This name is given to a process that can only occur in faults with very low normal stresses, or in faults lined with very ductile or weak material, such as fault gouge, which acts as a fault lubricant; that process is also known as aseismic slip.
This name is given to a process that can only occur in faults with very low normal stresses, or in faults lined with very ductile or weak material, such as fault gouge, which acts as a fault lubricant; that process is also known as aseismic slip. This name is also given to an eolian process which slowly moves heavy sand grains as they are hit by lighter, saltating grains. This term is also used to refer to a process similar to solifluction, which consists of a movement of less than one centimeter per year of unconsolidated flow. FTP, give the common term for continuous sliding of a fault, and the gradual downhill movement of regolith and soil.
This name is given to a process that can only occur in faults with very low normal stresses, or in faults lined with very ductile or weak material, such as fault gouge, which acts as a fault lubricant; that process is also known as aseismic slip.
creep (accept aseismic slip before mention in the question)