塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

doi:10.3969/j.issn.1673-8926.2017.05.008

岩性油气藏 ›› 2017, Vol. 29 ›› Issue (5): 67–75.doi: 10.3969/j.issn.1673-8926.2017.05.008

塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

姜海健¹, 陈强路¹, 乔桂林¹, 曹自成², 储呈林¹

1. 中国石化勘探开发研究院无锡石油地质研究所, 江苏无锡 214151;
2. 中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011

收稿日期:2016-12-10 修回日期:2017-03-03 出版日期:2017-09-21 发布日期:2017-09-21
作者简介:姜海健(1983-),男,硕士,工程师,主要从事碳酸盐岩地层沉积方面的研究工作。地址:(214151)江苏省无锡市滨湖区蠡湖大道2060号无锡石油地质研究所。Email:haijian_08@sina.com。
基金资助:
中国石化科技开发部项目“塔中、塔河奥陶系岩溶储层形成机理与分布”（编号：P13069）与中国石化西北油田分公司项目“塔里木盆地南部奥陶纪岩相古地理研究”（编号：KY2013-S-039）联合资助

Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin

JIANG Haijian¹, CHEN Qianglu¹, QIAO Guilin¹, CAO Zicheng², CHU Chenglin¹

1. Wuxi Institute of Petroleum Geology, Research Institute of Petroleum Exploration & Production, Sinopec, Wuxi 214151, Jiangsu, China;
2. Research Institute of Exploration & Production, Sinopec Northwest Oilfield Company, Urumqi 830011, China

Received:2016-12-10 Revised:2017-03-03 Online:2017-09-21 Published:2017-09-21

摘要/Abstract

摘要： 塔里木盆地中东部顺托果勒地区及邻区已取得重大油气突破，为了对该区早中奥陶世颗粒滩的发育及分布展开进一步研究，应用钻测井、岩心、薄片、地震等资料，对颗粒滩的特征、演化、分布规律等进行综合分析。研究区发育局限台地中低能颗粒滩、开阔台地中低能颗粒滩、开阔台地中高能颗粒滩、台地边缘颗粒滩、台地边缘生物丘-生物礁等沉积亚相，且不同滩体间常交互沉积。鹰山组沉积时期，顺托果勒地区为台内缓斜坡—低凹带，广泛发育开阔台地颗粒滩，导致局部地层厚度增大；一间房组沉积时期，随着海平面快速上升，台内颗粒滩向古城地区和顺托果勒北部地区迁移，从而使得这2个地区地层厚度增大。研究认为，古地貌是颗粒滩发育与否及其发育模式的决定性因素，而海平面的变化控制了颗粒滩的发育过程和沉积样式。

关键词: 冲积扇, 河流扇, 河流沉积, 分支河流体系, 沉积体系

Abstract: There are several new gas discoveries in Shuntuoguole area of mid-eastern Tarim Basin in recent years. So,it is necessary to re-understanding Lower-Middle Ordovician carbonate sedimentary facies for further exploration. Based on cores,thin sections,logging and seismic data,the characteristics,evolution and distribution of Lower-Middle Ordovician carbonate sedimentary facies were analyzed. Grain bank developed in variety of facies such as low-energy grain bank in the restricted platform,middle to high-energy grain bank facies and middle to lowenergy grain bank facies in open platform,bank facies and reef facies on margin of platform. In Yingshan period, grain bank facies widely developed in gentle slope and low-lying zone of intraplatform in Shuntuoguole area, which open platform grain bank increased local strata thickness. With rapid uprising of sea level,In Yijianfang period,open platform extended to whole Shuntuoguole area,grain bank migrated to Gucheng area and northern Shuntuoguole area. Platform is the key factor to develop grain bank,and the sea level change controls the process and pattern of grain bank.

Key words: alluvial fan, fluvial fan, fluvial deposits, distributive fluvial system, sedimentary system

中图分类号:

TE112.2

姜海健, 陈强路, 乔桂林, 曹自成, 储呈林. 塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布[J]. 岩性油气藏, 2017, 29(5): 67–75.

