The timing of India-Asia collision onset–Facts, theories, controversies
The timing of initial collision between India and Asia has remained controversial for half a
century. This paper attempts to review this crucial and hotly debated argument, describing …
century. This paper attempts to review this crucial and hotly debated argument, describing …
Outward-growth of the Tibetan Plateau during the Cenozoic: A review
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 …
evaluating models of collisional tectonics and holds important implications for processes …
[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 …
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 …
青藏高原与大陆动力学——地体拼合, 碰撞造山及高原隆升的深部驱动力
许志琴， 杨经绥， 李海兵， 张建新， 曾令， 森姜枚 - 中国地质, 2006 - geochina.cgs.gov.cn
提要: 运用地体和地体活动论观点, 提出青藏高原结构划分的新方案; 强调青藏高原的形成经历了
新元古代以来长期活动的过程, 青藏高原是一个“非原地” 诸多地体会聚, 拼合以及经历复合碰撞 …
新元古代以来长期活动的过程, 青藏高原是一个“非原地” 诸多地体会聚, 拼合以及经历复合碰撞 …
[PDF][PDF] 中新世以来我国季风-干旱环境演化与青藏高原的生长
安芷生， 张培震， 王二七， 王苏民， 强小科， 李力… - 第四纪研究, 2006 - dsjyj.com.cn
中新世以来我国季风-干旱环境演化与青藏高原的生长3 Page 1 第26卷第5期 2006年9月 第四纪
研究 QUATERNARY SC IENCES Vol. 26, No. 5 September, 2006 文章编号1001 - 7410 (2006) …
研究 QUATERNARY SC IENCES Vol. 26, No. 5 September, 2006 文章编号1001 - 7410 (2006) …
Magmatic record of India-Asia collision
New geochronological and geochemical data on magmatic activity from the India-Asia
collision zone enables recognition of a distinct magmatic flare-up event that we ascribe to …
collision zone enables recognition of a distinct magmatic flare-up event that we ascribe to …
Paleocene‐Eocene foreland basin evolution in the Himalaya of southern Tibet and Nepal: Implications for the age of initial India‐Asia collision
Siliciclastic sedimentary rocks derived from the southern Lhasa terrane, sitting depositionally
upon rocks of the northern Indian passive continental margin, provide an estimate of the age …
upon rocks of the northern Indian passive continental margin, provide an estimate of the age …
Gangdese magmatism in southern Tibet and India–Asia convergence since 120 Ma
A compilation of 290 zircon U–Pb ages of intrusive rocks indicates that the Gangdese
Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma. Two intense magmatic …
Batholith in southern Tibet was emplaced from c. 210 Ma to c. 10 Ma. Two intense magmatic …
Geologic evolution of the Himalayan-Tibetan orogen
A Yin, TM Harrison - Annual review of earth and planetary …, 2000 - annualreviews.org
A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …
Oblique stepwise rise and growth of the Tibet Plateau
P Tapponnier, X Zhiqin, F Roger, B Meyer, N Arnaud… - science, 2001 - science.org
Two end member models of how the high elevations in Tibet formed are (i) continuous
thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) …
thickening and widespread viscous flow of the crust and mantle of the entire plateau and (ii) …