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Late Carboniferous collision between the Tarim and Kazakhstan–Yili terranes in the western segment of the South Tian Shan Orogen, Central Asia, and implications …
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) …
[HTML][HTML] Genetic relationship between skarn and porphyry mineralization at the Saibo copper deposit, West Tianshan, NW China: Constraints from fluid inclusions, H …
The Saibo skarn–porphyry deposit, located in West Tianshan, NW China, is a large copper
deposit discovered recently; however, information regarding the differences and …
deposit discovered recently; however, information regarding the differences and …
Age, geochemistry, and tectonic implications of a late Paleozoic stitching pluton in the North Tian Shan suture zone, western China
Abstract The Central Asian orogenic belt is the largest tectonic assembly of continental and
oceanic terranes on Earth due to closure of the paleo–Asian Ocean in the Phanerozoic …
oceanic terranes on Earth due to closure of the paleo–Asian Ocean in the Phanerozoic …
Geochemical and geochronological studies of granitoid rocks from the Western Tianshan Orogen: implications for continental growth in the southwestern Central …
The Western Tianshan Orogen in northwestern China is part of the southwestern margin of
the Central Asian Orogenic Belt (CAOB), which represents the largest tectonic assembly of …
the Central Asian Orogenic Belt (CAOB), which represents the largest tectonic assembly of …
Early Neoproterozoic crustal evolution in northern Yili Block: Insights from migmatite, orthogneiss and leucogranite of the Wenquan metamorphic complex in the NW …
The northern part of the Yili Block, located in the northwest of the Chinese Tianshan, extends
westward to joint with the Aktau-Junggar domain in Kazakhstan, and is one of the major …
westward to joint with the Aktau-Junggar domain in Kazakhstan, and is one of the major …
Geochronology and geochemistry of Late Paleozoic magmatic rocks in the Lamasu–Dabate area, northwestern Tianshan (west China): evidence for a tectonic …
Voluminous Late Paleozoic igneous rocks and associated Cu–Au–Mo deposits occur in the
northwestern Tianshan district, **njiang, west China. However, the tectonic setting and …
northwestern Tianshan district, **njiang, west China. However, the tectonic setting and …
Detrital zircon ages of Proterozoic meta-sedimentary rocks and Paleozoic sedimentary cover of the northern Yili Block: Implications for the tectonics of microcontinents …
Abstract The Central Asian Orogenic Belt (CAOB) is one of the largest accretionary orogens
in the world. It was formed mainly by amalgamation of island arcs, accretionary wedges and …
in the world. It was formed mainly by amalgamation of island arcs, accretionary wedges and …
Detrital zircons from Neoproterozoic sedimentary rocks in the Yili Block: Constraints on the affinity of microcontinents in the southern Central Asian Orogenic Belt
Abstract The Yili Block is one of the Precambrian microcontinents dispersed in the Central
Asian Orogenic Belt (CAOB). Detrital zircon U–Pb ages and Hf isotopic data of …
Asian Orogenic Belt (CAOB). Detrital zircon U–Pb ages and Hf isotopic data of …
An Early Devonian to Early Carboniferous volcanic arc in North Tianshan, NW China: Geochronological and geochemical evidence from volcanic rocks
F An, Y Zhu, S Wei, S Lai - Journal of Asian Earth Sciences, 2013 - Elsevier
Abstract The Late Paleozoic volcanic and sedimentary rocks are widespread in the North
Tianshan along the north margin of the Yili block. They consist of basalt, basaltic andesite …
Tianshan along the north margin of the Yili block. They consist of basalt, basaltic andesite …
Middle-Late Ordovician arc-type plutonism in the NW Chinese Tianshan: Implication for the accretion of the Kazakhstan continent in Central Asia
Kazakhstan is one of the largest continental assemblages within the Central Asian Orogenic
Belt. It was formed by accretion and amalgamation of several continental fragments and …
Belt. It was formed by accretion and amalgamation of several continental fragments and …