桦甸盆地桦甸组油页岩成烃生物组成及生烃潜力

王勤; 谢小敏; 腾格尔; 芮晓庆; 许锦

doi:10.11781/sysydz201803403

桦甸盆地桦甸组油页岩成烃生物组成及生烃潜力

doi: 10.11781/sysydz201803403

王勤^1,2,3,
谢小敏^1,2,3, ,,
腾格尔^1,2,3,
芮晓庆^1,2,3,
许锦^1,2,3

1.
页岩油气富集机理与有效开发国家重点实验室, 江苏无锡 214126
2. 中国石油化工集团公司油气成藏重点实验室, 江苏无锡 214126
3. 中国石化石油勘探开发研究院无锡石油地质研究所, 江苏无锡 214126

基金项目: 国家重点基础研究发展计划（973计划）项目（2014CB239101）、国家自然科学基金项目（41603047，U1663202）和中石化科技部青年创新计划项目（P14132）资助。

详细信息

作者简介:
王勤(1971-),女,工程师,从事油气地球化学的实验和研究。E-mail:wangqin.syky@sinopec.com。

通讯作者:
谢小敏(1984-),女,硕士,高级工程师,从事有机岩石学和油气地球化学研究。E-mail:xiexm.syky@sinopec.com。

中图分类号: TE122.11
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出版历程
- 收稿日期: 2017-10-10
- 修回日期: 2018-04-10
- 刊出日期: 2018-05-28

Bio-precursor characterization and hydrocarbon generation potential of shale in Eocene Huadian Formation, Huadian Basin

WANG Qin^1,2,3,
XIE Xiaomin^{1,2,3
, ,},
TENGER Boltsjin^1,2,3,
RUI Xiaoqing^1,2,3,
XU Jin^1,2,3

1.
State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development, Wuxi, Jiangsu 214126, China
2. SINOPEC Key Laboratory of Petroleum Accumulation Mechanisms, Wuxi, Jiangsu 214126, China
3. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

摘要

摘要: 桦甸盆地始新统桦甸组中发育一套优质油页岩。利用显微镜及扫描电镜对该盆地光榔头矿区22个样品进行分析，并对2个含不同藻类的样品进行生烃热模拟实验，研究其成烃生物特征及生烃潜力。桦甸油页岩有机碳含量很高（10.6%～39.6%），氢指数含量高达887 mg/g，显示该套油页岩具有很好的生烃潜力。生物来源主要是蓝细菌组成的层状藻类体，其次结构藻类体较发育（以硅藻和葡萄球藻为主，底栖宏观藻类在部分样品中较多），高等植物主要包括碎屑镜质体、碎屑壳质体、孢子体等。生烃模拟实验结果显示，含较多底栖藻类的HD-20号样品在400℃（R_o=1.02%）时生烃量达到最大值（427 mg/g）；而以浮游藻类为主的HD-21号样品，在425℃时（R_o=1.18%）达到最大生烃量（909 mg/g）。虽然HD-20号样品具有很高的有机碳含量（39.6%），但其生烃量较浮游藻类为主的HD-21号样品（有机碳含量29.8%）差，指示底栖藻类具有较低的生烃潜力特征。
- 浮游藻类 /
- 底栖藻类 /
- 成烃生物 /
- 生烃潜力 /
- 始新统 /
- 桦甸盆地
Abstract: A set of high-quality oil shales developed in the Eocene Huadian Formation in the Huadian Basin, Jinlin Province. Twenty-two rock samples were collected from the Guanglangtou district for bio-precursor and hydrocarbon generation potential analyses. Two samples containing different types of algae were chosen for thermal simulation. The Huadian shale has a high TOC content (10.6%-39.6%) and a high Rock-Eval hydrogen index (HI) value (887 mg/g), suggesting a good hydrocarbon generation potential. Detailed bio-precursor analyses demonstrated that the organic matter was dominated by phytoplankton, such as lamalginite and telalginite (including botryococcus and diatom), and fragments from benthic macroalgal rhodophyte were found in some thin layers. Higher plants mainly include detrital vitrinoids, fungi and detrital plastids, and sporophytes. The sample HD-20 with more benthic algae produced the maximum amount of hydrocarbon (427 mg/g) at 400℃ (R_o=1.02%), while the sample HD-21 dominated by planktonic algae produced the maximum amount of hydrocarbon (909 mg/g) at 425℃ (R_o=1.18%). Thermal simulation experiments showed that the sample HD-21 had a much higher hydrocarbon generation potential than the sample HD-20, even though the TOC content of HD-20 was much higher, indicating that the benthic macroalgal macerals have a much lower capacity to generate oil when thermally mature.
- phytoplankton /
- benthic macroalgae /
- bio-precursor /
- hydrocarbon generation potential /
- Eocene /
- Huadian Basin

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参考文献(23)

