[an error occurred while processing this directive] [an error occurred while processing this directive] [an error occurred while processing this directive]
[an error occurred while processing this directive]
非常规油气

四川盆地营山地区上三叠统须家河组二段水化学特征及其成因

  • 张继伟 ,
  • 王显东 ,
  • 王永超 ,
  • 王志国
展开
  • 中国石油大庆油田有限责任公司勘探开发研究院
张继伟,1989年生,男,工程师,硕士,2015年毕业于中国石油大学(北京),主要从事油气成藏地质综合研究工作。 地址:(163000)黑龙江省大庆市让胡路区油田勘探开发研究院 西部勘探研究室。E-mail : starzjw@163.com

修回日期: 2023-02-09

  网络出版日期: 2023-04-06

Hydrochemical characteristics and genesis of the Upper Triassic Xujiahe 2 Member, Yingshan area, Sichuan Basin

  • ZHANG Jiwei ,
  • WANG Xiandong ,
  • WANG Yongchao ,
  • WANG Zhiguo
Expand
  • Exploration and Development Research Institute, PetroChina Daqing Oilfield Company, Daqing, Heilongjiang 163000, China

Revised date: 2023-02-09

  Online published: 2023-04-06

摘要

上三叠统须家河组是四川盆地天然气勘探的重点层系之一,近年来在营山地区须二段勘探见到了好的效果。沉积盆地中赋存的地层水对于揭示储层成岩作用以及油气的生成和分布具有重要意义。目前在针对营山地区须二段油气成藏的研究成果中,以地层水为研究目标来探索储层成岩和流体活动的鲜见报道。为此,通过对须二段水化学分析数据进行统计、计算开展了地层水化学成分和分布特征的研究;通过对比现今海水蒸发轨迹线得出主要离子的相对富集和贫乏程度并结合典型交汇图版,初步开展了地层水来源及成因的研究。研究结果表明:①研究区须二段水是(Na++K+)、Cl-和Ca2+为主要离子组分的高矿化度、CaCl2型水;②绝大多数地层水样品钠氯系数值小于0.85、变质系数值小于8、脱硫酸系数值为0、阳离子交换指数值大于0.129,反映出地质历史时期须二段封闭性好;③须二段现今地层水呈现高矿化度、Ca2+相对富集而Na+、Mg2+相对贫乏的特征,是地层水的蒸发浓缩作用、阳离子交替吸附作用、斜长石钠长石化以及绿泥石大量形成等共同作用的结果。

本文引用格式

张继伟 , 王显东 , 王永超 , 王志国 . 四川盆地营山地区上三叠统须家河组二段水化学特征及其成因[J]. 天然气勘探与开发, 2023 , 46(1) : 105 -111 . DOI: 10.12055/gaskk.issn.1673-3177.2023.01.013

Abstract

The Upper Triassic Xujiahe Formation functions as one of the key sequences for natural-gas exploration in Sichuan Basin. In recent years, the exploration of Xujiahe 2 Member in Yingshan area has achieved better results. Formation water in sedimentary basins is of great significance for revealing reservoir diagenesis, and hydrocarbon generation and distribution. In existing reservoir-forming achievements on Xujiahe 2 Member, there are few reports on exploring diagenesis and fluid activity based on formation water. Thus, both chemical composition and distribution characteristics of formation water were investigated via counting hydrochemical data about this member. By comparing present-day seawater evaporation marks, some enrichment and depletion degrees of main ions were obtained. Moreover, combined with typical cross-plots, not only source but genesis were analyzed preliminarily for formation water. Results show that (1) with CaCl2 as the main type and (Na++K+), Cl-, and Ca2+ as the main ion components, the formation water in Xujiahe 2 Member features high salinity; (2) for most formation-water samples, both sodium-chloride and metamorphic coefficients are less than 0.85 and 8, respectively, the desulfurization coefficient is 0, and the cation exchange index is more than 0.129, all reflecting a good sealing of this member during its geological history; and (3) the present-day formation water in Xujiahe 2 Member is characterized by high salinity, relatively rich Ca2+, and poorer Na+ and Mg2+, which may be caused by a joint effect including the evaporating concentration of formation water, the adsorption alternating of cations, the albitization of plagioclase, and the massive generation of chlorite.
[an error occurred while processing this directive]

