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前言 多年来,在辽东地区的老变质岩中相继发现了铜-锌矿床和矿化点四十余处,其中,工业价值最大的为红透山铜矿。它是我国典型的深变质块状硫化物矿床,赋存于太古界鞍山群的黑云角闪斜长片麻岩中。同位素年龄为27.70亿年(Pb_(206)～Pb_(207)法)～28.84亿年(Rb～Sr法)。 红透山地区在区域变质过程中产生了两次大的褶皱。第一次形成了展布较宽的东西
Foreword Over the years, more than 40 copper-zinc deposits and mineralization sites have been discovered in the old metamorphic rocks of the Liaodong area. Among them, the Hongtoushan copper mine has the largest industrial value. It is a typical deep metamorphic massive sulfide deposit in China, occurring in the biotite hornblende gneiss in the Archean Anshan Group. The isotopic age is 277 million years (Pb 206 Pb Pb 207) -2884 million years (Rb Sr method). The Hongtoushan area produced two large folds during regional metamorphism. For the first time formed a wider distribution of things