杜荒岭金矿赋存于燕山晚期的石英闪长（斑）岩中，严格受近EW向断裂构造带控制。
Duhuangling gold deposits occurred in the quartz diorite(porphyry)of Late Yanshan Epoch, the deposits are directiy controlled by EW trending fault structure zone.
杜荒岭金矿赋存于燕山晚期的石英闪长（斑）岩中，严格受近EW向断裂构造带控制。
Duhuangling gold deposits occurred in the quartz diorite(porphyry)of Late Yanshan Epoch, the deposits are directiy controlled by EW trending fault structure zone.
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