参考文献

[1] GROBE M, MACHEL H G. Saline groundwater in the Münsterland Cretaceous Basin, Germany: Clues to its origin and evolution[J]. Marine and Petroleum Geology, 2002, 19(3): 307-322.
[2] LOWENSTEIN T K, HARDIE L A. Secular variation in seawater chemistry and the origin of calcium chloride basinal brines[J]. Geology, 2003, 31(10): 857-860.
[3] CARPENTER A B. Origin and chemical evolution of brines in sedimentary basins[C]//SPE Annual Fall Technical Conference and Exhibition, 1-3 October1978, Houston, Texas,USA.
[4] HANOR J S, MCINTOSH J C. Are secular variations in seawater chemistry reflected in the compositions of basinal brines?[J]. Journal of Geochemical Exploration, 2006, 89(1-3): 153-156.
[5] 李贤庆, 侯读杰, 张爱云. 油田水地球化学研究进展[J]. 地质科技情报, 2001, 20(2): 51-54.
LI Xianqing, HOU Dujie, ZHANG Aiyun.Advancement of the geochemical study of oilfield water[J]. Geological Science and Technology Information, 2001, 20(2): 51-54.
[6] HANOR J S, MCINTOSH J C. Diverse origins and timing of formation of basinal brines in the Gulf of Mexico sedimentary basin[J]. Geofluids, 2007, 7(2): 227-237.
[7] 曾溅辉, 吴琼, 杨海军, 等. 塔里木盆地塔中地区地层水化学特征及其石油地质意义[J]. 石油与天然气地质, 2008, 29(2): 223-229.
ZENG Jianhui, WU Qiong, YANG Haijun, et al.Chemical characteristics of formation water in Tazhong Area of the Tarim Basin and their petroleum geological significance[J]. Oil & Gas Geology, 2008, 29(2): 223-229.
[8] 佟昕, 马鹏杰, 张世奇, 等. 东濮凹陷文东地区沙三段地层水特征及成岩响应[J]. 断块油气田, 2015, 22(5): 594-599.
TONG Xin, MA Pengjie, ZHANG Shiqi, et al.Characteristics and diagenetic response of Es3 formation water of Wendong Area, Dongpu depression[J]. Fault-Block Oil & Gas Field, 2015, 22(5): 594-599.
[9] 刘方槐, 颜婉荪. 油气田水文地质学原理[M]. 北京: 石油工业出版社, 1991.
LIU Fanghuai, YAN Wansun.Principles of Hydrogeology of Oil & Gas Fields[M]. Beijing: Petroleum Industry Press, 1991.
[10] 赵霞飞, 张闻林. 再论四川盆地须家河组的海相潮汐成因——进一步论证与层序分析[J]. 天然气工业, 2011, 31(9): 25-30.
ZHAO Xiafei, ZHANG Wenlin.A re-discussion on the origins of tidal deposits in the Xujiahe Formation of the Sichuan Basin: Further evidences and sequence analysis[J]. Natural Gas Industry, 2011, 31(9): 25-30.
[11] COUCH E L.Calculation of paleosalinities from boron and clay mineral data[J]. AAPG Bulletin, 1971, 55(10): 1829-1837.
[12] 施振生, 谢武仁, 马石玉, 等. 四川盆地上三叠统须家河组四段—六段海侵沉积记录[J]. 古地理学报, 2012, 14(5): 583-595.
SHI Zhensheng, XIE Wuren, MA Shiyu, et al.Transgression sedimentary records of the Member 4-6 of Upper Triassic Xujiahe Formation in Sichuan Basin[J]. Journal of Palaeogeography, 2012, 14(5): 583-595.
[13] 金惠, 杨威, 谢武仁, 等. 黏土矿物在四川盆地须家河组沉积环境研究中的应用[J]. 石油天然气学报, 2010, 32(6): 17-21.
JIN Hui, YANG Wei, XIE Wuren, et al.Application of clay minerals in sedimentary environmental research of Xujiahe Formation in Sichuan Basin[J]. Journal of Oil and Gas Technology, 2010, 32(6): 17-21.
[14] 文冬光, 沈照理, 钟佐燊. 水–岩相互作用的地球化学模拟理论及应用[M]. 武汉: 中国地质大学出版社, 1998.
WEN Dongguang, SHEN Zhaoli, ZHONG Zuoshen.Theories and Applications of Water-Rock Geochemistry Modelling[M]. Wuhan: China University of Geosciences Press, 1998.
[15] 徐兆辉, 汪泽成, 胡素云, 等. 四川盆地上三叠统须家河组沉积时期古气候[J]. 古地理学报, 2010, 12(4): 415-424.
XU Zhaohui, WANG Zecheng, HU Suyun, et al.Paleoclimate during depositional period of the Upper Triassic Xujiahe Formation in Sichuan Basin[J]. Journal of Palaeogeography, 2010, 12(4): 415-424.
[16] HANOR J S.Physical and chemical controls on the composition of waters in sedimentary basins[J]. Marine and Petroleum Geology, 1994, 11(1): 31-45.
[17] MCCAFFREY M A, LAZAR B, HOLLAND H D.The evaporation path of seawater and the coprecipitation of Brand K+ with halite[J]. Journal of Sedimentary Research, 1987, 57(5): 928-937.
[18] LEE DAVISSON M, CRISS R E.Na-Ca-Cl relations in basinal fluids[J]. Geochimica et Cosmochimica Acta, 1996, 60(15): 2743-2752.
[19] BIRKIE P, GARCIA B M, PADRON C M M. Origin and evolution of formation water at the Jujo-Tecominoacán oil reservoir, Gulf of Mexico. Part 1: Chemical evolution and water-rock interaction[J]. Applied Geochemistry, 2009, 24(4): 543-554.
[20] 沈忠民, 刘四兵, 吕正祥, 等. 川西坳陷中段陆相地层水纵向变化特征及水—岩相互作用初探[J]. 沉积学报, 2011, 29(3): 495-502.
SHEN Zhongmin, LIU Sibing, LV Zhengxiang, et al.Vertical geochemical characteristics of continental formation water and its water-rock interaction in the middle area of western Sichuan depression[J]. Acta Sedimentologica Sinica, 2011, 29(3): 495-502.
[21] 赵杏媛, 何东博. 黏土矿物分析及其在石油地质应用中的几个问题[J]. 新疆石油地质, 2008, 29(6): 756-757.
ZHAO Xingyuan, HE Dongbo.Clay mineral analysis and some problems of application in petroleum geology[J]. Xinjiang Petroleum Geology, 2008, 29(6): 756-757.
[22] 孙治雷, 黄思静, 张玉修, 等. 四川盆地须家河组砂岩储层中自生绿泥石的来源与成岩演化[J]. 沉积学报, 2008, 26(3): 459-468.
SUN Zhilei, HUANG Sijing, ZHANG Yuxiu, et al.Origin and diagenesis of authigenic chlorite within the sandstone reservoirs of Xujiahe Formation, Sichuan Basin, China[J]. Acta Sedimentologica Sinica, 2008, 26(3): 459-468.
文章导航

/

[an error occurred while processing this directive]