论文部分内容阅读
一九四九年详查铜陵铜官山鸡冠山区域时,在狮子山铜矿之氧化带内见有橄榄绿色之矿物生於石英脉之晶硐及裂缝内,该脉系穿插於三叠纪石灰岩及闪长岩侵入体之富含柘榴在接触带中,近处有白钨矿及黄铜矿,经室内吹管分析及显微化学试验,知其兼含铜钨,又作简单物理性检定,发浅蓝色萤光,後经陈四箴先生之定量分析,证明其为钨铜钙矿,在中国系初次发现,其成分与智利等处所产相彷,此系次生矿物,大致原生铜矿物受地表氧化时,含铜溶液与白钨矿相遇即可生成。
When a detailed examination of the Tongguanshan area in Tongguan, Tongling, in 1949, an olive-green mineral was found in the quartz veins and cracks in the oxidation zone of the Lion Rock copper mine, this vein was interspersed in the Triassic Limestone and diorite intrusions rich in pomegranate in contact with the zone, the vicinity of scheelite and chalcopyrite, the indoor analysis and microscopy of the blow pipe, known as both copper and tungsten, but also for a simple physical test , Made of light blue fluorescent, after the quantitative analysis of Mr. Chen Sizhen proved that it is tungsten copper calcium ore, first discovered in China, its composition and Chile and other places produced similar to this secondary minerals, roughly copper ores Material by the surface oxidation, the solution containing copper and scheelite encounter can be generated.