作者: E.D. Dempsey , R.E. Holdsworth , J. Imber , A. Bistacchi , G. Di Toro
DOI: 10.1016/J.JSG.2014.04.009
关键词:
摘要: Abstract Interconnected networks of faults and veins filled with hydrothermal minerals such as zeolite are widespread in many orogenic terrains. These fractures commonly form at relatively low temperatures (e.g.