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福建省燕山旋回的成矿系列由(1)与混合岩化作用有关的成矿类型、(2)与重熔花岗岩有关的成矿类型、(3)与同熔花岗岩有关的成矿类型、(4)与超基性、基性岩有关的成矿类型、(5)与火山作用有关的成矿类型和(6)与层控有关的成矿类型等六种成矿类型组成。除第二种类型主要分布在本省西部外,其他均主要分布在东部。岩浆活动受NE、NW、ENE、E—W及N—S向断裂构造控制,而以前二者为主。火山喷发中心常出现在NE向断裂构造与NW或ENE向断裂构造交汇处。燕山旋回的成矿作用与其构造岩浆活动有关。本文最后提出了本成矿系列的成矿模式和成矿预测。
The metallogenic series of the Yanshan cycle in Fujian Province consists of (1) metallogenic types related to migmatization, (2) metallogenic types related to remelted granite, (3) metallogenic types associated with the same melt granites, ( 4) metallogenic types related to ultrabasic and basic rocks, (5) metallogenic types related to volcanism and (6) metallogenic types related to strata control. Except that the second type is mainly distributed in the western part of the province, the others are mainly distributed in the east. Magmatic activity is dominated by NE, NW, ENE, E-W and N-S faults, whereas the former two dominated. Volcanic eruption centers often occur at the junction of NE-trending faults and NW or ENE-trending faults. The Yanshan cycle is related to its tectonic magmatism. In the end of this thesis, the metallogenic model and metallogenic prognosis of this metallogenic series are proposed.