塔中北坡奥陶系鹰山组热液改造型储层特征及发育模式

韩俊; 吕海涛; 曹自成; 邱华标; 王保才; 沙旭光; 刘军

doi:10.11781/sysydz2014S1018

塔中北坡奥陶系鹰山组热液改造型储层特征及发育模式

doi: 10.11781/sysydz2014S1018

中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011

详细信息

作者简介:
韩俊(1983-), 男, 硕士, 工程师, 从事碳酸盐岩储层研究工作.E-mail:278511010@qq.com.

中图分类号: TE2
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出版历程
- 收稿日期: 2014-10-15
- 修回日期: 2014-12-03
- 刊出日期: 2014-12-28

Characteristics and development model of hydrothermal alteration reservoir of Ordovician Yingshan Formation in northern slope of central Tarim Basin

Research Institute of Petroleum Exploration and Production, SINOPEC Northwest Company, Urumqi, Xinjiang 830011, China

摘要

摘要: 塔中北坡中下奥陶统鹰山组碳酸盐岩发育热液石英、板条状石膏、鞍型白云石等典型的低温热液矿物组合.对不同类型的石英包裹体测温,其温度范围明显高于地温演化的最高温度.分析了典型钻井鹰山组储层分布与本区潜在不整合面的关系,认为鹰山组储层为热液改造成因,与大气水岩溶作用关系不大.鹰山组热液改造型储层储集空间以孔洞(洞穴)、(扩溶)裂缝等次生储集空间为主,基质物性总体低孔低渗,可划分为洞穴型、孔洞—裂缝型和孔隙型3种类型.分析了鹰山组热液改造型储层的主控因素,提出断裂—裂缝体系是储层发育的前提条件,加里东晚期—海西期北东向、北东东向主干走滑断裂及次级隐伏断裂控制储层平面分布,深部热液流体改造储层,流体性质及岩性结构可能控制了储层纵向分布,初步建立了储层发育模式.该类储层发育厚度大,且受埋深影响不大,沿主干、次级断裂广泛发育,是塔里木盆地碳酸盐岩天然气勘探的一个新领域.
- 热液改造型储层 /
- 发育模式 /
- 塔中北坡 /
- 塔里木盆地
Abstract: In the Middle-Lower Ordovician Yingshan Formation in the northern slope of the central Tarim Basin, typical epithermal hydrothermal mineral assemblages, such as hydrothermal quartz, lath gypsum and saddle dolomite, were found in carbonate rocks. For different types of quartz inclusions, measured temperature was significantly higher than maximum evolution temperature. The relation between the Yingshan reservoir distribution in typical wells and the potential unconformities in the study area was studied, indicating that the Yingshan reservoirs generated from hydrothermal alteration, rather than the karstification of meteoric water. The main space of the Yingshan reservoirs was secondary hole (cave) and expansion fracture, with low porosity and permeability. They were divided into 3 types: hole type, hole-fracture type and pore type. Analysis of the main controlling factors of hydrothermal alteration reservoir showed that fault-fracture system was a precondition for reservoir deve-lopment, and the NE and NEE main strike-slip faults of the late Caledonian-Hercynian and the secondary faults controlled the plane distribution of hydrothermal reservoir. Deep hydrothermal fluid altered reservoir, and fluid properties and reservoir lithologic structure controlled the vertical distribution of hydrothermal reservoir. The development model of hydrothermal alteration reservoir was established. Hydrothermal alteration reservoirs, which were featured by big thickness, little affected by depth, and widely developed along main and secondary faults, were new gas exploration fielda of carbonate rocks in the Tarim Basin.
- hydrothermal alteration reservoir /
- developmenl model /
- northern slope of central Tarim /
- Tarim Basin

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参考文献(32)

