摩天岭古陆地壳演化与金矿床的分带

CRUSTAL EVOLUTION AND ZONING OF GOLD DEPOSITS IN MOTIANLING ANCIENT LAND

研究区地壳演化分四个阶段：结晶基底形成阶段（Ａｒ２－Ｐｔ１）；板块多次俯冲碰撞和火山喷发阶段（Ｐｔ２～３）；板块碰撞和岩浆侵入阶段（Ｐｚ）；板块碰合与新构造运动阶段（Ｍｚ－Ｋｚ）。金矿床分布可分三条带：北带，金－镍－钴和金－黄铁矿带；中带，金－多金属矿带；南带，金－铜矿带。

The crustal evolution is divided into four stages: the forming of crystalline basement (Ar2-Pt1); multiple subduction and collision of plates and volcanic eruption (Pt2￣3); collision of plates and magmatic intrusion (Pz); collision and junction of plates and new tectogenesis period (Mz-Kz). The gold deposits can be divided into north zone: AuNi and Aupyrite zones; middle zone: Aupolymetallic zone and south zone: AuCu zone.