Open AccessLab Experiments Show How Fault Surfaces Get Groovy
Author(s) -
Sarah Stanley
Publication year - 2017
Publication title -
eos
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/2017eo075601
Subject(s) - fault (geology) , computer science , reliability engineering , geology , engineering , seismology
Formation of nanometer-scale quartz beads could promote linear “slickenline” patterns and facilitate fault movement.