[1]	BOUCSEIN B,STEIN R.Black shale formation in the Late Paleocene/early Eocene Arctic Ocean and paleoenvironmental conditions:New results from a detailed organic petrological study[J].Marine and Petroleum Geology,2009,26(3):416-426.
[2]	PETERSEN H I,NYTOFT H P.Oil generation capacity of coals as a function of coal age and aliphatic structure[J].Organic Geochemistry,2006,37(5):558-583.
[3]	DEMAISON G J,MOORE G T.Anoxic environments and oil source bed genesis[J].Organic Geochemistry,1980,2(1):9-31.
[4]	DOW W G.Kerogen studies and geological interpretation[J].Journal of Geochemical Exploration,1977,7(2):79-99.
[5]	DUTTA S,MATHEWS R P,SINGH B D,et al.Petrology,palynology and organic geochemistry of Eocene lignite of Matanomadh,Kutch Basin,western India:Implications to depositional environment and hydrocarbon source potential[J].International Journal of Coal Geology,2011,85(1):91-102.
[6]	MULLER J.Palynology of Recent Orinoco delta and shelf sediments[J].Micropaleontology,1959,5(1):1-32.
[7]	PUTTMANN W,SUN Y Z,KALKREUTH W.Variation of petrological and geochemical compositions in a sequence of humic coals,cannel coals,and oil shales[J].Energy & Fuels,1994,8(6):1460-1468.
[8]	王永莉,刘招君,荆惠林,等.桦甸盆地古近系桦甸组油页岩矿床沉积特征[J].吉林大学学报(地球科学版),2005,35(6):720-724. WANG Yongli,LIU Zhaojun,JING Huilin,et al.Sedimentary characteristics of oil shale deposit of the Huadian Formation of Paleogene in Huadian Basin[J].Journal of Jilin University (Earth Science Edition),2005,35(6):720-724.
[9]	赵隆业,陈基娘,王天顺.关于中国油页岩的工业成因分类[J].煤田地质与勘探,1991,19(5):2-6. ZHAO Longye,CHEN Jiniang,WANG Tianshun.Industrial-original classification of Chinese oil shales[J].Coal Geology and Exploration,1991,19(5):2-6.
[10]	赵隆业,陈基娘,王天顺.我国油页岩成分和品级划分[J].现代地质,1991,5(4):423-429. ZHAO Longye,CHEN Jiniang,WANG Tianshun.Grade dividing and composition of oil shale in China[J].Geoscience,1991,5(4):423-429.
[11]	赵隆业,陈基娘,王天顺.油页岩定义和煤、油页岩界线和讨论[J].煤田地质与勘探,1991(1):15-16. ZHAO Longye,CHEN Jiniang,WANG Tianshun.The definition of oil shales and the borderline of oil and coal[J].Coal Geology and Exploration,1991(1):15-16.
[12]	吴冲龙,袁艳斌,李绍虎.抚顺盆地同沉积构造及其对煤和油页岩厚度的控制[J].煤田地质与勘探,1998(6):2-7. WU Chonglong,YUAN Yanbin,LI Shaohu.The synsedimentary structure framework and its controls on the thickness of extra-thick coal bed & oil thale,Fushun Basin,China[J].Coal Geo-logy & Exploration,1998(6):2-7.
[13]	SUN Pingchang,SACHSENHOFER R F,LIU Zhaojun,et al.Orga-nic matter accumulation in the oil shale-and coal-bearing Huadian Basin (Eocene;NE China)[J].International Journal of Coal Geology,2013,105:1-15.
[14]	PETERS K E.Guidelines for evaluating petroleum source rock using programmed pyrolysis[J].AAPG Bulletin,1986,70(3):318-329
[15]	DAMSTÉ J S S,DE LAS HERAS F X C,VAN BERGEN P F,et al.Characterization of Tertiary Catalan lacustrine oil shales:Discovery of extremely organicsulfur-rich Type I kerogens[J].Geochimica et Cosmochimica Acta,1993,57(2):389-415.
[16]	TISSOT B P,WELTE D H.Petroleum formation and occurrence[M].2nd ed.Heidelberg:Springer,1984:1-699.
[17]	PENIGUEL G,COUDERC R,SEYVE C.Les microalgues actuelles et fossiles-Interêts stratigraphique et pétrolier[J].Bulletin des Centres de Recherches Exploration-Production elf aquitaine,1989,13(2):455-482.
[18]	DAWES C J,SCOTT F M,BOWLER E.A light-and electron-microscopic survey of algal cell walls.I.Phaeophyta and Rhodophyta[J].American Journal of Botany,1961,48(10):925-934.
[19]	BOLD H C,WYNNE M J.Introduction to the algae:Structure and reproduction[M].Englewood Cliffs,New Jersey USA:Prentice Hall,1978:55.
[20]	边立曾,张水昌,张宝明,等.河北张家口下花园地区新元古代下马岭组油页岩中的红藻化石[J].微体古生物学报,2005,22(3):209-216. BIAN Lizeng,ZHANG Shuichuang,Zhang Baoming,et al.Red algal fossils discovered from the Neoproterozoic Xiamaling oil shales,Xiahuayuan town of Hebei province[J].Acta Micropalaeontologica Sinica,2005,22(3):209-216.
[21]	孟庆强,秦建中,刘文斌,等.多细胞宏观底栖藻类生烃特点实验研究[J].石油学报,2008,29(6):822-826. MENG Qingqiang,QIN Jianzhong,LIU Wenbin,et al.Experimental study on hydrocarbon generation of multi-cellular benthic macroalga[J].Acta Petrolei Sinica,29(6):822-826.
[22]	HARWOOD J L,JONES A L.Lipid metabolism in algae[J].Advances in Botanical Research,1989,16:1-53.
[23]	NELSON M M,PHLEGER C F,NICHOLS P D.Seasonal lipid composition in macroalgae of the northeastern Pacific Ocean[J].Botanica Marina,2005,45(1):58-65.