Farrell

概述

2 zones (Murchison and Farrell) with several sub-parallel lenticular narrow fissure lodes in shears, massive stratiform, 12 m thick, average 1-2 m. North Mt. Farrell, New North Mt. Farrell deposits. High S isotope values is evidence of volcanic origin. Extensional basin in an arc-continental collision zone.

地质背景

构造环境: Siliciclastic-felsic in mature epicontinental arc

资源与开采

投产年份: 1935

数据溯源

数据来源: USGS MRDS