全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

巢湖地区栖霞组碳酸盐烃源岩的形成及影响因素

, PP. 873-886

Keywords: 下扬子,栖霞组,孢粉相,古环境,碳酸盐烃源岩,非均质分布

Full-Text   Cite this paper   Add to My Lib

Abstract:

?高演化碳酸盐烃源岩的研究对我国南方油气勘探至关重要.为此,选择下扬子巢湖地区发育较完整的茨苔山栖霞组碳酸盐岩地层,开展沉积学、孢粉相和有机地球化学综合研究;在古环境重建基础上,探讨烃源岩的形成及影响因素.结果表明,栖霞组为二叠纪海侵期形成的生物成因碳酸盐缺氧沉积,纵向上,有机和无机组分变化大.烃源岩的形成是海侵和海侵期间频繁发生的充氧事件引发的高生物产率与缺氧环境综合作用的结果.受自稀释和沉积后作用影响,烃源岩呈非均质分布在多个层段中,累计厚度超过40m,并可通过有机、生物和矿物组成特征进行识别.本次研究认为,碳酸盐岩成为烃源岩并非需要较高的粘土含量.沉积学、孢粉相和有机地球化学方法的结合,为我国高演化碳酸盐烃源岩评价和预测提供了一条更为直接和有效的途径.

