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断裂带连通性:加利福尼亚州旧金山湾区断层的滑动速率

Fault zone connectivity: slip rates on faults in the san francisco bay area, california.

作者信息

Bilham R, Bodin P

出版信息

Science. 1992 Oct 9;258(5080):281-4. doi: 10.1126/science.258.5080.281.

Abstract

The slip rate of a fault segment is related to the length of the fault zone of which it is part. In turn, the slip rate of a fault zone is related to its connectivity with adjoining or contiguous fault zones. The observed variation in slip rate on fault segments in the San Francisco Bay area in California is consistent with connectivity between the Hayward, Calaveras, and San Andreas fault zones. Slip rates on the southern Hayward fault taper northward from a maximum of more than 10 millimeters per year and are sensitive to the active length of the Maacama fault.

摘要

一个断层段的滑动速率与其所属断层带的长度有关。反过来,一个断层带的滑动速率又与其与相邻或毗连断层带的连通性有关。在加利福尼亚州旧金山湾区观察到的断层段滑动速率变化与海沃德、卡拉维拉斯和圣安德烈亚斯断层带之间的连通性一致。海沃德断层南段的滑动速率从每年超过10毫米的最大值向北逐渐减小,并且对马卡马断层的活动长度很敏感。

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