摘要
辽宁省白云金矿区遭受了长期的构造—岩浆热事件影响 ,形成了复杂的构造形迹。其演化大致可划分为早期塑性流变、中期韧性剪切、后期脆性断裂等阶段。金矿属岩浆热液型 。
As long as long time ago,the Baiyun Gold Deposit suffered long term's accendent of magma hydrothermalism which influcenced the gold doposit into a conplex one.The evolution could be devided into three stages.1.e.early term's plastic transportation,medium term's tough shear and late term's britlleness fracture.Its direct ore control tectonies is britlleness fracture.
出处
《黄金》
CAS
2002年第5期4-7,共4页
Gold
关键词
塑性流变
韧性剪切
脆性断裂
白云金矿床
辽宁
plastic tranformation
tough shear
britlleness fracture
Baiyun gold deposit
Liaoning Province
