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福建中生代火山活动的基本特征 及构造环境

卢清地

岩石矿物学杂志2001,Vol.20Issue(1):57-68,12.
岩石矿物学杂志2001,Vol.20Issue(1):57-68,12.

福建中生代火山活动的基本特征 及构造环境

Basic Characteristics and Tectonic Setting of Mesozoic Volcanic Rocks in Fujian Province

卢清地1

作者信息

  • 1. 福建地勘局区域地质调查队,
  • 折叠

摘要

Abstract

Mesozoic volcanic activities experienced three stages, namely theLate Triassic_Late Jurassic initial stage, the Late Jurassic flourishing stage and the Cretaceous weakening_withering stage. The three stages, controlled by the same tectonic mechanism, show remarkable differences and also transitional characteristics in such aspects as volcanic activities, rock assemblages, petrochemistry and geochemistry. Studies show that the formation of Mesozoic volcanic rocks was intimately related to the subduction of the Pacific plate towards the Eurasian plate, and these volcanic rocks can be called Zhejiang_Fujian type volcanic rocks.

关键词

中生代火山岩/岩石化学/地球化学/构造环境/福建

分类

天文与地球科学

引用本文复制引用

卢清地..福建中生代火山活动的基本特征 及构造环境[J].岩石矿物学杂志,2001,20(1):57-68,12.

基金项目

本文系福建省地质矿产勘查开发局“八五”基础地质重点科研项目“1:50万福建省地质图及说明书修编”项目的部分成果。 ()

岩石矿物学杂志

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