摘要
华安玉又名九龙璧,即色彩鲜艳具条带状构造的(绿帘石)透辉石长英质角岩,其形成主要受地层、构造及侵入岩等因素的控制。从华安玉矿的成因入手,对华安玉矿的成矿机理进行初步探讨。
The Hua＇an Jadestone, also known as Jiulongbi jade, is the bright-coloured epidote or diopside felsic hornfels with aribbon structure. The ore-formation of the Hua＇an Jadestone is controlled by the strata, structures and intrusive rocks. The ore-forming mechanism of the Hua＇an Jadestone is under discussion in the paper according to the cause of its formation.
出处
《福建地质》
2009年第2期115-118,共4页
Geology of Fujian
关键词
成矿机理
初探
华安玉
ore-forming mechanism, preliminary study, the Hua＇an Jadestone
