Timing and mechanisms of Tibetan Plateau uplift

L Ding, P Kapp, F Cai, CN Garzione, Z **ong… - Nature Reviews earth & …, 2022 - nature.com
The timing of the initial India–Asia collision and the mechanisms that led to the eventual
formation of the high (> 5 km) Tibetan Plateau remain enigmatic. In this Review, we describe …

Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at~ 7 Ma

J Sun, Z Ding, W **ao, BF Windley - Earth-Science Reviews, 2022 - Elsevier
The Asian interior contains the Central Asian Orogenic Belt (CAOB, the longest accretionary
orogen on Earth), the largest mid-latitude desert, and the most widespread late Cenozoic …

[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 …

Ancient orogenic and monsoon-driven assembly of the world's richest temperate alpine flora

WN Ding, RH Ree, RA Spicer, YW **ng - Science, 2020 - science.org
Origins of an alpine flora The evolution of high mountain floras is strongly influenced by
tectonic and climatic history. Ding et al. document the timing, tempo, and mode by which the …

No high Tibetan plateau until the Neogene

T Su, A Farnsworth, RA Spicer, J Huang, FX Wu… - Science …, 2019 - science.org
The Late Paleogene surface height and paleoenvironment for the core area of the Qinghai-
Tibetan Plateau (QTP) remain critically unresolved. Here, we report the discovery of the …

[HTML][HTML] The influence of soil chemistry on branched tetraether lipids in mid-and high latitude soils: Implications for brGDGT-based paleothermometry

C De Jonge, EE Kuramae, D Radujković… - … et Cosmochimica Acta, 2021 - Elsevier
Branched glycerol dialkyl glycerol tetraethers (BrGDGTs) are a suite of orphan bacterial
membrane lipids commonly used as paleo-environmental proxies for mean annual air …

Orographic rainfall drives the Himalaya drainage divide to move north

S Bian, X Tan, Y Liu, S Fan, J Gong, C Zhou, F Shi… - Geomorphology, 2024 - Elsevier
Abstract The Yarlung River flows between the east-trending Himalayan and Gangdese
orogens, and across several north-trending rifts. It carries rich information on the Indian …

A history of the Asian monsoon and its interactions with solid Earth tectonics in Cenozoic South Asia

PD Clift, AAG Webb - Geological Society, London, Special …, 2019 - lyellcollection.org
Although there is some evidence for an Eocene monsoon, the most important intensification
of rainfall appears to start at c. 24 Ma in the Early Miocene. Many palaeoceanographical …

A late miocene terrestrial temperature history for the northeastern Tibetan plateau's period of tectonic expansion

C Chen, Y Bai, X Fang, H Guo, Q Meng… - Geophysical …, 2019 - Wiley Online Library
Abstract During the Late Miocene, the climate patterns and ecosystems of continental land
masses experienced crucial transitions, but whether the principal driver was regional …

Biotic interchange through lowlands of Tibetan Plateau suture zones during Paleogene

J Liu, T Su, RA Spicer, HE Tang, FX Wu… - Palaeogeography …, 2019 - Elsevier
A substantial biotic interchange took place between Gondwanan India and Laurasia
immediately following the India-Eurasia collision. Located just north of the collision zone, the …