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首编大别造山带侵入岩地质图(1∶50万)及其说明

陈玲 马昌前 张金阳 刘园园 佘振兵 张超

地质通报2012,Vol.31Issue(1):13-19,7.
地质通报2012,Vol.31Issue(1):13-19,7.

首编大别造山带侵入岩地质图(1∶50万)及其说明

The first geological map of intrusive rocks in Dabie orogenic belt and its adjacent areas and its explanatory notes.

陈玲 1马昌前 2张金阳 1刘园园 3佘振兵 4张超1

作者信息

  • 1. 中国地质大学(武汉)地球科学学院,湖北武汉430074
  • 2. 中国地质调查局中国国土资源航空物探遥感中心,北京100083
  • 3. 中国地质大学/地质过程与矿产资源国家重点实验室,湖北武汉430074
  • 4. 中国地质大学(武汉)资源学院,湖北武汉430074
  • 折叠

摘要

Abstract

The exposed intrusive rocks of different ages in the Dabie orogenic belt which possess about 50% of the total surface area of that belt have great significance for understanding the evolution of the Dabie orogenic belt. In order to exchange the basic information obtained from the authors recent researches funded by the National Natural Science Foundation of China with other researchers, this paper presents the first geological map of intrusive rocks in Dabie orogenic belt and its adjacent areas (1:500000). This map is based on previous relevant maps and incorporates the latest data (including geochemical data and geochronological data) in the past two decades and the unpublished data obtained by the authors research group. It displays the spatial distribution, intrusive ages, petrologjc features and geochemical features. Also, in order to improve the readability of the map, the authors give serial number to the intrusive bodies.The research shows that the Early Cretaceous intrusive bodies possess the majority of all the intrusive rocks, while Neoproterozioc and Early Paleozoic bodies are much less. Most of the Neoproterozioc intrusive bodies occur as stocks in southern Dabie, Hong'an area in western Dabie and northern Huaiyang area. The Early Paleozoic intrusive bodies are much smaller, constituting paired magmatic belts in south and north parts of Dabie orogenic belt. The Late Jurrassic intrusive bodies are mainly distributed in the lower and middle reaches of the Yangtze River. The Early Cretaceous intrusive bodies are widely spread, covering 47% of the total area of the orogenic belt. The Late Mesozoic magma is probably associated with the northwestward subduction of Paleo-Pacific plate underneath the South China block and subsequent extensional events.

关键词

大别造山带/侵入岩/地质图

Key words

Dabie orogenic belt/ intrusive body/ geological map

分类

天文与地球科学

引用本文复制引用

陈玲,马昌前,张金阳,刘园园,佘振兵,张超..首编大别造山带侵入岩地质图(1∶50万)及其说明[J].地质通报,2012,31(1):13-19,7.

基金项目

国家自然科学基金重点项目《大别造山带中生代侵入岩类成因、岩浆动力学与构造体制转换》(批准号:40334037)和湖北省自然科学基金重点项目《鄂北大别山地区中生代典型花岗岩体铀的含矿性研究》(编号:2009CDA004) (批准号:40334037)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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