fault slip rate

基本解釋

The fault slip rate is an important parameter of describing and measuring the intensity of fault activity.
斷層平均滑動速率是描述和衡量斷層活動強(qiáng)度的一個重要指標(biāo)。
Based on data of field investigation in major area of Lenglongling fault zone, geometric characteristics and slip rate of the fault zone are studied.
根據(jù)對冷龍嶺斷裂重點(diǎn)地段的野外調(diào)查，研究了該斷裂的幾何特征及滑動速率。
The pattern of the progressive evolution of offset streams might indicate that the slip rate of the fault in the same place is relatively constant during a certain period.
斷錯水系的演化圖象則進(jìn)一步提供了在一定時(shí)段內(nèi)，同一地點(diǎn)滑動速率基本穩(wěn)定的線索。