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福建马坑和阳山是两个伴有多金属(钼)矿化的重要钙矽卡岩型铁矿床,位于永—梅上古生代拗陷东南部的北东向龙漳次一级基底断裂凹陷带中。有关本区钙矽卡岩型铁矿床的一般地质情况、交代矿化特征和生成条件,作者等已于1980年作过介绍。本文着
Fujian Makeng and Yangshan are two important calcium skarn-type iron deposits associated with polymetallic (molybdenum) mineralization. They are located in the NE-trending Longzhang first-order basement fault in the southeastern part of the Yongsmeicuo Paleozoic depression Depression belt. The general geological conditions of calcareous skarn type iron ore deposits in this area, account of mineralization characteristics and formation conditions have been introduced by the author in 1980. This article