Results 51 to 60 of about 1,111,472 (195)
The Lesser Xing’an-Zhangguangcai Range tectonic belt in northeastern China is located along the eastern margin of the Central Asian Orogenic Belt and serves as the key to understanding the tectonic transition between the Paleo-Asian Ocean and Paleo ...
Liye Liu +13 more
doaj +1 more source
Reconstructing the evolutionary history of the Paleo-Tethys Ocean remains at the center of debates over the linkage between Gondwana dispersion and Asian accretion.
Xia, Xiao-Ping +9 more
core +1 more source
The closing time of the Paleo-Asian Ocean and the tectonic evolution of the northern margin of the North China Craton are still controversial. The geochronology and geochemistry of the Zhaojinggou monzogranite pluton provide new constraints on the late ...
Jia-Ying Wang +8 more
core +1 more source
The Paleo–Asian Ocean, originated from the breakup of the Rodinia supercontinent, had undergone a long and complex process of expansion and closure. The oceanic lithosphere of the Paleo–Asian Ocean subducted beneath the surrounding continents, including ...
王博, Wang, Bo
core
Much controversy exists regarding the timing of the final closure of the Paleo-Asian Ocean and the resultant formation of the Central Asian orogenic belt.
Zhao, G +15 more
core +1 more source
Supporting Information for [Closure of the eastern Paleo-Asian Ocean: Insights from an upper Permian sedimentary record of subduction to collision in northeast China]THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE.
Zhang, H (via Mendeley Data)
core +1 more source
Multi-proxy reconstruction of surface water pCO2 in the northern Arabian Sea since 29ka [PDF]
We report here the results of a multi-proxy study to reconstruct surface water pCO2 concentrations in the northern Arabian Sea. Our results show that [delta]11B and Mg/Ca measurements of the planktonic foraminifer Globigerinoides sacculifer yield ...
Yu, Jimin +15 more
core +1 more source
Zircon U–Pb geochronology and geochemistry of granitic rocks in central Mongolia
The Central Asian Orogenic Belt had been formed by amalgamation of voluminous subduction–accretionary complexes during the Late Neoproterozoic to the Mesozoic period. Mongolia is situated in the center of this belt.
Boldbaatar Dolzodmaa +3 more
doaj +1 more source
The response of the large‐scale ocean circulation to 20th century Asian and non‐Asian aerosols
Multidecadal trends in the large-scale ocean circulation are influenced by changes in radiative forcings such as long-lived greenhouse gases, volcanic aerosols, and solar irradiance.
T. Cowan, Cai, W., W. Cai, Cowan, T.
core +1 more source
Mesozoic magmatism and crustal evolution in the Xing’an–Mongolia Orogenic Belt, NE China
The Xing’an–Mongolia Orogenic Belt (XMOB), located in the eastern Central Asian Orogenic Belt (CAOB), is a critical area for understanding Phanerozoic crustal accretion and reworking.
Wen-Ting Zhang, Ying Wei, Ming-Xing Ling
doaj +1 more source