[1]	朱光有,张水昌,王欢欢,等.塔里木盆地北部深层风化壳储层的形成与分布[J].岩石学报,2009,25(10):2384-2398.
[2]	马永生,蔡勋育,赵培荣.深层、超深层碳酸盐岩油气储层形成机理研究综述[J].地学前缘,2011,18(4):181-192.
[3]	马永生,蔡勋育,赵培荣,等.深层超深层碳酸盐岩优质储层发育机理和三元控储模式[J].地质学报,2010,84(8):1087-1094.
[4]	郭建华.塔北、塔中地区下古生界深埋藏古岩溶[J].中国岩溶,1996,15(3):207-216.
[5]	陈学时,易万霞,卢文忠.中国油气田古岩溶与油气储层[J].沉积学报,2004,22(2):244-253.
[6]	刘忠宝,于炳松,李廷艳,等.塔里木盆地塔中地区中上奥陶统碳酸盐岩层序发育对同生期岩溶作用的控制[J].沉积学报,2004,22(1):103-109.
[7]	康玉柱.塔里木盆地寒武—奥陶系古岩溶特征与油气分布[J].新疆石油地质,2005,26(5):472-450.
[8]	苗继军,贾承造,邹才能,等.塔中地区下奥陶统岩溶风化壳储层特征与勘探[J].天然气地球科学,2007,18(4):497-500.
[9]	陈新军,蔡希源,纪友亮,等.塔中奥陶系大型不整合面与风化壳岩溶发育[J].同济大学学报:自然科学版,2007,35(8):1122-1127.
[10]	杨海军,韩剑发,孙崇浩,等.塔中北斜坡奥陶系鹰山组岩溶型储层发育模式与油气勘探[J].石油学报,2011,32(3):199-205.
[11]	罗亚男,罗新生,张云峰,等.塔中北斜坡下奥陶统鹰山组热液岩溶特征及发育模式[J].重庆科技学院学报:自然科学版,2012,14(3):19-22.
[12]	朱东亚,金之钧,胡文瑄.塔中地区热液改造型白云岩储层[J].石油学报,2009,30(5):698-704.
[13]	吕修祥,杨宁,解启来,等.塔中地区深部流体对碳酸盐岩储层的改造作用[J].石油与天然气地质,2005,26(3):284-289.
[14]	王嗣敏,金之钧,解启来.塔里木盆地塔中45井区碳酸盐岩储层的深部流体改造作用[J].地质论评,2004,50(5): 543-546.
[15]	吴茂炳,王毅,郑孟林,等.塔中地区奥陶纪碳酸盐岩热液岩溶及其对储层的影响[J].中国科学:D辑:地球科学,2007,37(增刊1):83-92.
[16]	赵霞.塔里木盆地塔中45井及柯坪西克尔萤石成因讨论[J].西北地质,2000,33(3):5-8.
[17]	张兴阳,顾家裕,罗平.塔中45井萤石成因与油气成藏[J].新疆石油地质,2004,25(5):479-482.
[18]	张兴阳,顾家裕,罗平,等.塔里木盆地奥陶系萤石成因及其油气地质意[J].岩石学报,2006,22(8): 2220-2228.
[19]	张兴阳,张水昌,罗平,等.塔中地区晚燕山—喜马拉雅期油气调整与热液活动的关系[J].科学通报,2007,52(增刊1):192-198.
[20]	邬光辉,李启明,张宝收.塔中Ⅰ号断裂坡折带构造特征及勘探领域[J].石油学报,2005,26 (1): 27-30.
[21]	李传新,贾承造,李本亮,等.塔里木盆地塔中低凸起北斜坡古生代断裂展布与构造演化[J].地质学报,2009,83(8):1065-1073.
[22]	杨海军,韩剑发,陈利新,等.塔中古隆起下古生界碳酸盐岩油气复式成藏特征及模式[J].石油与天然气地质,2007,28(6):784-790.
[23]	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[J].海相油气地质,2014,19(2):15-22.
[24]	邵龙义,韩俊,马锋,等.塔里木盆地东部寒武系白云岩储层及相控特征[J].沉积学报,2010,28(5):953-961.
[25]	朱东亚,金之钧,胡文瑄,等.塔里木盆地深部流体对碳酸盐岩储层影响[J].地质论评,2008,54(3):348-354.
[26]	金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-253.
[27]	潘文庆,刘永福,Dickson,等.塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型[J].沉积学报,2009,27(5):983-994.
[28]	Qiu Nansheng, Jian Chang, Yinhui Zuo, et al.Thermal evolution and Lower Paleozoic source rocks maturation in the Tarim Basin, Northwest China[J].AAPG Bulletin,2012,96(5):789-821.
[29]	孟庆强,朱东亚,胡文瑄,等.热力学和动力学双重控制下的大气降水溶蚀—充填机制[J].中国科学:D辑:地球科学,2013,43(11):1797-1806.
[30]	N P 詹姆斯, P W 肖凯. 古岩溶[M].胡文海,胡征钦译. 北京:石油工业出版社,1992.
[31]	Jr Smith L B,G R Davies.Structurally controlled hydrothermal alteration of carbonate reservoirs: introduction[J].AAPG Bulletin, 2006,90(11):1635-1640.
[32]	Jr Smith L B.Origin and reservoir characteristics of Upper Ordovician Trenton-Black River hydrothermal dolomite reservoirs in New York[J].AAPG Bulletin,2006,90(11): 1691-1718.