Science. 1966 Aug 26;153(3739):990-2. doi: 10.1126/science.153.3739.990.
Stick-slip often accompanies frictional sliding in laboratory experi ments with geologic materials. Shallow focus earthquakes may represent stick slip during sliding along old or newly formed faults in the earth In such a situation, observed stress drops repre sent release of a small fraction of the stress supported by the rock surround ing the earthquake focus.
在地质材料的实验室实验中，黏滑现象通常伴随着摩擦滑动。浅源地震可能代表着在地球旧断层或新形成的断层上滑动时的黏滑现象。在这种情况下，观测到的应力降代表着地震震源周围岩石所承受的一小部分应力的释放。
