作 者: ;
机构地区: 中山大学地球科学系
出 处: 《南方钢铁》 2000年第2期12-14,共3页
摘 要: 论述了广东信宜东田—白马矿田金矿床的空间分布及主要矿床特征 ,并指出断裂带、断裂面的波形变化和加里东期片麻状黑云母花岗岩为主要的控矿因素 . The spatial distribution and main geological characteristics of the gold deposits at Dongtian_Baima mine in Xinyi are described in the present discussion. It is shown that the main factors controlling the deposits are the fracture zones, change in the fracture surface waves and Caledomian gneissic biotite granites.