Journal ArticleDOI
Juvenile versus recycled crust in the Central Asian Orogenic Belt: Implications from ocean plate stratigraphy, blueschist belts and intra-oceanic arcs
Inna Safonova,Inna Safonova +1 more
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TLDR
The Central Asian Orogenic Belt (CAOB) represents the world's largest province of Phanerozoic juvenile crustal growth during ca. 800 m.y. as discussed by the authors.About:
This article is published in Gondwana Research.The article was published on 2017-07-01. It has received 133 citations till now. The article focuses on the topics: Accretionary wedge & Oceanic crust.read more
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Mesozoic tectono-magmatic response in the East Asian ocean-continent connection zone to subduction of the Paleo-Pacific Plate
Sanzhong Li,Yanhui Suo,Xiyao Li,Jie Zhou,M. Santosh,M. Santosh,Pengcheng Wang,Guangzeng Wang,Lingli Guo,Shengyao Yu,Haoyuan Lan,Liming Dai,Zaizhen Zhou,Xianzhi Cao,Junjiang Zhu,Bo Liu,Suhua Jiang,Gang Wang,Guowei Zhang,Guowei Zhang +19 more
TL;DR: In this article, the authors provide a comprehensive synthesis of the state-of-the-art information from deformation analysis, magmatism, geochronology, tomography and other fields from this region.
Journal ArticleDOI
No excessive crustal growth in the Central Asian Orogenic Belt: Further evidence from field relationships and isotopic data
Alfred Kröner,Victor Kovach,D. V. Alexeiev,Kuo-Lung Wang,Kuo-Lung Wang,Jean Wong,Kirill E. Degtyarev,I. K. Kozakov +7 more
TL;DR: In this article, the authors provide new field observations and isotopic data for key areas of the Central Asian Orogenic Belt (CAOB), reiterating their previous assessment that no excessive crustal growth occurred during its ca. 800 Ma long orogenic evolution.
Journal ArticleDOI
Multiple Tethyan ocean basins and orogenic belts in Asia
TL;DR: In this article, the evolution of the Tethyan ocean basins in Asia illustrates that Asia has been a giant convergent zone for more than 500 million years, and the Phanerozoic construction and evolution of Asia involved the opening and closure of Tithyan ocean basin and the collision and accretion of Gondwana-derived continental blocks and the Indian Craton Subduction processes, arc and back-arc basin generation, and continent-continent and arccontinent collisions led to the principal orogenic events.
Journal ArticleDOI
Intra-oceanic arcs of the Paleo-Asian Ocean
Inna Safonova,Inna Safonova,A.V. Kotlyarov,Sergey K. Krivonogov,Sergey K. Krivonogov,Wenjiao Xiao +5 more
TL;DR: In this article, structural position of intra-oceanic arc volcanic rocks in association with back-arc terranes and accretionary complexes, major periods of intra oceanic arc magmatism and related juvenile crustal growth, geochemical features and typical ranges of Nd isotope values of volcanic rocks are discussed.
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Phanerozoic granitoids in the central and eastern parts of Central Asia and their tectonic significance
Tao Wang,Ying Tong,Lei Zhang,Shan Li,He Huang,Jianjun Zhang,Lei Guo,Qidi Yang,Dawei Hong,Tatiana V. Donskaya,Dmitry P. Gladkochub,Narantsetseg Tserendash +11 more
TL;DR: In the Central Asian Orogenic Belt (CAOBB) as discussed by the authors, the granitoids occupy a total area more than 8 million km2, with three major area peaks at Cambro-Ordovician, Carboniferous-Permian, and Jurassic.
References
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Book
Orogenic Andesites and Plate Tectonics
TL;DR: In this article, the authors define Orogenic Andesite and discuss its properties and properties, including the following: 1.1 Topography, gravity, heat flow, and conductivity.
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Tectonic models for accretion of the Central Asian Orogenic Belt
TL;DR: The Central Asian Orogenic Belt ( c. 1000-250 Ma) formed by accretion of island arcs, ophiolites, oceanic islands, seamounts, accretionary wedges, and oceanic plateaux and microcontinents in a manner comparable with that of circum-Pacific Mesozoic-Cenozoic orogens is studied in this article.
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Mantle geochemistry: the message from oceanic volcanism
TL;DR: Basaltic volcanism'samples' the Earth's mantle to great depths, because solid-state convection transports deep material into the (shallow) melting region as mentioned in this paper.
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Orogenic gold deposits : A proposed classification in the context of their crustal distribution and relationship to other gold deposit types
TL;DR: The orogenic gold deposits were formed during compressional to transpressional deformation processes at convergent plate margins in accretionary and collisional orogens as discussed by the authors, with gold deposition from 15-20 km to the near surface environment.