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1978年12月1日至10日铀矿地质科技情报网在韶关召开了花岗岩型铀矿床成因学术讨论会。目的是交流科研成果,探索成矿规律及找矿方向,活跃学术空气,促进铀矿地质事业发展。会议代表共七十余人,都是在花岗岩地区工作多年的地质工作者,还邀请了贵阳地化所、南大地质系、成都地院三系、抚州地院、705队和755队的代表莅临指导。会议上对花岗岩型铀矿床的成因提出了不同的看法,概括起来有以下三种观点:1.岩浆热液说,根据矿田中花岗岩体的演化及成岩与成矿的时、空连续性(一般谈岩矿时差大都是指主体侵入期与成矿时差,实际上主侵入期后
December 1, 1978 to 10 uranium Geology and Technology Information Network held in Shaoguan granite-type uranium deposit genesis seminars. The purpose is to exchange scientific research achievements, explore mineralization laws and prospecting directions, activate academic atmosphere and promote the development of uranium geological undertakings. A total of more than 70 representatives of the conference, are geologists working in granite area for many years, also invited the Guiyang Institute of Geochemistry, South University Department of Geology, Chengdu courtyard three lines, Fuzhou ground, 705 teams and 755 team representatives come guide. At the conference, different opinions on the genesis of the granitic uranium deposit were put forward, and summarized as follows: 1. Magmatic hydrothermal fluids said that according to the evolution of granitoids and the time and diagenesis of ore bodies and their mineralization, Talking about the time difference between rock and mine mostly refers to the main period of invasion and mineralization, in fact, after the main invasion period