塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式<sup>*</sup>

doi:10.7605/gdlxb.2017.02.028

古地理学报 ›› 2017, Vol. 19 ›› Issue (2): 364-372. doi: 10.7605/gdlxb.2017.02.028

塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式^*

李源^{1, 2}, 鲁新便³, 蔡忠贤², 张恒², 刘显凤⁴

1 新疆农科院土壤肥料与农业节水研究所,新疆乌鲁木齐 830091。
3中国石化西北油田分公司勘探开发研究院,新疆乌鲁木齐 830011。
3中国石化西北油田分公司勘探开发研究院,新疆乌鲁木齐 830011。
4长江大学地球科学学院,湖北武汉 430100

收稿日期:2016-06-24 修回日期:2016-07-19 出版日期:2017-04-01 发布日期:2017-04-01
通讯作者: 通讯作者简介蔡忠贤,男,1963年生,教授,现在中国地质大学(武汉),主要从事碳酸盐岩储集层地质学研究。E-mail: zxcai@cug.edu.cn。
作者简介:李源,男,1987年生,博士,2016年毕业于中国地质大学(武汉),现在新疆农业科学院主要从事资源管理研究。E-mail: liyuan586287@126.con。
基金资助:
*国家重大基础研究发展项目“973”计划(编号: 2012CB214804)资助

Development model of Hercynian cave system in karst canyon area of Tahe Oilfield, Tarim Basin

Li Yuan^{1, 2}, Lu Xinbian³, Cai Zhongxian², Zhang Heng², Liu Xianfeng⁴

1 Soil Fertilizer and Agricultural Water Saving Research Institute 。of Xinjiang Academy of Agricultural Sciences, Urümqi 830091,Xinjiang;
2 Faculty of Earth Resources,China University of Geosciences(Wuhan),Wuhan 430074,Hubei;
3 Research Institute of Petroleum Exploration & Production, Northwest Company, SINOPEC, Urümqi 830011,Xinjiang;
4 School of Geoscience, Yangtze University, Wuhan 430100,Hubei;

Received:2016-06-24 Revised:2016-07-19 Online:2017-04-01 Published:2017-04-01
About author:About the first author Li Yuan,born in 1987,graduated from China University of Geosciences(Wuhan)in 2016 with his Ph.D. degree. Now he is mainly engaged in resource management at Xinjiang Academy of Agricultural Sciences. E-mail: liyuan586287@126.com.About the corresponding author Cai Zhongxian,born in 1963,is a professor in China University of Geosciences(Wuhan).He is mainly engaged in carbonate reservoir geology. E-mail: zxcai@cug.edu.cn.
Supported by:
Financially supported by the National Basic Research Program(973 Program) of China(No.2012CB214804)

摘要/Abstract

摘要： 塔河油田岩溶峡谷区发育大型岩溶洞穴型储集层,勘探效果较好。基于三维地震资料、钻井资料,并结合地震属性提取技术,对地下岩溶洞穴系统、古地貌、古水文系统进行精细刻画,探讨洞穴形成机理,进而总结洞穴发育模式。研究结果表明: (1)峡谷上游段地表水垂向侵蚀作用强烈,峡谷失去了排水功能演变为干谷,下游段水动力条件减弱。(2)峡谷区岩溶洞穴类型划分为暗河洞穴、峡谷—断裂双控型洞穴。暗河洞穴主要发育在峡谷上游段,与峡谷呈“映射”关系。峡谷—断裂双控洞穴发育于峡谷两侧,垂向上具有多层性特征。(3)综上探讨峡谷区岩溶洞穴形成机理,认为较充足的水源补给条件以及水流强烈的垂向侵蚀溶蚀作用控制了暗河洞穴发育,多期次排泄基面下降以及断裂系统共同控制峡谷—断裂双控洞穴的发育。结合现代恩施地区洞穴系统特征,提出了峡谷地区洞穴发育模式,为下一步洞穴储集层预测和勘探实践提供理论借鉴。

