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HEAT-FLOW ACROSS THE TOE OF ACCRETIONARY PRISMS - THE ROLE OF FLUID FLUX
WANG, CY; LIANG, GP; SHI, YL
1993-04-23
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
卷号20期号:8页码:659-662
摘要Compaction-driven fluid flow in accretionary prisms is ineffective in changing heat flow across the lower slope, even when the rate of fluid flow is greatly enhanced by hydrofracturing, as results of numerical analysis show. For most faults which are long relative to their thickness, conductive heat loss to the wall rock is much more effective in heat transport than advective transport along the faults.
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:A1993LA34200006
出版者AMER GEOPHYSICAL UNION
引用统计
文献类型期刊论文
条目标识符http://ir.amss.ac.cn/handle/2S8OKBNM/27248
专题中国科学院数学与系统科学研究院
通讯作者WANG, CY
作者单位1.CHINESE ACAD SCI,INST MATH,BEIJING,PEOPLES R CHINA
2.CHINESE ACAD SCI,GRAD SCH,BEIJING,PEOPLES R CHINA
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GB/T 7714
WANG, CY,LIANG, GP,SHI, YL. HEAT-FLOW ACROSS THE TOE OF ACCRETIONARY PRISMS - THE ROLE OF FLUID FLUX[J]. GEOPHYSICAL RESEARCH LETTERS,1993,20(8):659-662.
APA WANG, CY,LIANG, GP,&SHI, YL.(1993).HEAT-FLOW ACROSS THE TOE OF ACCRETIONARY PRISMS - THE ROLE OF FLUID FLUX.GEOPHYSICAL RESEARCH LETTERS,20(8),659-662.
MLA WANG, CY,et al."HEAT-FLOW ACROSS THE TOE OF ACCRETIONARY PRISMS - THE ROLE OF FLUID FLUX".GEOPHYSICAL RESEARCH LETTERS 20.8(1993):659-662.
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