JIANG Haijian, CHEN Qianglu, QIAO Guilin, CAO Zicheng, CHU Chenglin. Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin[J]. Lithologic Reservoirs, 2017, 29(5): 67–75.

参考文献

[1] 罗平,张静,刘伟,等. 中国海相碳酸盐岩油气储集层基本特征.地学前缘,2008,15(1):36-50. LUO P,ZHANG J,LIU W,et al. Characteristics of marine carbonate hydrocarbon reservoirs in China. Earth Science Frontiers, 2008,15(1):36-50.
[2] 文华国,郑荣才,党录瑞,等. 四川盆地东部五百梯地区长兴组礁、滩相储层特征.岩性油气藏,2010,22(2):24-31. WEN H G,ZHENG R C,DANG L R,et al. Characteristics of reef and shoal facies reservoir of Upper Permian Changxing Formation in Wubaiti area,eastern Sichuan Basin. Lithologic Reservoirs,2010,22(2):24-31.
[3] 段金宝,李平平,陈丹,等. 元坝气田长兴组礁滩相岩性气藏形成与演化.岩性油气藏,2013,25(3):43-47. DUAN J B,LI P P,CHEN D,et al. Formation and evolution of the reef flat facies lithologic gas reservoir of Changxing Formation in Yuanba Gas Field,Sichuan Basin. Lithologic Reservoirs, 2013,25(3):43-47.
[4] 王招明,赵宽志,邬光辉,等. 塔中Ⅰ号坡折带上奥陶统礁滩型储集层发育特征及其主控因素. 石油与天然气地质,2007, 28(6):797-801. WANG Z M,ZHAO K Z,WU G H,et al. Characteristics and main controlling factors of the Upper Ordovician reef-bank reservoir development in the Tazhong I slope-break zone. Oil & Gas Geology,2007,28(6):797-801.
[5] 姜海健,马红强,钱一雄,等. 塔里木盆地S76井与TZ62井奥陶系礁滩相储层发育差异性对比. 石油与天然气地质,2011, 32(4):512-521. JIANG H J,MA H Q,QIAN Y X,et al. Differences of the Ordovician reef-bank reservoirs in S-76 and TZ-62 well in the Tarim Basin. Oil & Gas Geology,2011,32(4):512-521.
[6] 王铁冠,宋到福,李美俊,等. 塔里木盆地顺南-古城地区奥陶系鹰山组天然气气源与深层天然气勘探前景. 石油与天然气地质,2014,35(6):753-762. WANG T G,SONG D F,LI M J,et al. Natural gas source and deep gas exploration potential of the OrdovicianYingshan Formation in the Shunnan-Gucheng region,Tarim Basin. Oil & Gas Geology,2014,35(6):753-762.
[7] 云露,曹自成. 塔里木盆地顺南地区奥陶系油气富集与勘探潜力. 石油与天然气地质,2014,35(6):788-797. YUN L,CAO Z C. Hydrocarbon enrichment pattern and exploration potential of the Ordovician in Shunnan area,Tarim Basin. Oil & Gas Geology,2014,35(6):788-797.
[8] 沙旭光,马庆佑,吕海涛,等. 塔里木盆地古城墟隆起奥陶系油气成藏特征及主控因素.海相油气地质,2014,19(2):15-22. SHA X G,MA Q Y,LYU H T,et al. Hydrocarbon accumulation and main controlling factors of Ordovician reservoir in Guchengxu uplift,Tarim Basin. Marine Origin Petroleum Geology,2014, 19(2):15-22.
[9] 王冠,樊太亮,刘海龙. 塔里木盆地塔中-古城地区奥陶系碳酸盐岩台地边缘相特征及演化. 现代地质,2014,28(5):995-1007. WANG G,FAN T L,LIU H L. Characteristics and evolution of Ordovician carbonate platform marginal facies in Tazhong-Gucheng area,Tarim Basin. Geoscience,2014,28(5):995-1007.
[10] 朱长见,肖中尧,张宝民,等. 塔里木盆地古城4井区上寒武统-奥陶系储集层特征. 石油勘探与开发,2008,35(2):175-181. ZHU C J,XIAO Z Y,ZHANG B M,et al. Upper Cambrian-Ordovician reservoir characteristics in well Gucheng-4 area, Tarim Basin. Petroleum Exploration and Development,2008, 35(2):175-181.
