Final amalgamation of the Tianshan and Junggar orogenic collage in the southwestern Central Asian Orogenic Belt: Constraints on the closure of the Paleo-Asian …
Y Han, G Zhao - Earth-Science Reviews, 2018 - Elsevier
Abstract The Tianshan and Junggar orogenic collage occupies the southwestern part of the
Central Asian Orogenic Belt and was assembled by collision/accretion of several continental …
Central Asian Orogenic Belt and was assembled by collision/accretion of several continental …
Tectonic evolution, superimposed orogeny, and composite metallogenic system in China
J Deng, Q Wang, G Li - Gondwana Research, 2017 - Elsevier
Continental China is a mosaic of numerous tectonic blocks, which amalgamated from
Neoarchean to Cenozoic broadly coeval with the cycles of global supercontinents such as …
Neoarchean to Cenozoic broadly coeval with the cycles of global supercontinents such as …
Late Carboniferous collision between the Tarim and Kazakhstan–Yili terranes in the western segment of the South Tian Shan Orogen, Central Asia, and implications …
BF Han, GQ He, XC Wang, ZJ Guo - Earth-Science Reviews, 2011 - Elsevier
The Tian Shan of Central Asia is located in the southwestern part of the Central Asian
Orogenic Belt (CAOB, also known as the Central Asian Orogenic System or CAOS) …
Orogenic Belt (CAOB, also known as the Central Asian Orogenic System or CAOS) …
Accretionary processes and metallogenesis of the Central Asian Orogenic Belt: Advances and perspectives
As one of the largest Phanerozoic orogens in the world, the Central Asian Orogenic Belt
(CAOB) is a natural laboratory for studies of continental dynamics and metallogenesis. This …
(CAOB) is a natural laboratory for studies of continental dynamics and metallogenesis. This …
Neoproterozoic to Paleozoic long‐lived accretionary orogeny in the northern Tarim Craton
Abstract The Tarim Craton, located in the center of Asia, was involved in the assembly and
breakup of the Rodinia supercontinent during the Neoproterozoic and the subduction …
breakup of the Rodinia supercontinent during the Neoproterozoic and the subduction …
[HTML][HTML] Natural observations of subduction initiation: Implications for the geodynamic evolution of the Paleo-Asian Ocean
G Yang, Y Li, L Tong, Z Wang, G Si, P Lindagato… - Geosystems and …, 2022 - Elsevier
Initiation of new subduction zones is an integral part of Earth's plate tectonics regime. It is
generally accepted that the negative buoyancy of sufficiently old oceanic lithosphere …
generally accepted that the negative buoyancy of sufficiently old oceanic lithosphere …
The Paleozoic northern margin of the Tarim Craton: passive or active?
Whether the northern Tarim Craton was an active or passive continental margin during the
Paleozoic is vital to our understanding of the subduction polarity of paleo-oceanic plates in …
Paleozoic is vital to our understanding of the subduction polarity of paleo-oceanic plates in …
Structure, age, and tectonic development of the Huoshishan–Niujuanzi ophiolitic mélange, Beishan, southernmost Altaids
Abstract The Huoshishan–Niujuanzi ophiolitic mélange (HNO) is located near the central
part of the Beishan Orogenic Belt in the southernmost Altaids. The HNO consists of …
part of the Beishan Orogenic Belt in the southernmost Altaids. The HNO consists of …
Cambrian to early Silurian ophiolite and accretionary processes in the Beishan collage, NW China: implications for the architecture of the Southern Altaids
The mechanism of continental growth of the Altaids is currently under debate between
models invoking continuous subduction-accretion or punctuated accretion by closure of …
models invoking continuous subduction-accretion or punctuated accretion by closure of …