GEOLOGIC BACKGROUND FOR EVALUATING SURFACE-FAULTING HAZARDS

Yasutaka IKEDA

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GEOLOGIC BACKGROUND FOR EVALUATING SURFACE-FAULTING HAZARDS

机译：评估表面破坏危险的地质背景

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Geologic observations have indicated that moderate- to large-scale faults have moved repeatedly in the recent geologic past. This allows us to evaluate the future behavior of a fault based on geologic information. In this paper, the essential characteristics of active faults are reviewed, and problems in evaluating surface faulting by using geologic information are discussed.

机译：地质观测表明，在近期的地质历史中，中大型断层已经反复发生。这使我们能够根据地质信息评估断层的未来行为。本文综述了活动断层的基本特征，并讨论了利用地质信息评估地表断层的问题。

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来源
《Structural engineering earthquake engineering》 |2002年第2期|p.143s-147s|共5页
作者
Yasutaka IKEDA;
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作者单位

Department of Earth and Planetary Science, University of Tokyo (Hongo 7-3-1, Bunkyo-ku, Tokyo 113-0033, Japan);

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原文格式 PDF
正文语种 eng
中图分类建筑施工;
关键词
active faults; surface faulting; tectonics; paleoseismology; slip rate; secondary faults; blind faults;

机译：活动断层;表面断层;构造;古地震学;滑移率;二次断层;盲断;

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GEOLOGIC BACKGROUND FOR EVALUATING SURFACE-FAULTING HAZARDS

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