碱性地层水对火山碎屑岩改造作用的实验研究

郭欣欣; 刘立; 曲希玉; 蒙启安; 宋土顺; 于淼

doi:10.11781/sysydz201303314

碱性地层水对火山碎屑岩改造作用的实验研究

doi: 10.11781/sysydz201303314

郭欣欣^1,2,
刘立^1, ,,
曲希玉³,
蒙启安⁴,
宋土顺¹,
于淼¹

1.
吉林大学地球科学学院, 长春 130061
2. 东北农业大学资源与环境学院, 哈尔滨 150030
3. 中国石油大学(华东) 地球科学与技术学院, 山东青岛 266555
4. 大庆油田有限责任公司勘探开发研究院, 黑龙江大庆 163712

基金项目: 国家自然科学基金项目(40972075);高等学校博士学科点专项科研基金项目(20090061120043);吉林大学基本科研业务费项目(200903024)

详细信息

作者简介:
郭欣欣(1982- ),女,博士研究生,从事储层地质学研究.E-mail:xinxin8504021@163.com.

通讯作者:
刘立(1955- ),男,教授,博士生导师,从事储层、层序地层及沉积学研究.E-mail: liuli0892@vip.sina.com.

中图分类号: TE122
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出版历程
- 收稿日期: 2012-08-19
- 修回日期: 2013-03-22
- 刊出日期: 2013-05-28

Experimental study on reformation of volcanic clastic rocks by alkaline formation water

Guo Xinxin^1,2,
Liu Li^{1
, ,},
Qu Xiyu³,
Meng Qi'an⁴,
Song Tushun¹,
Yu Miao¹

1.
College of Earth Sciences, Jilin University, Changchun, Jilin 130061, China
2. College of Resources and Environment, North East Agricultural University, Harbin, Heilongjiang 150030, China
3. School of Geosciences, China University of Petroleum, Qingdao, Shandong 266555, China
4. Exploration and Development Research Institute of Daqing Oilfield Ltd Co, PetroChina, Daqing, Heilongjiang 163712, China

摘要

摘要: 以塔木察格盆地火山碎屑岩(流纹质凝灰岩、沉凝灰岩)为研究对象,通过密闭容器中地层水—火山碎屑岩相互作用的水热实验,研究了不同温度下碱性地层水对火山碎屑岩成分的改造.研究显示:在碱性地层水作用下,火山碎屑岩以石英溶解为主,且随着温度的升高,石英的溶解度逐渐加大,而长石及碳酸盐矿物的溶蚀较弱;同时,通过扫描电镜(SEM)的观察发现:流纹质凝灰岩在100,120,140,160℃下样品表面有钙十字沸石生成;沉凝灰岩在100℃时有方解石生成,在120℃和180℃时样品表面有钙十字沸石生成.结合南贝尔凹陷石英保存完好,长石、碳酸盐矿物溶蚀溶解较强的特征,表明碱性流体对该区火山碎屑岩次生孔隙贡献较少.
- 火山碎屑岩 /
- 碱性地层水 /
- 溶解 /
- 水热实验 /
- 南贝尔凹陷 /
- 塔木察格盆地
Abstract: The hydrothermal experiments of volcanic clastic rocks chosen from the Nanbeier Sag of the Tamtsag Basin and formation water were researched under different temperatures in a closed container.The results show that quartz can be dissolved by alkaline formation water and the dissolution intensity will be enhanced with the increasing of temperature;on the contrary,the dissolution degree of feldspar and calcite is very low.Meanwhile,by scanning electronic microscope (SEM),phillipsite is found on the surface of rhyolitic tuff sample (at the temperature of 100,120,140 and 160℃) and sedimentary tuff sample (at the temperature of 120 and 180℃);calcite is found on the surface of sedimentary tuff at 100℃.Considering the good preservation of quartz and strong dissolution of feldspar and carbonate,it is proved that the formation water contributes few to the secondary poro-sity of the Nanbeier Sag of the Tamtsag Basin.
- volcanic clastic rock /
- alkaline formation water /
- dissolution /
- hydrothermal experiment /
- Nanbeier Sag /
- Tamtsag Basin

