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地球科学进展  2000, Vol. 15 Issue (5): 583-585    DOI: 10.11867/j.issn.1001-8166.2000.05.0583
综述与评述     
热对流成岩作用的基本特征与研究意义
刘 立,于均民,孙晓明,杨庆杰
①吉林大学朝阳校区地球科学学院,吉林 长春 130061;②西北地质研究所,甘肃 兰州 730020;③大港油田集团有限责任公司地质勘探开发研究院,天津 大港 300280;④大庆石油管理局勘探开发研究院,黑龙江 大庆 163712
BASIC CHARACTERISTICS OF THERMAL CONVECTION DIAGENESIS AND ITS RESEARCH SIGNIFICANCE
LIU Li, YU Jun-min,SUN Xiao-ming, YANG Qing-jie
(①College of the Earth Science,Chaoyang School District of Jilin University,Changchun 130026,China;②North West Geology Institute,Lanzhou 730020,China;③Geological Exploration&Development Research Institute,Dagang Oilfield Group Ltd.Co,Dagang 300280,China;④Exploration&Development Research Institute,Daqing Petroleum Administrative Bureau,Daqing 163712,China
 全文: PDF(238 KB)  
摘要:

介绍了热对流产生的条件与地质背景,指出火成侵入体、盐丘和活跃断层周围等温线陡倾斜场所易发生热对流成岩作用。综述了岩浆成因热对流的岩石学记录,包括热变质作用、突然升温—逐渐降温的自生矿物组合和相对高温的自生矿物类型,分析了自生伊利石的K/Ar年龄在热对流成岩作用研究中的作用。阐述了热对流成岩作用对盆地动力学、砂岩储层和油气运移研究的意义。

关键词: 热对流热对流成岩作用盆地流体热对流的岩石学记录自生伊利石的K/Ar年龄    
Abstract:

As a new research field of fluids-rock interaction, the thermal convection diagenesis is developing under the basis of basin-geofluids research. This paper introduces the condition and geological settings for the thermal convection diagenesis taking place, points out that the places around igneous intrusions or around salt domes or active faults are subjected to diagenetic reaction. The authors comprehensively discuss the lithologic records of thermal convection caused by magma activity, including thermal contact metamorphic rock, thermal alterated rock, the authigenic minerals assemblages of temperature suddenly increasing-temperature gradually decreasing, relatively higher temperature authigenic minerals,analyses the importance of the K/Ar age of authigenic illite in the research of thermal convection diagenesis. The authors also emphases the significance of thermal convection diagenesis research in the field of basin dynamics, the reservoir of sandstone and migration of petroleum.

Key words:  Thermal convection    Thermal convection diagenesis    Basin geofluids    The lithologicrecords of thermal convection    K/Ar age of authigenic illite.
收稿日期: 1999-11-17 出版日期: 2000-10-01
:  P588.1  
基金资助:

国家教育部博士点科学基金项目“裂谷盆地中砂岩的热对流成岩作用及其动力学机制研究”(编号:1999018707)资助。

通讯作者: 刘立(1955-),男,内蒙古喜桂图旗人,教授,主要从事储层沉积地质学和盆地动力学研究。    
作者简介: 刘立(1955-),男,内蒙古喜桂图旗人,教授,主要从事储层沉积地质学和盆地动力学研究。
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引用本文:

刘 立,于均民,孙晓明,杨庆杰. 热对流成岩作用的基本特征与研究意义[J]. 地球科学进展, 2000, 15(5): 583-585.

LIU Li, YU Jun-min,SUN Xiao-ming, YANG Qing-jie. BASIC CHARACTERISTICS OF THERMAL CONVECTION DIAGENESIS AND ITS RESEARCH SIGNIFICANCE. Advances in Earth Science, 2000, 15(5): 583-585.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2000.05.0583        http://www.adearth.ac.cn/CN/Y2000/V15/I5/583

[1] Lawrence S R, Cornford C. Basin geofluids[J]. Basin Research, 1995, 57: 1~7.
[2] Dickinson W R.沉积盆地动力学[A].见:李思田,王华,路凤香主编.盆地动力学——基本思路与若干研究方法[C].武汉:中国地质大学出版社,1999.190~199.
[3] Wood J R, Heweett T A. Fluid convection and mass transfer in porous sandstones—a theoretical model[J]. Geochim Cosmochim Acta, 1982, 46: 1 707~1 713.
[4] Wood J R, Heweett T A. Reservoir diagenesis and convective fluid flow[A]. In: MeCdonald D A, Surdam R C, eds. Clastic Diagenesis[C]. AAPG, Memoir37, 1984.99~110.
[5] Davis S H, Rosenblat S, Wood J R,et al. Convective fluid flow and diagenetic patterns in domed sheets[J]. American Journal of Science, 1985, 285:207~223.
[6] Bjфrlykke K, Mo A, Palm E. Modelling of thermal convection in sedimentary basins and its relevance to diagenetic reactions[J]. Marine and Petroleum Geology, 1988, 5:338~350 .
[7] Girard J-P, Deynoux M, Nahon D. Diagenesis of the upper Proterozoic siliciclastic sediments of the Taoudeni Basin (west Africa) and relation to diabase emplacemet[J]. Journal of Sedimentary Petrology, 1989, 59:233~248.
[8] Merino E, Gierre J-P, May M T,et al. Diagenetive mineralogy, geochemistry, and dynamics of Mesozoic arkoses, Hartford rift basin, Connecticut, USA [J]. Journal of Sedimentary Petrology, 1997, 67:212~224.
[9] Summer N S, Verosub K L. Diagenesis and organic maturation of sedimentary rocks under volcanic strata,Oregon[J].Am Assoc Pet Geol Bull, 1994, 76: 1 190~1 199.
[10] Liu Li, Yu Junmin. Petrographic studies on hydrothermally altered conglomerates at Naer Creek, Sichuan Province, China[J]. Journal of Geoscientific Research in Northeast Asia,1999,2:1~6.
[11] De Ros L F. Heterogeneous generation and evolution of diagenetic quartarenites in the Silurian—Devonian Furnas Formation of the Parana basin, southern Brazil[J]. Sedimentary Geology, 1998, 116: 99~128.
[12] Bjфrlykke K. Fluid flow processes and diagenesis in sedimentary basins[A]. In:Parnell J, ed. Geofluids: origin, Migration, and Evolution of Fluids in Sedimentary Basins[C]. Geol Soc Lond Spec Publ 78,1994.127~140.
[13] Boles J R, Franks S G. Clay diagenesis in Wilcox sandstones of southwest of Texas: implications of smectite diagenesis on sandstone cementation[J]. Journal of Sedimentary Petrology, 1979, 49: 55~70.
[14] Price L C. Aqueous solubility of crude oil to 400℃and 2,000 bars pressure in the presence of gas[J]. Journal of Petroleum Geology, 1981, 4: 195~223.
[15] Rabinowicz M D, Danurand J-L, Jakubowski,et al. Convection in a North Sea oil reservoir: influnence on diagensis and hydrocarbon migration[J]. Earth and Planetary Science Letters, 1985, 74: 387~404.

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