References

[1]  1 Hunt J M. Petroleum Geochemistry and Geology. San Francisco: Freeman, 1979. 1-617
[2]  2 Flügel E. 碳酸盐岩微相. 马永生, 译. 北京: 地质出版社, 2004. 1-882
[3]  3 Karl R, Teodoro M M, Valeria D, et al. Nature and origin of organic matter in carbonates from speleothems, marine cements and coral skeletons. Org Geochem, 1997, 26: 361-378??
[4]  4 Harris P M, Katz B J. Carbonate mud and carbonate source rocks. In: AAPG 2005 Annual Convention Abstract Volume, 2004. 36
[5]  5 Tyson R V. Sedimentary Organic Matter: Organic Facies and Palynofacies. London: Chapman and Hall, 1995. 1-615
[6]  6 Ricken W. Sedimentation as a Three-component System: Organic Carbon, Carbonate, Noncarbonate. Berlin: Springer-Verlag, 1993. 1―207
[7]  7 Suss E. Interaction of organic compounds with calcium carbonate-II, Organo-carbonate association in Recent sediments. Geochim Cosmochim Acta, 1973, 37: 2435-2447??
[8]  8 蔡进功, 郭志刚, 李从先, 等. 水体中有机质的类型与有机质沉积作用. 同济大学学报(自然科学版), 2005, 33: 1213-1218
[9]  9 蔡进功, 徐金鲤, 杨守业, 等. 泥质沉积物颗粒分级及其有机质富集的差异性. 高校地质学报, 2006, 12: 234-241
[10]  10 蔡进功, 包于进, 杨守业, 等. 泥质沉积物和泥岩中有机质的赋存形式与富集机制. 中国科学D辑: 地球科学, 2007, 37: 244-253
[11]  11 Baldock J A, Skjemstad J O. Role of the soil matrix and minerals in protecting natural organic materials against biological attack.Org Geochem, 2000, 31: 697-710??
[12]  12 Al-Ameri T K, Batten D J. Palynomorph and palynofacies indications of age, depositional environments and source potential for hydrocarbons: Lower Cretaceous Zubair Formation, southern Iraq. Cret Res, 1997, 18: 789-797??
[13]  13 Al-Ameri T K, Al-Musawi F S, Batten D J. Palynofacies indications of depositional environments and source potential for hydrocarbons: Uppermost Jurassic-basal Cretaceous Sulaiy Formation, southern Iraq. Cret Res, 1999, 20: 359-363??
[14]  14 Al-Ameri T K, Al-Najar T K, Batten D J. Palynostratigraphy and palynofacies indications of depositional environments and source potential for hydrocarbons: The mid Cretaceous Nahr Umr and lower Mauddud formations, Iraq. Cret Res, 2001, 22: 735-742??
[15]  15 Bombardiere L, Gorin G E. Stratigraphical and lateral distribution of sedimentary organic matter in Upper Jurassic carbonates of SE France. Sediment Geol, 2000, 132: 177-203??
[16]  16 Carvalho M A, Filho J G M, Menezes T R. Paleoenvironmental reconstruction based on palynofacies analysis of the Aptian-Albian succession of the Sergipe Basin, northeastern Brazil. Mar Micropaleontol, 2006, 59: 56-81??
[17]  17 Ercegovac M, Kostic A. Organic facies and palynofacies: Nomenclature, classification and applicability for petroleum source rock evaluation. Int J Coal Geol, 2006, 68: 70-78??
[18]  18 Ruf M, Link E, Pross J, et al. Integrated sequence stratigraphy: Facies, stable isotope and palynofacies analysis in a deeper epicontinental carbonate ramp (Late Jurassic, SW Germany). Sediment Geol, 2005, 175: 391-414??
[19]  19 Tribovillard N, Bialkowski A, Tyson R V, et al. Organic facies variation in the late Kimmeridgian of the Boulonnais area (northernmost France). Mar Petrol Geol, 2001, 18: 371-389??
[20]  20 Tyson R V. Palynofacies analysis. In: Jenkins D J, ed. Applied Micropalaeontology. Dordrecht: Kluwer Academic Publishers, 1993. 153-191
[21]  21 秦建中, 刘宝泉, 国建英, 等. 关于碳酸盐烃源岩的评价标准. 石油实验地质, 2004, 26: 281-286
[22]  22 Pederson T F, Calvert S E. Anoxia versus productivity: What controls the formation of organic-carbon-rich sediments and sedimentary rock. Am Assoc Petrol Geol Bull, 1990, 74: 454-466
[23]  23 Tyson R V, Pearson T H. Modern and ancient continental shelf anoxia: An overview. In: Tyson R V, Pearson T H, eds. Modern and Ancient Continental Shelf Anoxia. Geol Soc Spec Publ, 1991, 58: 1-24??
[24]  24 张宝民, 张水昌, 边立曾, 等. 浅析中国新元古-下古生界海相烃源岩发育模式. 科学通报, 2007, 52(增刊Ⅰ): 58-69
[25]  25 梁狄刚, 郭彤楼, 陈建平, 等. 中国南方海相生烃成藏研究的若干新进展(一)南方四套区域性海相烃源岩的分布. 海相油气地质, 2008, 13: 1-16
[26]  26 林小云. 中下扬子地区海相烃源岩评价及成藏条件. 武汉: 中国地质大学出版社, 2007. 11-48
[27]  27 李双应, 岳书仓. 安徽巢湖二叠系栖霞组碳酸盐岩斜坡沉积. 沉积学报, 2002, 20: 7-12
[28]  28 冯增昭, 杨玉卿, 金振奎, 等. 中国南方二叠纪岩相古地理. 北京: 石油大学出版社, 1997. 1-242
[29]  29 李建国, David J B. 孢粉相: 原理及方法. 古生物学报, 2005, 44: 138-156
[30]  30 肖传桃, 丁静, 胡望水, 等. 下扬子地区中二叠世上升流相区古生态学研究. 沉积学报, 2009, 27: 319-325
[31]  31 Batten D J. Palynofacies and palaeoenvironmental interpretation. In: Jansonius J, McGregor D C, eds. Palynology: Principles and Applications. Am Assoc Stratigr Palynol Found, 1996, 3: 1011-1064
[32]  32 吕炳全, 瞿建忠. 下扬子地区早二叠世海进和上升流形成的缺氧环境的沉积. 科学通报, 1989, 22: 1721-1724
[33]  33 颜佳新, 刘新宇. 从地球生物学角度讨论华南中二叠世海相烃源岩缺氧沉积环境成因模式. 地球科学—中国地质大学学报, 2007, 32: 789-796
[34]  34 杜小弟, 黄志诚, 陈智娜, 等. 下扬子区二叠系层序地层的地球化学特征. 高校地质学报, 1996, 2: 348-356
[35]  35 郭福生, 潘家永, 刘林清, 等. 浙江江山石炭-二叠系碳酸盐岩碳氧同位素特征研究. 地球化学, 2004, 33: 1-8
[36]  36 王成善, 李祥辉, 陈洪德, 等. 中国南方二叠纪海平面变化及升降事件. 沉积学报, 1999, 17: 536-541
[37]  37 吴基文, 李东平. 皖南地区二叠纪层序地层学研究. 地层学杂志, 2001, 25: 18-23
[38]  38 Smojic S B, Smajlovic J, Koch G, et al. Source potential and palynofacies of Late Jurassic ‘‘Lemes facies”, Croatia. Org Geochem, 2009, 40: 833-845??
[39]  39 Batten D J. Identification of amouphous sedimentary organic matter by transmitted light microscopy. In: Brooks J, ed. Petroleum Geochemistry and Exploration of Europe. Geol Soc Spec Publ, 1983, 11: 275-287
[40]  40 Bertrand P, Pittion J L, Bernaud C. Fluorescence of sedimentary organic matter in relation to its chemical composition. Org Geochem, 1986, 10: 641-647??
[41]  41 梁狄刚, 郭彤楼, 陈建平, 等. 中国南方海相生烃成藏研究的若干新进展(二)南方四套区域性海相烃源岩的地球化学特征. 海相油气地质, 2009, 14: 1-15
[42]  42 腾格尔, 刘文汇, 徐永昌, 等. 高演化海相碳酸盐烃源岩地球化学综合判识—以鄂尔多斯盆地为例. 中国科学D辑: 地球科学, 2006, 36: 167-176
[43]  43 Bogdanov Y A, Gurvich Y G, Lisitzin A P. Model for the accumulation of calcium carbonate in bottom sediments of Pacific Ocean. Geochem Int, 1980, 17: 125-132
[44]  44 Ibach L E J. Relationship between sedimentation rate and total organic carbon content in ancient marine sediments. Am Assoc Petrol Geol Bull, 1982, 66: 170-183
[45]  45 郭念发, 姚柏平, 吴群. 安徽无为盆地油气地质条件评价. 安徽地质, 1999, 9: 289-294
[46]  46 Riediger C L, Bloch J D. Depositional and diagenetic controls on source rock characteristics of the Lower Jurassic “Nordegg Member”, Westerm Canada. J Sediment Res, 1995, A65: 112-126

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133