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参考文献(19)

[1]	王建伟,鲍志东,陈孟晋,等.砂岩中的凝灰质填隙物分异特征及其对油气储集空间影响:以鄂尔多斯盆地西北部二叠系为例[J].地质科学,2005,40(3):429-438.
[2]	张凡芹,王伟锋,王建伟,等.苏里格庙地区凝灰质溶蚀作用及其对煤成气储层的影响[J].吉林大学学报:地球科学版,2006,36(3):365-369.
[3]	曲希玉,刘立,蒙启安,等.大气水对火山碎屑岩改造作用的研究:以塔木查格盆地为例[J].石油实验地质,2012,34(3):285-290.
[4]	曲希玉,刘立,胡大千,等.CO₂流体对含片钠铝石砂岩改造作用的实验研究[J].吉林大学学报:地球科学版,2007,37(4):690-696.
[5]	Amrhein C,Suarez D L.The use of a surface complexation model to describe the kinetics of ligand-promoted dissolution of anorthite at 25℃[J].Geochim et Cosmochim Acta,1988,52(12):278-279.
[6]	Blake R E,Walter L M.Effects of organic acids on the dissolution of orthoclase at 80℃and pH=6[J].Chemical Geology,1996,132(1/4):91-102.
[7]	Hellmann R.The albite-water system:PartⅠ.The kinetics of dissolution as a function of pH at 100,200,and 300℃[J].Geochim et Cosmochim Acta,1994,58(2):595-611.
[8]	Gout R,Oelkers E H,Schott J,et al.The surface chemistry and structure of acid-leached albite:New insights on the dissolution mechanism of the alkali feldspars[J].Geochim et Cosmochim Acta,1997,61(14):3013-3018.
[9]	罗孝俊,杨卫东,李荣西,等.pH值对长石溶解度及次生孔隙发育的影响[J].矿物岩石地球化学通报,2001,20(2):103-107.
[10]	向廷生,蔡春芳,付华娥.不同温度、羧酸溶液中长石溶解模拟实验[J].沉积学报,2004,22(4):597-602.
[11]	Blatt H,Middleton G,Murray R.The Origin of Sedimentary Rocks[M].Second edition.Englewood Cliffs,New Jersey:Prentice&Hall,Inc,1980:332-362.
[12]	曾允孚,夏文杰.沉积岩石学[M].北京:地质出版社,1986:194-199.
[13]	Knauss K G,Wolery T J.The dissolution kinetics of quartz as afunction of pH and time at 70℃[J].Geochimet Cosmochim Acta,1988,52(1):43-53.
[14]	Tester J W,Worley W G.Correlating quartz dissolution kinetics in pure water from 25 to 625℃[J].Geochim Cosmochim Acta,1994,58(11):2407-2420.
[15]	Dove P M.The dissolution kinetics of quartz in sodium chloride solutions at 25°to 300°[J].American Journal of Science,1994,294:665-712.
[16]	Worley W G,Tester J W,Grigsby C O.Quartz dissolution kine-tics from 100-200℃as a function of pH and ionic strength[J].AICHE J,1996,42(12):3442-3457.
[17]	邱隆伟,姜在兴,操应长,等.泌阳凹陷碱性成岩作用及其对储层的影响[J].中国科学:D辑:地球科学,2001,31(9):752-759.
[18]	邱隆伟,姜在兴,陈文学,等.一种新的储层孔隙成因类型:石英溶解型次生孔隙[J].沉积学报,2002,20(4):621-627.
[19]	王小琴.塔木察格盆地南贝尔凹陷火山碎屑岩储层成岩作用.长春:吉林大学,2009