天然气地球科学

• 天然气地质学 • 上一篇    下一篇

塔北隆起中部东河塘组高精度层序地层及沉积体系研究

赵建华,林畅松,刘永福,刘景彦,范秋海,范倩倩   

  1. 1.中国地质大学(北京)能源学院,北京 100083;2.中国地质大学(北京)海洋学院,北京 100083;
    3.中国石油塔里木油田勘探开发研究院,新疆   库尔勒 841000
  • 收稿日期:2013-05-16 修回日期:2013-07-11 出版日期:2014-03-10 发布日期:2014-03-10
  • 通讯作者: 赵建华zhao_jh2013@163.com. E-mail:zhao_jh2013@163.com.
  • 作者简介:赵建华(1985-),男,河北承德人,博士研究生,主要从事沉积学与盆地分析研究.E-mail:zhao_jh2013@163.com.
  • 基金资助:

    国家自然科学基金重点项目“塔里木盆地古生代古构造、古地理演变与成藏效应”(编号:41130422);国家重点基础研究发展计划“973”项目“中国西部典型叠合盆地隆坳格局形成演化与岩性地层圈闭发育模式”(编号:2006CB202302)联合资助.

Study on the High-resolution Sequence Stratigraphy and Depositional Systems of the Donghetang Formation in the Central Tabei Uplift

ZHAO Jian-hua,LIN Chang-song,LIU Yong-fu,LIU Jing-yan,FAN Qiu-hai,FAN Qian-qian   

  1. 1.School of Energy and Resources,China University of Geosciences,Beijing 100083,China;
    2.School of Ocean Sciences,China University of Geosciences,Beijing 100083,China;
    3.Research Institution of Petroleum Exploration and Development,Tarim Oilfield,PetroChina,Kolar 841000,China
  • Received:2013-05-16 Revised:2013-07-11 Online:2014-03-10 Published:2014-03-10

摘要:

高精度层序地层为储层精细对比提供了重要手段。应用高精度层序地层学的理论和方法,以岩心、测井资料、地震资料和野外露头为基础建立了塔北隆起中部东河塘组高精度层序地层格架。塔北隆起中部东河塘组由一个完整的海平面升降旋回构成一个三级层序,以其内部相对稳定的水进面为界进行高精度层序划分,可划分出6个四级层序。通过野外露头对比、岩心观察、测井及地震特征的对比,在层序内部识别出浪控三角洲和滨岸沉积体系,明确了沉积体系的分布规律,总结了物源供给、古地貌及海平面变化等因素对沉积体系发育的控制作用。

关键词: 高精度层序地层, 塔北隆起, 东河塘组, 沉积体系

Abstract:

High-resolution sequence stratigraphy provides an important method for reservoir hierarchy correlation.With the application of high-resolution sequence stratigraphic theory and method,the high-resolution sequence stratigraphy framework of the Donghetang Formation in the central Tabei Uplift was established based on the analysis of well logs,core,outcrop and seismic data.As a third-order sequence,the Donghetang Formation consists of a complete eustatic cycle.According to its relatively stable transgressive surface,it can be divided into six 4th order sequences.Wave-dominated deltas and coastal sedimentary systems were recognized within the sequence and their distribution patterns were defined.It can be concluded that the development of depositional systems are controlled by provenance,palaeogeomorphology and sea-level change.

Key words: High-resolution sequence stratigraphy, Tabei Uplift, Donghetang Formation, Depositional systems

中图分类号: 

  • TE121.3

[1]Mitchum R M,Vanwagoner J C.High-resolution sequence and their stacking patterns:Sequence stratigraphic evidence of high-frequency eustatic cycles[J].Sedimentary Geology,1991,70:131-160.[ZK)]

[2]Nummedal D,Riley G W,Templet P L.High-resolution sequence architecture:A chronostratigraphic model based on equilibrium profile studies[M]//Posamentier H W,Colin P.Sequence Stratigraphy and Facies Associations,International Association of Sedimentologists Special Publication.New York:John Wiley and Sons,1993,18:55-68.

[3]Lin Changsong,Liu Jingyan,Liu Lijun,et al.High resolution sequence stratigraphy analysis:Construction of chronostratigraphic sequence framework on facies and reservoir scale[J].Geoscience,2002,16(3):276-281.[林畅松,刘景彦,刘丽军,等.高精度层序地层分析:建立沉积相和储层规模的等时地层格架[J].现代地质,2002,16(3):276-281.]

