福建省溪口组新祠角岩段的角岩(化)成因探讨  

Discussion on Genesis of Hornfels in Xinci Hornfels Member of Xikou Formation, Fujian

作　　者：林主清 陈斯盾[1] 杨玲雅[1] 揭育金[1] 

机构地区：[1]福建省区域地质调查队,三明365001

出　　处：《福建地质》2002年第4期246-251,共6页Geology of Fujian

摘　　要：福建省早三叠世溪口组新祠角岩段 ,常为热液多金属矿产及非金属矿产的含矿层位 ,其角岩 (化 )主要为火山 -沉积及热液蚀变Xinci hornfels member of Xikou formation in Fujian is often ore bearing bed of the hydrothermal polymetallic ore and nonmetallic ore, the genesis of hornfels is mainly volcangenic and hydrothermal alteration

关 键 词：角岩 火山-沉积成因 溪口组 福建 化学成分 

分 类 号：P581[天文地球—岩石学]