[11] 郑兴平,潘文庆,常少英,等. 塔里木盆地奥陶系台缘类型及其储层发育程度的差异性. 岩性油气藏,2011,23(5):1-4. ZHENG X P,PANWQ,CHANG SY,et al. Relationship between Ordovician platform margin types and reef-shoal reservoirs in Tarim Basin. Lithologic Reservoirs,2011,23(5):1-4.
[12] 刘存革,李国蓉,罗鹏,等. 塔里木盆地北部寒武系大型进积型台地-斜坡地震层序、演化与控制因素. 地质学报,2016, 90(4):669-687. LIU C G,LI G R,LUO P,et al. Seismic sequences,evolution and control factors of large Cambrian progradational platformslope system in the northern Tarim Basin,northwest China. Acta Geologica Sinica,2016,90(4):669-687.
[13] 陈强路,储呈林,杨鑫,等. 塔里木盆地寒武系沉积模式与烃源岩发育.石油与实验地质,2015,37(6):689-695. CHEN Q L,CHU C L,YANG X,et al. Sedimentary model and development of the Cambrian source rocks in the Tarim Basin, NW China. Petroleum Geology & Experiment,2015,37(6):689-695.
[14] 何登发,周新源,张朝军,等. 塔里木地区奥陶纪原型盆地类型及其演化.科学通报,2007,52(增刊1):126-135. HE D F,ZHOU X Y,ZHANG C J,et al. Prototype basin types and their evolution in Ordovician,Tarim Basin. Chinese Science Bulletin,2007,52(Suppl 1):126-135.
[15] 徐旭辉. 塔里木古生代原型盆地分析的油气勘探意义. 石油与天然气地质,2002,23(3):224-228. XU X H. The significance of the analysis of Tarim Paleozoic prototype basins in oil and gas exploration. Oil & Gas Geology, 2002,23(3):224-228.
[16] 卫端,高志前,孟苗苗,等. 塔河地区鹰山组高精度层序划分及沉积模式.岩性油气藏,2016,28(6):68-77. WEI D,GAO Z Q,MENG M M,et al. High-precision sequence division and sedimentary model of Yingshan Formation in Tahe area,Tarim Basin. Lithologic Reservoirs,2016,28(6):68-77.
[17] 熊剑飞,余腾孝,曹自成,等. 塔里木盆地奥陶系"鹰山组"的解体及中下统界线的划分. 地层学杂志,2013,37(3):283-291. XIONG J F,YU T X,CAO Z C,et al. The breakup of the Ordovi cian Yingshan Formation and the Lower-Middle Ordovician boundary in theTarim Basin. Journal of Stratigraphy,2013,37(3):283-291.
[18] 姜海健,陈强路,尤东华,等. 塔里木盆地柯坪-巴楚地区奥陶系层序界面特征及成因分析.新疆地质,2015,33(1):84-89. JIANG H J,CHEN Q L,YOU D H,et al. The different Ordovician sequence boundary's features and factors of Keping-Bachu area in Tarim Basin. Xinjiang Geology,2015,33(1):84-89.
[19] 邵红梅,冯子辉,王成,等. 塔里木盆地古城地区下古生界白云岩储层类型及成因. 大庆石油地质与开发,2014,33(5):111-116. SHAO H M,FENG Z H,WANG C,et al. Types and geneses of the dolomite reservoirs in lower paleozoic of Gucheng area of Tarim Basin. Petroleum Geology and Oilfield Development in Daqing,2014,33(5):111-116.
[20] 王冠,张云峰,杨柳明,等. 塔里木板块古城4井中奥陶统一间房组的海进序列.微体古生物学报,2011,28(1):137-143. WANG G,ZHANG Y F,YANG L M,et al. Transgressive sequences throughout the Yijianfang formation (Darriwilian, Middle Ordovician)at well Gucheng 4,Tarim block,NW China. Acta Micropaleontologica Sinica,2011,28(1):137-143.
[21] 钱一雄,尤东华. 塔中地区西北部奥陶系白云岩(化)成因分析.新疆石油地质,2006,27(2):146-150. QIAN Y X,YOU D H. An analysis of Ordovician dolomitization origin in northwestern Tazhong area. Xinjiang Petroleum Geology,2006,27(2):146-150.