[4]Yang Yongjian,Liu Jiaduo,Tian Jingchun,et al.Sequence Lithofacies paleogeography of cambrian in Tarim Basin\[J\].Natural Gas Geoscience,2011,22(3):450-459.\[杨永剑,刘家铎,田景春,等.塔里木盆地寒武纪层序岩相古地理特征\[J\].天然气地球科学,2011,22(3):450-459.\]

[5]Lin Changsong,Liu Jingyan,Zhang Yanmei,et al.The Characteristics of eogene tectonic sequence stratigraphy and effection response of foreland tectonic movement of the Palaeogene Kuqa Depression [J].Science in China:Series D,2002,32(3):177-183.[林畅松,刘景彦,张燕梅,等.库车坳陷第三系构造层序的构成特征及其对前陆构造作用的响应[J].中国科学:D辑,2002,32(3):177-183.]

[6]Wang Zhaoming,Tian Jun,Shen Yinmin,et al.Sedimentary facies of Donghe sandstone during the Late Devonian to Early Carboniferous in Tarim Basin[J].Journal of Palaeogeography,2004,32(11):648-654.[王招明,田军,申银民,等.塔里木盆地晚泥盆世—早石炭世东河砂岩沉积相[J].古地理学报,2004,6(3):289-296.]

[7]Zhu Xiaomin,Zhang Qiang,Lv Xueyan,et al.Comparison of the sedimentary  characteristics of the Donghe sandstone section between the Tabei and Tazhong areas,Tarim Basin[J].Chinese Geology,2005,32(11):648-654.[朱筱敏,张强,吕雪雁,等.塔里木盆地塔北与塔中地区东河砂岩段沉积特征对比[J].中国地质,2005,32(11):648-654.]

[8]Zhang Huiliang,Yang Haijun,Shou Jianfeng,et al.Sedimentary periods of Donghe sandstone and hydrocarbon exploration in Tarim Basin[J].Acta Petrolei Sinica,2009,30(6):835-842.[张惠良,杨海军,寿建峰,等.塔里木盆地东河砂岩沉积期次及油气勘探[J].石油学报,2009,30(6):835-842.]

[9]Chu Chenglin,Lin Changsong,Zhu Yongfeng,et al.Study on the sequence stratigraphy and depositional system of Donghe sandstone in Tabei Uplift[J].Journal of Southwest Petroleum University:Science & Technology Edition,2011,33(1):15-20.[储呈林,林畅松,朱永峰,等.塔北隆起东河砂岩层序地层和沉积体系研究[J].西南石油大学学报:自然科学版,2011,33(1):15-20.]

[10]Zhang Qin,Tang Xuan,Yang Yiting,et al.Petroleum migration in Lower Devonian Donghe Formation sandstone (P3d),in Tazhong area of Tarim Basin[J].Natural Gas Geoscience,2011,22(6):996-1000.\[张琴,唐玄,杨镜婷,等.塔中地区泥盆系东河砂岩石油运聚方向研究\[J\].天然气地球科学,2011,22(6):996-1000.]

[11]Liu Jingyan,Ronald J Steel,Lin Changsong,et al.Geomorphology control on the development of reservoir Depositional systems,Devonian Donghetang Formation in the Tabei Uplift of the Tarim Basin,China[J].Marine and Petroleum Geology,2012,38:177-194.

[12]Guo Jianhua,Zhu Meiheng,Liu Chensheng,et al.Sedimentary facies and sequence stratigraphy of Donghe sandstone in Akekule Uplift[J].Oil & Gas Geology,2005,26(6):808-815.[郭建华,朱美衡,刘辰生,等.阿克库勒凸起东河砂岩的沉积相与层序地层[J].石油与天然气地质,2005,26(6):808-815.]

[13]Gu Jiayu,Zhang Xingyang,Guo Bincheng.Characteristics of sedimentation and reservoir of the Donghe sandstone in Tarim Basin and their synthetic analysis[J].Journal of Palaeogeography,2006,8(3):285-294.[顾家裕,张兴阳,郭彬程.塔里木盆地东河砂岩沉积和储层特征及综合分析[J].古地理学报,2006,8(3):285-294.]

[14]Shen Yinmin,Jia Jinhua,Qi Yingmin,et al.Sedimentary facies of Donghe sandstone in the Upper Devonian-Lower Carboniferous and discovery of Hadexun Oilfield in Tarim Basin[J].Journal of Palaeogeography,2011,13(3):279-286.[申银民,贾进华,齐英敏,等.塔里木盆地上泥盆统—下石炭统东河砂岩沉积相与哈得逊油田的发现[J].古地理学报,2011,13(3):279-286.]

[15]Xin Renchen,Jia Jinhua,Yang Bo.Sequence stratigraphic framework and palaeogeography of the Upper Devonian to Lower Carboniferous in Tarim Basin[J].Journal of Palaeogeography,2011,13(6):665-676.[辛仁臣,贾进华,杨波.塔里木盆地上泥盆—下石炭统层序地层格架与古地理[J].古地理学报,2011,13(6):665-676.]