关键词: 古岩溶地貌, 古水系, 洞穴系统, 峡谷, 岩溶模式, 海西期, 塔河油田, 塔里木盆地

Abstract: Giant karst cave reservoir develop in the karst canyon area of Tahe Oilfield,with good explotation result. Through high resolution 3D seismic data,data of drilling and the seismic attributes extracting the karst cave system,palaeo-gemorphology and palaeo-drainage system were rebuilt. The karst development mechanism was discussed and the model of the karst cave were summarized as following: (1)Surface water has strong vertical erosion in upper reaches of the canyon,the canyon lost the drainage function and evolution into dry valley,hydrodynamic conditions in lower reaches of canyon is weaken. (2)Cave types divided into underground water caves,canyon-fault caves,underground water caves development in the upstream of canyon, underground caves and canyon are mapping relationship,canyon-fault caves development on both sides of the canyon,with multilayer characteristics in vertical. (3)With a comprehensive analysis of the karst cave genesis mechanism in the canyon area,we thought that the underground water cave development in an adequate water supply condition and strong vertical erosion of water,canyon-fault caves development in a multiple-stage drop of base level and fault systems. Combined with the characteristics of modern Enshi cave systems. evolutionary model of the karst cave in canyon are proposed,which provides a theoretical reference for further cave reservoir prediction and exploration practice.

Key words: palaeo-karst geomorphology, palaeo-drainage system, cave system, canyon, karst model, Hercynian, Tahe Oilfield , Tarim Basin

中图分类号:

P588.24+5

李源, 鲁新便, 蔡忠贤, 张恒, 刘显凤. 塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式^*[J]. 古地理学报, 2017, 19(2): 364-372.

Li Yuan, Lu Xinbian, Cai Zhongxian, Zhang Heng, Liu Xianfeng. Development model of Hercynian cave system in karst canyon area of Tahe Oilfield, Tarim Basin[J]. JOPC, 2017, 19(2): 364-372.