[22] 李凌,谭秀成,陈景山,等. 塔中北部中下奥陶统鹰山组白云岩特征及成因.西南石油大学学报,2007,29(1):34-36. LI L,TAN X C,CHEN J S,et al. Characteristics and origin of dolostones in Yingshan Formation,Lower and Middle Ordovician, north of central Tarim Basin. Journal of Southwest Petroleum University,2007,29(1):34-36.
[23] 张丽娟,李勇,周成刚,等. 塔里木盆地奥陶纪岩相古地理特征及礁滩分布.石油与天然气地质,2007,28(6):731-737. ZHANG L J,LI Y,ZHOU C G,et al. Lithofacies paleogeographical characteristics and reef-shoal distribution during the Ordovician in the Tarim Basin. Oil & Gas Geology,2007,28(6):731-737.
[24] 胡晓兰,樊太亮,高志前,等. 塔里木盆地奥陶系碳酸盐岩颗粒滩沉积组合及展布特征. 沉积学报,2014,32(3):418-428. HU X L,FAN T L,GAO Z Q,et al. The depositional combination characteristics and distribution of Ordovician carbonate shoals in the Tarim Basin. Acta Sedimentologica Sinica,2014, 32(3):418-428.
[25] 任凭,林畅松,韩剑发,等. 塔中北斜坡鹰山组碳酸盐岩沉积微相特征与演化. 天然气地球科学,2015,26(2):241-251. REN P,LIN C S,HAN J F,et al. Microfacies characteristics and depositional evolution of the Lower Ordovician Yingshan Formation in north slope of Tazhong area,Tarim Basin. Natural Gas Geoscience,2015,26(2):241-251.
[26] 邬光辉,李浩武,徐彦龙,等. 塔里木克拉通基底古隆起构造-热事件及其结构与演化.岩石学报,2012,28(8):2435-2452. WU G H,LI H W,XU Y L,et al. The tectonothermal events, architecture and evolution of Tarim craton basement paleouplifts. Acta Petrologica Sinica,2012,28(8):2435-2452.
[27] 杨鑫,徐旭辉,陈强路,等. 塔里木盆地前寒武纪古构造格局及其对下寒武统烃源岩发育的控制作用. 天然气地球科学, 2014,25(8):1164-1171. YANG X,XU X H,CHEN Q L,et al. Paleotectonics pattern in Pre-Cambrian and its control on the deposition of the Lower Cambrian source rocks in Tarim Basin,NW China. Natural Gas Geoscience,2014,25(8):1164-1171.
[28] 江茂生,朱井泉,陈代钊,等. 塔里木盆地奥陶纪碳酸盐岩碳、锶同位素特征及其对海平面变化的响应. 中国科学:D辑地球科学,2002,32(1):36-42. JIANG M S,ZHU J Q,CHEN D Z,et al. The carbonate strontium and carbon isotope characteristics and response of Ordovician sea level change,Tarim Basin. Science China:Series D Earth Sciences,2002,32(1):36-42.
[29] 胡明毅,钱勇,胡忠贵,等. 塔里木柯坪地区奥陶系层序地层与同位素地球化学响应特征. 岩石矿物学杂志,2010,29(2):199-205. HU M Y,QIAN Y,HU Z G,et al. Carbon isotopic and element geochemical responses of carbonate rocks and Ordovician sequence stratigraphy in Keping area,Tarim Basin. Acta Petrologica et Mineralogica,2010,29(2):199-205.
[30] 马庆佑,吕海涛,蒋华山,等. 塔里木盆地台盆区构造单元划分方案. 海相油气地质,2015,20(1):1-9. MA Q Y,LYU H T,JIANG H S,et al. A division program of structural units in the Paleozoic platform-basin region,Tarim Basin. Marine Origin Petroleum Geology,2015,20(1):1-9.
[31] 厉玉乐,王显东,孙效东,等. 古城低凸起构造演化及有利勘探方向. 大庆石油地质与开发,2014,33(5):97-102. LI Y L,WANG X D,SUN X D,et al. Structural evolution and favorable exploration direction for Gucheng low uplift. Petroleum Geology and Oilfield Development in Daqing,2014,33(5):97-102.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed

塔里木盆地中东部中下奥陶统颗粒滩发育特征及分布

Characteristics and distribution of Lower-Middle Ordovician grain bank in mid-eastern Tarim Basin

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 10

[1]	张本健, 田云英, 曾琪, 尹宏, 丁熊. 四川盆地西北部三叠系须三段砂砾岩沉积特征[J]. 岩性油气藏, 2021, 33(4): 20-28.
[2]	隋立伟. 塔南凹陷古地貌特征对沉积体系和油气分布的影响[J]. 岩性油气藏, 2020, 32(4): 48-58.
[3]	印森林, 陈恭洋, 陈玉琨, 吴小军. 砂砾岩储层孔隙结构模态控制下的剩余油分布——以克拉玛依油田七东1区克下组为例[J]. 岩性油气藏, 2018, 30(5): 91-102.
[4]	刘腾, 王军, 张京思, 张藜, 蔡少武. 地震Wheeler域变换结合时频分析技术用于渤海油田岩性油气藏描述[J]. 岩性油气藏, 2018, 30(3): 124-132.
[5]	陈骥, 姜在兴, 刘超, 许文茂. “源-汇”体系主导下的障壁滨岸沉积体系发育模式——以青海湖倒淌河流域为例[J]. 岩性油气藏, 2018, 30(3): 71-79.
[6]	杨占龙, 肖冬生, 周隶华, 黄云峰, 黄小鹏, 沙雪梅. 高分辨率层序格架下的陆相湖盆精细沉积体系研究——以吐哈盆地西缘侏罗系—古近系为例[J]. 岩性油气藏, 2017, 29(5): 1-10.
[7]	张昌民, 胡威, 朱锐, 王绪龙, 侯国伟. 分支河流体系的概念及其对油气勘探开发的意义[J]. 岩性油气藏, 2017, 29(3): 1-9.
[8]	李晨, 樊太亮, 高志前, 钱小会, 傅巍. 冲积扇高分辨率层序地层分析——以辽河坳陷曙一区杜84块SAGD开发区馆陶组为例[J]. 岩性油气藏, 2017, 29(3): 66-75.
[9]	陈锋，朱筱敏，葛家旺，黎明，吴陈冰洁. 珠江口盆地陆丰南地区文昌组层序地层及沉积体系研究[J]. 岩性油气藏, 2016, 28(4): 67-77，94.
[10]	吴小军，李晓梅，谢丹，孙国强 . 多点地质统计学方法在冲积扇构型建模中的应用[J]. 岩性油气藏, 2015, 27(5): 87-92.
[11]	陈玉琨，王延杰，朱亚婷，刘红现，周玉辉，闫家宁 . 克拉玛依油田七东1 区克下组冲积扇储层构型表征[J]. 岩性油气藏, 2015, 27(5): 92-97.
[12]	江涛，李慧勇，李新琦，许鹏，胡安文. 渤西沙垒田凸起走滑断裂背景下油气成藏特征[J]. 岩性油气藏, 2015, 27(5): 172-175.
[13]	朱筱敏，黄捍东，代一丁，朱世发，陶文芳，刘从印. 珠江口盆地番禺 4 洼文昌组层序格架与沉积体系研究[J]. 岩性油气藏, 2014, 26(4): 1-8.
[14]	胡斌，张靓，季汉成，郭新安，陈栋. 北部湾盆地迈陈凹陷东部物源方向及沉积体系时空演化[J]. 岩性油气藏, 2014, 26(4): 22-27.
[15]	陶文芳，朱筱敏，范乐元，陈贺贺. 苏丹穆格莱德盆地 X 区西斜坡 AG 组—Tendi 组沉积体系分析[J]. 岩性油气藏, 2014, 26(3): 51-58.