Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt

The aim of this reprint is to immerse interested readers in the evolutionary history and mineralization of the Central Asian Orogenic Belt (CAOB). The Central Asian Orogenic Belt (CAOB) is the result of long-lived multi-stage tectonic evolution, including Proterozoic to Paleozoic accretion and colli...

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description The aim of this reprint is to immerse interested readers in the evolutionary history and mineralization of the Central Asian Orogenic Belt (CAOB). The Central Asian Orogenic Belt (CAOB) is the result of long-lived multi-stage tectonic evolution, including Proterozoic to Paleozoic accretion and collision, Mesozoic intracontinental modification, and Cenozoic rapid deformation and uplift. The accretionary and collisional orogenesis of its early history generated a huge orogenic collage consisting of diverse tectonic units including island arcs, ophiolites, accretionary prisms, seamounts, oceanic plateaus, and micro-continents. These incorporated orogenic components preserved valuable detailed information on orogenic processes and continental crust growth, which make the CAOB a key region for the understanding of continental evolution, mantle–crust interaction, and associated mineralization. In this reprint, new data and study advances on tectonic evolution and the mineralization effect of the south domain of the CAOB, including the Kazakhstan–West Junggar orocline system, Altai–East Junggar orogenic belt, Tianshan orogenic belt, Beishan orogenic belt, Xing–Meng orogenic belt, and northern North China Craton, are introduced. Precise zircon U-Pb ages and isotopes from individual parts of the CAOB have been provided. We pave the way to deeply understand accretionary orogeny and mineralization processes in the accretionary orogenic belt.
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publisherStr MDPI - Multidisciplinary Digital Publishing Institute
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spelling doab-20.500.12854ir-1529692025-02-20T13:21:42Z Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt Chen, Jiafu Ju, Nan Zhao, Zhonghai accretionary orogen tectonic evolution geochemistry mineralization CAOB thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general thema EDItEUR::R Earth Sciences, Geography, Environment, Planning The aim of this reprint is to immerse interested readers in the evolutionary history and mineralization of the Central Asian Orogenic Belt (CAOB). The Central Asian Orogenic Belt (CAOB) is the result of long-lived multi-stage tectonic evolution, including Proterozoic to Paleozoic accretion and collision, Mesozoic intracontinental modification, and Cenozoic rapid deformation and uplift. The accretionary and collisional orogenesis of its early history generated a huge orogenic collage consisting of diverse tectonic units including island arcs, ophiolites, accretionary prisms, seamounts, oceanic plateaus, and micro-continents. These incorporated orogenic components preserved valuable detailed information on orogenic processes and continental crust growth, which make the CAOB a key region for the understanding of continental evolution, mantle–crust interaction, and associated mineralization. In this reprint, new data and study advances on tectonic evolution and the mineralization effect of the south domain of the CAOB, including the Kazakhstan–West Junggar orocline system, Altai–East Junggar orogenic belt, Tianshan orogenic belt, Beishan orogenic belt, Xing–Meng orogenic belt, and northern North China Craton, are introduced. Precise zircon U-Pb ages and isotopes from individual parts of the CAOB have been provided. We pave the way to deeply understand accretionary orogeny and mineralization processes in the accretionary orogenic belt. 2025-02-20T13:21:40Z 2025-02-20T13:21:40Z 2024 book ONIX_20250220_9783725825615_333 9783725825615 9783725825622 https://directory.doabooks.org/handle/20.500.12854/152969 eng application/octet-stream Attribution 4.0 International https://mdpi.com/books/pdfview/book/10153 MDPI - Multidisciplinary Digital Publishing Institute 10.3390/books978-3-7258-2562-2 10.3390/books978-3-7258-2562-2 46cabcaa-dd94-4bfe-87b4-55023c1b36d0 9783725825615 9783725825622 368 Basel open access
spellingShingle accretionary orogen
tectonic evolution
geochemistry
mineralization
CAOB
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title_full Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title_fullStr Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title_full_unstemmed Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title_short Tectonic–Magmatic Evolution and Mineralization Effect in the Southern Central Asian Orogenic Belt
title_sort tectonic ndash magmatic evolution and mineralization effect in the southern central asian orogenic belt
topic accretionary orogen
tectonic evolution
geochemistry
mineralization
CAOB
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
topic_facet accretionary orogen
tectonic evolution
geochemistry
mineralization
CAOB
thema EDItEUR::G Reference, Information and Interdisciplinary subjects::GP Research and information: general
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning
url ONIX_20250220_9783725825615_333