摘要
热水锡多金属矿区位于阳春盆地的南缘,以北东-北北东向构造为主,矿(化)体受含矿花岗斑岩体及云英岩化带控制。本文对阳春市热水锡多金属矿区地质特征及找矿标志进行了分析。
Hot water tin polymetallic mining area is located in yangchun southern margin of the basin, north of the east - north north east to structure is given priority to, mine 0 by the ore-bearing granite porphyry and greisenization zone control. In this paper, the yangchun hot tin polymetallic mine geological characteristics and ore-prospecting criteria are analyzed.
出处
《世界有色金属》
2017年第1期192-192,194,共2页
World Nonferrous Metals
关键词
阳春市
热水锡多金属矿
地质特征
找矿标志
yangchun
Hot water tin polymetallic
Geological characteristics
Prospecting marks