http://www.gdlxb.cn/CN/Y2017/V19/I2/364

参考文献

1 蔡忠贤,刘永立,段金宝. 2009. 岩溶流域的水系变迁: 以塔河油田6区西北部奥陶系古岩溶为例. 现代地质,28(1): 31-34. [Cai Z X,Liu Y L,Duan J B. 2009. Transition of river system in karst basin: A case study on Ordovician palaeokarst in the northwest of Block 6,Tahe oilfield. Geoscience,28(1): 31-34]
2 何宇彬. 1991. 试论均匀状厚层灰岩水动力剖面及实际意义. 中国岩溶,10(4): 1-12. [He Y B. 1991. Hydrodynamic section of thick homogeneous limestone and its practical significance. Carsologica Sinica,10(4): 1-12]
3 何宇彬. 1994. 试论喀斯特水动力剖面模式. 地球科学—中国地质大学学报,19(1): 119-126. [He Y B. 1994. Comment on karst hydrodynamical section. Earth Science-Journal of China University of Geosciences,19(1): 119-126]
4 焦方正,翟晓先. 2008. 海相碳酸盐岩非常规大油气田: 塔河油田勘探研究与实践. 北京: 石油工业出版社. [Jiao F Z,Zhai X X. 2008. Marine Carbonate Unconventional Oil and Gas Fields: Tahe Oilfield Exploration Research and Practice. Beijing: Petroleum Industry Press]
5 康志宏. 2006. 塔河碳酸盐岩油藏岩溶古地貌研究. 新疆石油地质,27(5): 522-525. [Kang Z H. 2006. The karst palaeogeomorphology of Carbonate Reservoir in Tahe Oilfield. Xinjiang Petroleum Geology,27(5): 522-525]
6 廖涛,侯加根,陈利新,马克,杨文明,董越. 2015. 塔北哈拉哈塘油田奥陶系岩溶储集层发育模式. 石油学报,36(11): 1380-1391. [Liao T,Hou J G,Chen L X,Ma K,Yang W M,Dong Y. 2015. Evolutionary model of the Ordovician karst reservoir in Halahatang oilfield,northern Tarim Basin. Acta Petrolei Sinica,36(11): 1380-1391]
7 廖涛,侯加根,陈利新,马克,杨文明,董越,白晓佳. 2016. 断裂对塔北地区哈拉哈塘油田奥陶系非暴露岩溶缝洞型储集层的控制作用. 古地理学报,18(2): 221-235. [Liao T,Hou J G,Chen L X,Ma K,Yang W M,Dong Y,Bai X J. 2016. Fault controlling on non-exposed karst fracture-vug reservoirs of the Ordovician in Halahatang Oilfield,northern Tarim Basin. Journal of Palaeogeography(Chinese Edition),18(2): 221-235]
8 刘峰. 2010. 湖北省恩施市板桥暗河管道系统特征及成因分析. 成都理工大学硕士论文. [Liu F. 2010. Underground River Piping Characteristics and Genetic Analysis of Banqiao in Enshi City,Hubei Province. Master's Dissertation of Chengdu University of Technology]
9 刘永立,蔡忠贤. 2009. 塔河油田四区奥陶系古岩溶流域的倒淌河及其成因研究. 现代地质,23(6): 1121-1125. [Liu Y L,Cai Z X. 2009. The inverted river and its origin in palaeokarst Drainage Basin of Ordovicician in Block 4,Tahe Oilfield. Geoscience,23(6): 1121-1125]
10 鲁新便,何成江,邓光校,鲍典. 2014. 塔河油田奥陶系油藏喀斯特古河道发育特征描述. 石油实验地质,36(3): 268-274. [Lu X B,He C J,Deng G X,Bao D. 2014. Development features of karst ancient river system in Ordovician reservoirs,Tahe Oilfield. Petroleum Geology & Experiment,36(3): 268-274]
11 桑琴,未勇,程超,黄静,何术坤,郭贵安,吴昌龙,彭祚远. 2012. 蜀南地区二叠系茅口组古岩溶地区水系分布及岩溶地貌单元特征. 古地理学报,14(3): 393-402. [Sang Q,Wei Y,Chen C,Huang J,He S K,Guo G A,Wu C L,Peng Z Y. 2012. Distribution of palaeokarst water system and palaeogeomorphic unit characteristics of the permian Maokou formation in southern Sichaun Province. Journal of Palaeogeography(Chinese Edition),14(3): 393-402]
12 杨明德. 1998a. 喀斯特流域水文地貌系统. 北京: 地质出版社,40-74. [Yang M D. 1998a. Karst River Basin Landform System. Beijing:Geological Pulbishing House, 40-74]
13 杨明德. 1998b. 岩溶峡谷区溶洞发育特征及水动力条件. 中国岩溶,17(3): 187-195. [Yang M D. 1998b. Development of cavities in karstic valley in respondent to hydodynamics. Carsologica Sinica,17(3): 187-195]
14 Bahorich M,Farmer S. 1995. 3D seismic discontinuity for faults and stratigraphic features: The coherence cube.The leading edge,14(10): 1053-1058.
15 Ford D,Williams P. 2007. Karst Hydrogeology and Geomorphology. New York: John Wiley & Sons Ltd., 103-140.
16 Hill C A,Polyak V J. 2005. Progressive lowering of the water table in the Grand Canyon as recorded by cave and mine deposits. Geological Society of America,Abstracts with Programs, 37(6): 16.
17 Hill C A,Eberz N,Buecher R H. 2008. A karst connection model for Grand Canyon,Arizona,USA. Geomorphology,95(3): 316-334.
18 Hill C A,Polyak V J. 2010. Karst hydrology of Grand Canyon,Arizona,USA. Journal of Hydrology,390(3): 169-181.
19 Huntoon P W. 2000. Variability of karstic permeability between unconfined and confined aquifers,Grand Canyon region,Arizona. Environmental & Engineering Geoscience,6(2): 155-170.
20 James N P,Choquette P W. 1988. Paleokarst. New York: Springer Verlag, 227-248.
21 Palmer A N. 2007. Cave Geology. Ohil, USA: Cave books, 74-92.

