曲宏健. Review of Magmatite and Magmatism during Early Yanshan Tectonic Sub Period in Wuyi-Yunkai Area[J]. 2017, (1): 68-73. DOI: 10.16056/j.1005-7676.2017.01.018.
武夷—云开地区早燕山构造亚阶段岩浆岩与岩浆作用
摘要
武夷—云开地区位于华夏地块中部
是中国华南重要的岩浆岩带
其中早燕山期岩浆岩分布范围广
经历了170、165
1
50、145
1
30 Ma 3个岩浆活动期
对早燕山期的成矿起到重要的影响作用。此地地质意义非凡
是众多地质学者不断探索的时空区域
岩浆岩源区深达地幔
引发地质学者对地幔柱的探究。近期对其侏罗纪岩浆岩改为白垩纪的地质改动
也使得"晚侏罗世东部高原"问题成为热点话题。富集Ag、Pb、Cu等元素
成矿受岩浆多期侵入影响
中深成、浅成侵入岩分别形成不同矿床。
Abstract
Wuyi-Yunkai area is located in the central part of cathaysia block
is an important magmatic belt in southern China
and the magmatic during early Yanshan period distributes widely
it have experienced 170
165-150
145-130 Ma three magmatic activity stage
and have an important impact on mineralization during the early Yanshanian. The geological significance is extraordinary here
and Wuyi-Yunkai area is the space-time region that many geological scholars continue to explore
magmatic source region is deep in the earth’s mantle
so it promotes many geological scholars do researches on mantle plume. Recently the Jurassic magmatite are changed to Cretaceous geological magmatite
that also makes "the late Jurassic eastern plateau" issue become a hot topic. This area enriches Ag
Pb
Cu and other elements
and metallogenic was affected by multiphase of magma
deep and hypabyssal intrusive rocks promoted to form different deposits.