Outward-growth of the Tibetan Plateau during the Cenozoic: A review

C Wang, J Dai, X Zhao, Y Li, SA Graham, D He, B Ran… - Tectonophysics, 2014 - Elsevier
The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

Tectonic evolution of the Sevier and Laramide belts within the North American Cordillera orogenic system

WA Yonkee, AB Weil - Earth-Science Reviews, 2015 - Elsevier
The thin-skin Sevier and thick-skin Laramide belts of the North American Cordillera provide
a long-term record of the interrelations between evolving styles of mountain building and …

[PDF][PDF] 喜马拉雅-青藏高原造山带地质演化

尹安 - ACTA GEOSCIENTIA SINICA, 2001 - faculty.epss.ucla.edu
摘要喜马拉雅2 青藏高原造山带的地质历史显示出, 自从约70Ma 印度板块2
亚洲板块开始碰撞以来, 至少有1 360 km 的SN 向缩短量被喜马拉雅2 青藏高原造山带所吸收 …

[PDF][PDF] 青藏高原碰撞造山带: Ⅲ. 后碰撞伸展成矿作用

侯增谦, 曲晓明, 杨竹森, 孟祥金, 李振清, 杨志明… - 矿床地质, 2006 - researchgate.net
摘要“后碰撞” 作为大陆碰撞造山作用的特定过程, 以其重要的构造演化标示性特征和强烈的爆发
式金属成矿作用, 受到人们的高度重视. 但涉及后碰撞的一系列重要地质问题 …

The rise and demise of the Paleogene Central Tibetan Valley

Z Xiong, X Liu, L Ding, A Farnsworth, RA Spicer… - Science …, 2022 - science.org
Reconstructing the Paleogene topography and climate of central Tibet informs
understanding of collisional tectonic mechanisms and their links to climate and biodiversity …

[PDF][PDF] Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses

P Kapp, PG DeCelles - American Journal of Science, 2019 - ajsonline.org
The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

[PDF][PDF] 冈底斯斑岩铜矿(化) 带: 西藏第二条“玉龙” 铜矿带? Ξ

曲晓明, 侯增谦, 黄卫 - 矿床地质, 2001 - cgl.org.cn
摘要通过广泛的野外地质调查和岩石地球化学, 矿床学, Re-Os 同位素, 硫, 铅同位素的综合研究,
首次比较系统地论述了雅鲁藏布江北侧冈底斯斑岩型铜矿带含矿斑岩的岩石地球化学特征和 …

[PDF][PDF] 大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约

葛文春, 吴福元, 周长勇, AAA Rahman - 科学通报, 2005 - researchgate.net
摘要大兴安岭北部的额尔古纳地块上分布有大面积时代和成因不明的花岗岩体,
其中位于塔河县城附近的塔河岩体主要由斑状正长花岗岩和二长花岗岩组成 …

Crustal deformation in the India‐Eurasia collision zone from 25 years of GPS measurements

G Zheng, H Wang, TJ Wright, Y Lou… - Journal of …, 2017 - Wiley Online Library
Abstract The India‐Eurasia collision zone is the largest deforming region on the planet;
direct measurements of present‐day deformation from Global Positioning System (GPS) …

[引用][C] 青藏高原碰撞造山带: Ⅱ. 晚碰撞转换成矿作用

侯增谦, 潘桂棠, 王安建, 莫宣学, 田世洪, 孙晓明… - 矿床地质, 2006