盆地地热场模拟的若干问题探讨

吴冲龙; 李星; 刘刚; 田宜平

doi:10.11781/sysydz199901001

盆地地热场模拟的若干问题探讨

doi: 10.11781/sysydz199901001

中国地质大学, 武汉 430074

基金项目: 国家自然科学基金“九五”重点项目(49732005)的成果之一

详细信息

作者简介:
吴冲龙男 52岁教授 (博士生导师)煤及油气地质、数学地质

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出版历程
- 收稿日期: 1998-08-08
- 刊出日期: 1999-01-25

STUDY ON SOME IMPORTANT PROBLEMS OF GEOTHERMAL FIELD SIMULATION OF BASINS

China University of Geosciences, Wuhan 430074

摘要

摘要: 本文探讨了盆地地热场模拟所面临的诸多难题的解决途径和方法.作者从地下热流状态平衡与破坏的角度出发,用正常地热场的概念来描述常规上地幔热流对地热场的贡献,而用附加地热场的概念来描述岩浆侵入等事件对地热场的贡献;讨论了采用地壳热结构分析来获取盆地基底热流数值的方法,以及根据重力补偿地区的盆地基底与莫霍面的倒影关系所建立的莫霍面埋深经验公式的有效性;以Ungerer等提供的岩石热导率与岩性、地温之间的关系曲线为基础,采用双重回归方法建立了岩石热导率的经验公式.这些方法在一些盆地的地热场模拟中取得了成效.
- 盆地地热场 /
- 地热场模拟 /
- 正常地热场 /
- 附加地热场 /
- 地壳热结构 /
- 莫霍面埋深经验公式
Abstract: Geothermal field simulation is the basis of basin modeling.This paper probes into some difficult problems about geothermal field simulation of basins and their solving method:(1) From the angle of equilibrum and wreck of underground thermal state,the authors adopt the concepts of normal geothermal field and appended geothermal field to describe the contribution of normal crust mantle convection to the geothermal field and the contribution of magmatic intrusion to geothermal field respectively;(2) The authors try to discuss the method of gaining the thermal flow value about basin bottom,that by using analyzing paleo geothermal structure,and also try to discuss the availability of empirical formula for burial depth of Moho surface which is established on the basis of the relationship of inverted image between basin bottom and Moho surface in gravity compensated area;and (3) Based on the relation curve among thermal conductivity,lithologic characters and earth temperature provided by Ungerer etc,the authors establish an empirical formula about the thermal conductivity of rock through double regression.These methods have been applied to simulation of thermal field of several basins.
- geothermal field of basin /
- simulation of geothermal field /
- normal geothermal field /
- appended geothermal field /
- geothermal structure of the earth crust /
- empirical formula of burial depth of Moho surface

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参考文献(20)

[1]	柳少波,顾家裕.包裹体在石油地质研究中的应用与问题讨论.石油与天然气地质,1997,18(4):236～331
[2]	方同辉,马鸿文.建立古地温曲线的理想地质温压计.地质科技情报,1997,16(4):93～100
[3]	汪集等.辽河裂谷盆地地壳-上地幔热结构.中国科学,B辑,1986(3)
[4]	王良书,施央申.油气盆地地热研究.南京:南京大学出版社,1989
[5]	吴冲龙等.中国煤变质作用的热动力学分析.载于:杨起主编的《中国煤变质作用》.北京:煤炭工业出版社,1996:90～149
[6]	吴冲龙.煤变质作用热动力学分析的原理与方法.煤炭学报,1997,22(3):225～229
[7]	Bethke C M.A numerical model of com paction-driven groundw ater flow and heat tran sfer and its application to the paleohyd rology of in tracratonic sedimentary basins.Journal of Geophy sical Research,1985,90:6817～6828
[8]	Black well D D.The structure and physical properties of the Earth's Crust.In:ed.by Heacock J G.,American GeophsicalU-nion,Washington D C:169～184
[9]	Kinsm an D J J.Riftvalley basin and sedimen tary history of Traling Continental margins.In:Petroleum and global tectonics,eds.by Fisher and Jud son,Published by Princeton Un ivesity Press,Princeton and London,1975,83～126
[10]	Mckenzie D.Some Rem arks on the development of sedimentary basins.Earth and Planetary Science Letters,1978,40:25～32
[11]	Morgen P and Sass J H.Thermal regime of the continental litho sphere.J.Geody nam ics,1984,1:143～166
[12]	Morgen P.Structure and evolution of the continental lithosphere.in:Physics and Chemistry of the Earth,ed.by Pollack H N And Murthy V R.Pergamon Press,Oxford,1984,15:107～193
[13]	Pollack H N and Chapm an D S.Mantie heat flow.Earth Planet.Sci.Lett,1977,34:174～184
[14]	Quintard M and Bernard D.Free convection in sediments.in:Them al modeling in sedimentary basins,ed.by Burrus J.,Paris,Editions Technip,1986,271～286
[15]	Rabinowicz M,Kandu rand J L,Jakubow ske M,Schott J and Cassan J P.Convection in a North Sea oil reservoir:inferences on diagenesis and hydrocarbon migration.Earth and Planetary S cience Letters,1985,74:387～404
[16]	Royden L and C E Keen.Rifting process and therm al evolution of the continental margin of eastern Canada determined from sub sidence curves.Earth and Planetary Science L etters,1980,51:342～361
[17]	Sass J H et al.Heat flow from the crust of the United State,Chap ter 13.in:Physical Properties of rocks and minerals,ed.by Tou lou Y S,Judd W R and Ror R F.McGraw Hill,New York,1981
[18]	Ungerer P Burrus J,Do ligez B,Chenet P Y and Bessis F.Basin evaluation by integrated two-dimen sional modeling of heat trasfer,fluid flow,hydrocarbon generation,and migration.A A PG,1990,74(3):309～335
[19]	Willet S D and Chapm an D S.Temperatures,fluid flow and therm al history of the Uinta basin.in:Migration of hydrocar-bons in sed imentary basins,Ed.by Do ligez B.Paris,Edetions Technip,1987,533～552
[20]	Wu Chong long,Li Sitian and Cheng Shou tian.The statistical prediction of the vitrinite reflectance and study of ancient geothem al field in Songliao Basin,China.J ournal of China Unversity of Geosciences,1991,2(1):91～101