Timing and mechanisms of Tibetan Plateau uplift
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 …
formation of the high (> 5 km) Tibetan Plateau remain enigmatic. In this Review, we describe …
Reorganization of Asian climate in relation to Tibetan Plateau uplift
Reorganization of the Asian climate from one dominated by global planetary wind systems
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …
青藏高原隆起与环境变化研究
李吉均， 方小敏 - 1998 - ir.lzu.edu.cn
摘要简要的回顾和总结了国内外近年来, 尤其国家“八五” 和“九五” 攀登计划青藏项目执行以来,
围绕青藏高原隆升过程和环境变化所取得的主要进展, 存在问题和挑战. 它表明青藏高原的隆起 …
围绕青藏高原隆升过程和环境变化所取得的主要进展, 存在问题和挑战. 它表明青藏高原的隆起 …
Global warming in the pipeline
Improved knowledge of glacial-to-interglacial global temperature change yields Charney
(fast-feedback) equilibrium climate sensitivity 1.2±0.3° C (2σ) per W/m2, which is 4.8° C±1.2° …
(fast-feedback) equilibrium climate sensitivity 1.2±0.3° C (2σ) per W/m2, which is 4.8° C±1.2° …
Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
An atlas of Phanerozoic paleogeographic maps: the seas come in and the seas go out
CR Scotese - Annual Review of Earth and Planetary Sciences, 2021 - annualreviews.org
Paleogeography is the study of the changing surface of Earth through time. Driven by plate
tectonics, the configuration of the continents and ocean basins has been in constant flux …
tectonics, the configuration of the continents and ocean basins has been in constant flux …
Atmospheric CO2 over the Past 66 Million Years from Marine Archives
Throughout Earth's history, CO2 is thought to have exerted a fundamental control on
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …
environmental change. Here we review and revise CO2 reconstructions from boron isotopes …
[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) …
[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 …
geological framework and initial growth were fundamentally the result of multiple, previous …
A global temperature control of silicate weathering intensity
Silicate weathering as an important negative feedback can regulate the Earth's climate over
time, but much debate concerns its response strength to each climatic factor and its …
time, but much debate concerns its response strength to each climatic factor and its …