HEAT-FLOW ACROSS THE TOE OF ACCRETIONARY PRISMS - THE ROLE OF FLUID FLUX

被引：10

作者：

WANG, CY

LIANG, GP

SHI, YL

机构：

[1] CHINESE ACAD SCI,INST MATH,BEIJING,PEOPLES R CHINA

[2] CHINESE ACAD SCI,GRAD SCH,BEIJING,PEOPLES R CHINA

来源：

GEOPHYSICAL RESEARCH LETTERS | 1993年 / 20卷 / 08期

关键词：

D O I：

10.1029/93GL00331

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

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.

引用

页码：659 / 662

页数：4

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