[16]Jia Chengzao,Wei Guoqi.The summary of the achievements on the tectonic researches in Tarim Basin during the period of 9th five-year plan[J].Petroleum Exploration and Development,2003,30(1):11-14.[贾承造,魏国齐.“九五”期间塔里木盆地构造研究成果概述[J].石油勘探与开发,2003,30(1):11-14.]

[17]He Bizhu,Jiao Cunli,Xu Zhiqin,et al.Manifestation of the Middle-Late Caledonian Tectonic Movement along the Altun-West Kunlun orogenic belt in the Tangguzibasi Depression,Tarim Basin[J].Acta Petrologica Sinica,2011,27(11):3435-3448.[何碧竹,焦存礼,许志琴,等.阿尔金—西昆仑加里东中晚期构造作用在塔里木盆地塘沽兹巴斯凹陷中的响应[J].岩石学报,2011,27(11):3435-3448.]

[1] 高崇龙,纪友亮,靳军,王剑,任影,曾力,王道伟,张昊,李谨杰. 古隆起埋藏期沟谷残丘地貌下沉积体系及油气藏发育模式——以准噶尔盆地腹部石南地区清水河组一段为例[J]. 天然气地球科学, 2018, 29(8): 1120-1137.
[2] 杨占龙,黄云峰,沙雪梅,吴青鹏,黄小鹏,郝彬. 吐哈盆地鄯善弧形带东翼中—下侏罗统沉积体系发育模式[J]. 天然气地球科学, 2018, 29(3): 349-357.
[3] 张广权,胡向阳,孙兵,贾跃玮. 松辽盆地龙凤山凝析气藏营四砂组沉积特征及控制因素分析[J]. 天然气地球科学, 2017, 28(4): 502-513.
[4] 赵春晨,刘护创,任来义,陈治军,李科社,白晓寅,王小多. 银额盆地YHC1井白垩系气藏形成的地质环境及其远景意义[J]. 天然气地球科学, 2017, 28(3): 439-451.
[5] 廖计华,王华,甘华军,孙鸣,王颖,蔡露露,郭帅,郭佳. 莺歌海盆地东方区中新统黄流组一段高精度层序地层特征与隐蔽油气藏预测[J]. 天然气地球科学, 2017, 28(2): 241-253.
[6] 王琪,田兵,马晓峰,牟炜卫,高丽华. 珠江口盆地白云深水区深水水道沉积体系及成因模式[J]. 天然气地球科学, 2017, 28(10): 1497-1505.
[7] 韩银学,王龙颖,杨东升,曾清波,白海强,郭帅,杨香华. 珠江口盆地白云凹陷珠海组南部物源及其油气勘探意义[J]. 天然气地球科学, 2017, 28(10): 1537-1545.
[8] 陈彬滔,潘树新,方乐华,张庆石,李成刚,梁苏娟. 松辽盆地齐家—古龙凹陷青山口组泥页岩层段储层特征[J]. 天然气地球科学, 2016, 27(2): 298-308.
[9] 孟祥霞,王宏斌,姚清洲,余建平,代冬冬,杨丽莎. 塔北隆起构造演化特征及对奥陶系碳酸盐岩的控储控藏作用[J]. 天然气地球科学, 2015, 26(S1): 109-120.
[10] 马永平,黄林军,滕团余,谭开俊,王国栋,尹路. 准噶尔盆地玛湖凹陷斜坡区三叠系百口泉组高精度层序地层研究[J]. 天然气地球科学, 2015, 26(S1): 33-40.
[11] 龙礼文,李相博,刘广林,廖建波,赵园园,李智勇. 鄂尔多斯盆地延长组深水砂岩储层岩石学特征及地质意义[J]. 天然气地球科学, 2015, 26(4): 634-640.
[12] 肖传桃,肖胜,叶飞,梁文君. 柴达木盆地昆北—阿拉尔地区坡折带及其对岩性油气藏的控制[J]. 天然气地球科学, 2015, 26(11): 2085-2092.
[13] 常象春,王铁冠,程 斌,王 鑫,邓冰红. 塔北隆起中部原油轻烃地球化学特征及其意义[J]. 天然气地球科学, 2014, 25(7): 1058-1064.
[14] 周俊峰, 张虎权, 刘建新, 姚清洲, 王锦喜. 塔北隆起YM1-2构造带古生界断裂特征及成因机制分析[J]. 天然气地球科学, 2012, 23(2): 237-243.
[15] 肖立新, 陈能贵, 张健, 沈金龙, 张顺存. 准噶尔盆地南缘古近系紫泥泉子组沉积体系分析[J]. 天然气地球科学, 2011, 22(3): 426-431.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!