Central China orogenic belt and amalgamation of East Asian continents
Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …
Tectonic architecture and multiple orogeny of the Qinling Orogenic Belt, Central China
Abstract The Qinling Orogenic Belt (QOB) is located between the North China and South
China Blocks, and has been considered to have formed by the collision between these …
China Blocks, and has been considered to have formed by the collision between these …
秦岭印支期构造背景, 岩浆活动及成矿作用
陈衍景 - 中国地质, 2010 - geochina.cgs.gov.cn
提要: 秦岭造山带以其独特的大地构造位置, 复杂的地质演化和丰富的矿产资源而成为地质科学
研究的焦点, 科学家已经基本清楚了其大地构造格局和地质演化轮廓, 共识其在印支期(三叠纪 …
研究的焦点, 科学家已经基本清楚了其大地构造格局和地质演化轮廓, 共识其在印支期(三叠纪 …
秦岭造山带早中生代花岗岩成因及其构造环境
张成立， 王涛， 王晓霞 - 高校地质学报, 2008 - geology.nju.edu.cn
秦岭早中生代花岗岩以准铝到过铝质中钾—高钾钙碱性岩石为主. 它们具有相对富集LILE,
LREE, 贫化HFSE 和Nb, Ta 不同程度亏损的后碰撞花岗岩的地球化学特征 …
LREE, 贫化HFSE 和Nb, Ta 不同程度亏损的后碰撞花岗岩的地球化学特征 …
南岭与中生代花岗岩类有关的成矿作用及其大地构造背景
华仁民， 陈培荣， 张文兰， 姚军明， 林锦富， 张展适… - 高校地质 …, 2005 - geology.nju.edu.cn
由于受到来自印支半岛的挤压, 在华南内部发生了以碰撞-挤压-推覆-隆升为主的印支造山运动.
南岭地区印支期花岗岩(240~ 205Ma) 主要形成于碰撞及“后碰撞”(post-collision) 的动力学环境 …
南岭地区印支期花岗岩(240~ 205Ma) 主要形成于碰撞及“后碰撞”(post-collision) 的动力学环境 …
Tectonic evolution of the Qinling orogen, China: review and synthesis
Y Dong, G Zhang, F Neubauer, X Liu, J Genser… - Journal of Asian Earth …, 2011 - Elsevier
This contribution reviews the tectonic structure and evolution of the Qinling orogenic belt,
which extends east–west nearly 2500 km across Central China and is a giant orogenic belt …
which extends east–west nearly 2500 km across Central China and is a giant orogenic belt …