安徽地质2016，Vol.26Issue(2)：87-91,5.
大兴安岭中生代岩浆岩及岩浆作用研究进展
PROGRESS IN STUDY ON THE MESOZOIC MAGMATIC ROCKS AND MAGMATISM IN DAXING’ANLING
杨斌 1邓丽军 2仲雪辰3
作者信息
- 1. 东华理工大学地球科学学院，江西南昌 330013
- 2. 江西省地质矿产勘查开发局九一六地质大队，江西九江 332100
- 3. 江西省地质矿产勘查开发局赣中地质大队，江西南昌 330002
- 折叠
摘要
Abstract
The Daxing’anling area lies in northeast of China as a part of the eastern extension of the Xingmeng orogenic belt. In geological history, multi-stage magmatic activities took place in the area, of which the Mesozoic magmatism was the strongest, most widespread and closest to ore formation. On the basis of summarizing previous data, considering structural geology setting and zircon isotopic dating, this paper discussed magmatic rocks and magmatism of the Mesozoic era in the area, and this study is helpful to restoring the geological evolution history and mastering the development law providing reference for scientific research and mineral exploration in the area.关键词
大兴安岭/中生代/岩浆岩及岩浆作用Key words
Mesozoic/magmatic rocks and magmatism/Daxing’anling分类
天文与地球科学引用本文复制引用
杨斌,邓丽军,仲雪辰..大兴安岭中生代岩浆岩及岩浆作用研究进展[J].安徽地质,2016,26(2):87-91,5.
