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DOI10.1016/j.lithos.2024.107550
Early Paleozoic metamorphism and anatexis of lower retro-/back-arc crust in the western Central Qilian belt, NE Tibet
发表日期2024
ISSN0024-4937
EISSN1872-6143
起始页码472
卷号472
英文摘要The tectonic-thermal mechanism of crustal melting provides vital information on continental differentiation and orogenic evolution. This study aims to understand the evolution and tectonic setting of newly discovered lower crustal leucosome-rich granulites of the Qilian Orogen, NW China. Tonalitic leucosome within garnet amphibolite occurs in net-like arrays or as stringers and has diffuse boundaries with the host, with enriched LILE, and high Sr and Sr/Y ratios, similar to that of adakite, formed by water-fluxed melting. However, granitic leucosome within garnet granitic gneiss shows sharp contacts with the host, and has low Sr, Ba, K and Pb but high Rb, Rb/Sr, with negative Eu anomalies, consistent with dehydration melting. Petrographic observations, geochemical data and pseudosection modelling suggest that garnet amphibolite experienced water-fluxed melting and garnet granitic gneiss underwent dehydration melting, respectively. LA-ICP-MS zircon and titanite dating indicate the anatectic event proceeded at -480-470 Ma. Phase equilibrium modelling suggests the garnet amphibolite and garnet granitic gneiss share a similar P-T path involving decompression heating from -12.1 kbar/711-746 degrees C to reach peak temperatures of 798-836 degrees C at 10.4 kbar, and subsequently decompression cooling to 4.6-7.6 kbar/ 600-672 degrees C. The calculated P-T conditions suggest Barrovian-type metamorphism with thermal gradients of 24.2 degrees C/km for the Central Qilian lower crust. We interpret a retro-/back-arc setting resulting from the southward subduction of the North Qilian oceanic lithosphere.
英文关键词Central Qilian belt; Water -fluxed melting; Phase equilibrium modelling; Geochronology; Lower crust
语种英语
WOS研究方向Geochemistry & Geophysics ; Mineralogy
WOS类目Geochemistry & Geophysics ; Mineralogy
WOS记录号WOS:001195839000001
来源期刊LITHOS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/299066
作者单位Northwest University Xi'an; Macquarie University; Yanan University; China Geological Survey; Xi'an Center, China Geological Survey
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GB/T 7714
. Early Paleozoic metamorphism and anatexis of lower retro-/back-arc crust in the western Central Qilian belt, NE Tibet[J],2024,472.
APA (2024).Early Paleozoic metamorphism and anatexis of lower retro-/back-arc crust in the western Central Qilian belt, NE Tibet.LITHOS,472.
MLA "Early Paleozoic metamorphism and anatexis of lower retro-/back-arc crust in the western Central Qilian belt, NE Tibet".LITHOS 472(2024).
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