Journal ArticleDOI
Early Paleozoic metamorphic rocks of the Erguna block in the Great Xing'an Range, NE China: Evidence for the timing of magmatic and metamorphic events and their tectonic implications
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TLDR
In this article, the Mohe Complex of the Erguna block was analyzed for metamorphism in the form of discrete zircon grains or metamorphic rims around detrital cores and they record remarkably consistent 206 Pb/ 238 U ages between 495-±2-Ma and 497-±6-Ma.About:
This article is published in Tectonophysics.The article was published on 2011-03-02. It has received 185 citations till now. The article focuses on the topics: Gneiss & Zircon.read more
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A Tale of Amalgamation of Three Permo-Triassic Collage Systems in Central Asia: Oroclines, Sutures, and Terminal Accretion
Wenjiao Xiao,Brian F. Windley,Shu Sun,Jiliang Li,Baochun Huang,Chunming Han,Chao Yuan,Min Sun,Hanlin Chen +8 more
TL;DR: The Central Asian Orogenic Belt as discussed by the authors records the accretion and convergence of three collage systems that were finally rotated into two major oroclines, the Mongolia collage system was a long, N-S-oriented composite ribbon that was rotated to its current orientation when the Mongol-Okhotsk orogine was formed.
Journal ArticleDOI
Introduction to tectonics of China
TL;DR: In the last three decades, extensive geological, geochemical and geophysical investigations have been carried out on these cratonic blocks and intervening orogenic belts, producing an abundant amount of new data and competing interpretations.
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A review of the Paleozoic tectonics in the eastern part of Central Asian Orogenic Belt
Yongjiang Liu,Yongjiang Liu,Yongjiang Liu,Weimin Li,Weimin Li,Zhiqiang Feng,Zhiqiang Feng,Quanbo Wen,Quanbo Wen,Franz Neubauer,Chenyue Liang,Chenyue Liang +11 more
TL;DR: The Central Asian Orogenic belt (CAOB) is the largest accretionary orogen in the world, which is responsible for considerable Phanerozoic juvenile crustal growth as discussed by the authors.
Journal ArticleDOI
The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt
TL;DR: The NE China Khondalite Belt as mentioned in this paper is a terrane formed by a collision between currently unidentified terranes with the Southeastern Angara-Anabar Province at about 500-Ma, where the rocks were deformed and metamorphosed to granulite facies.
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Final amalgamation of the Central Asian Orogenic Belt in NE China: Paleo-Asian Ocean closure versus Paleo-Pacific plate subduction — A review of the evidence
TL;DR: The Central Asian Orogenic Belt (CAOB) evolved through complex closure of the Paleo-Asian Ocean from the Neoproterozoic to the late Phanerozoic.
References
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Journal ArticleDOI
Three natural zircon standards for u‐th‐pb, lu‐hf, trace element and ree analyses
M. Wiedenbeck,P. Allé,Fernando Corfu,William L. Griffin,M. Meier,F. Oberli,A. von Quadt,J.C. Roddick,W. Spiegel +8 more
TL;DR: In this paper, the results of a study to develop natural zircon geochemical standards for calibrating the U-(Th)-Pb geochronometer and Hf isotopic analyses are reported.
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Correction of common lead in U-Pb analyses that do not report 204Pb
TL;DR: In this article, the authors proposed a correction method that neither uses 204Pb nor assumes concordance, but uses a numeric solution to a set of equations relating the content of radiogenic lead in a zircon or other U/Th-enriched mineral to its total lead content.
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Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia
TL;DR: A new tectonic model, postulating the growth of giant subduction-accretion complexes along a single magmatic arc now found contorted between Siberia and Baltica, shows that Asia grew by 5.3 million square kilometres during the Palaeozoic era as mentioned in this paper.
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In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard
TL;DR: In this paper, an internal standard-independent calibration strategy for LA-ICP-MS analysis of anhydrous minerals and glasses was described, where the ablation yield correction factor (AYCF) was used to correct the matrix-dependent absolute amount of materials ablated during each run.