥陶系海相碳酸盐岩地质特征与成藏模式研究[J]. 天然气地球科学, 2016, 27(1): 92-101.
[15] 孙东,杨丽莎,王宏斌,郑多明,孙勤华,李国会,代冬冬,房启飞. 塔里木盆地哈拉哈塘地区走滑断裂体系对奥陶系海相碳酸盐岩储层的控制作用[J]. 天然气地球科学, 2015, 26(S1): 80-87.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!