Data resulting from slide-hold-slide friction experiments on three types of carbonate faults rocks.

This data set is corresponding to the Park, Y., Hirose, T., and Ree, JH, "<em>Carbonate fault mirrors with extremely low frictional healing rates: A possible source of aseismic creep</em>" Geophysical Research Letters, 2021. The data set shows that carbonate fault mirrors have significantly low (near-zero) frictinoal healing rates, while newly formed gouges and gouges generated from destroyed fault mirrors have high frictional healing rates. This results have significant implications on modeling aseismic creep of carbonate fault zones having multiple fault mirror patches.

本数据集对应于Park Y、Hirose T与Ree JH于2021年发表在《地球物理研究快报》（Geophysical Research Letters）的论文《碳酸盐断层镜面（carbonate fault mirrors）具有极低摩擦愈合速率（frictional healing rate）：无震蠕滑（aseismic creep）的潜在来源》。本数据集显示，碳酸盐断层镜面的摩擦愈合速率显著偏低（接近零），而新形成的断层泥（gouge）以及由受损断层镜面产生的断层泥则拥有较高的摩擦愈合速率。该研究结果对于构建带有多块断层镜面区域的碳酸盐断层带无震蠕滑模型具有重要意义。