[1]	刘大卫, 李映涛, 韩俊, 张继标, 汝智星, 杨孝群, 王石, 黄诚, 肖重阳. 塔里木盆地顺北地区奥陶系鹰山组超深层白云岩类型及成储潜力评价^*[J]. 古地理学报, 2025, 27(1): 126-140.
[2]	汪彦, 王诺宇, 杨德彬, 张恒, 张娟, 张长建, 张晓. 塔河油田西北部奥陶系古水系结构特征及演化^*[J]. 古地理学报, 2024, 26(6): 1467-1482.
[3]	贾进华. 塔里木盆地阿瓦提凹陷三叠系层序特征与沉积古地理演化^*[J]. 古地理学报, 2024, 26(4): 763-778.
[4]	张锡婷, 范坤宇, 郭佩, 李鹏真, 苗如霖, 邓宾. 早始新世温室气候与海侵作用对库车坳陷库姆格列木群含盐层系沉积的协同控制作用^*[J]. 古地理学报, 2024, 26(4): 926-940.
[5]	胡宗全, 高志前, 刘旺威, 卫端. 塔里木盆地东北缘兴地断裂以北地区下寒武统富有机质泥页岩沉积环境与发育机制^*[J]. 古地理学报, 2023, 25(6): 1235-1256.
[6]	陈海颖, 张立强. 基于成岩相的深层碎屑岩优质储集层发育规律研究: 以塔里木盆地顺9井区柯坪塔格组为例[J]. 古地理学报, 2023, 25(6): 1379-1393.
[7]	王珊, 曹颖辉, 闫磊, 杜德道, 马德波, 张翔, 陈志勇, 周慧, 杨敏, 白莹. 塔里木盆地中下寒武统蒸发岩沉积特征及发育模式^*[J]. 古地理学报, 2023, 25(4): 889-905.
[8]	钱一雄, 何治亮, 陈代钊, 储呈林, 董少峰, 张庆珍. 塔北埃迪卡拉系奇格布拉克组多类型共生鲕粒特征及其成因探讨^*[J]. 古地理学报, 2023, 25(1): 56-74.
[9]	贾润幸, 方维萱. 塔里木盆地西南部下白垩统克孜勒苏群沉积特征与成矿成藏作用^*[J]. 古地理学报, 2022, 24(5): 1017-1028.
[10]	韩强, 耿锋, 虎北辰, 高山林, 金仙梅, 王玺童, 李振宇. 塔里木盆地中石化探区含氦气藏资源调查研究^*[J]. 古地理学报, 2022, 24(5): 1029-1036.
[11]	林旭, 李玲玲, 刘海金, 陈济鑫. 黄河上游物质在新近纪未流入晋陕峡谷^*[J]. 古地理学报, 2022, 24(3): 568-582.
[12]	陈宇航, 姚根顺, 邵大力, 鲁银涛, 吕福亮, 曹全斌, 唐鹏程, 李仕芳. 坦桑尼亚滨海盆地陆坡峡谷沉积特征及其控制因素^*[J]. 古地理学报, 2021, 23(6): 1158-1173.
[13]	赖锦, 包萌, 刘士琛, 李栋, 王松, 杨科夫, 陈旭, 王贵文, 丁修建. 塔里木盆地深层、超深层白云岩优质储集层测井预测^*[J]. 古地理学报, 2021, 23(6): 1225-1242.
[14]	郑剑锋, 刘禹, 朱永进, 梁峰. 塔里木盆地乌什地区上震旦统奇格布拉克组地球化学特征及其地质意义^*[J]. 古地理学报, 2021, 23(5): 983-998.
[15]	姜应兵, 李兴娟. 塔里木盆地塔河油田TH12402井区中下奥陶统古岩溶洞穴发育模式^*[J]. 古地理学报, 2021, 23(4): 824-836.

选择文件类型/文献管理软件名称

选择包含的内容

塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式^*

Development model of Hercynian cave system in karst canyon area of Tahe Oilfield, Tarim Basin

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式*

Development model of Hercynian cave system in karst canyon area of Tahe Oilfield, Tarim Basin

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

塔里木盆地塔河油田岩溶峡谷区海西早期洞穴系统发育模式^*