2017
DOI: 10.1016/j.gr.2016.08.009
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Sediment recycling and crustal growth in the Central Asian Orogenic Belt: Evidence from Sr–Nd–Hf isotopes and trace elements in granitoids of the Chinese Altay

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Cited by 59 publications
(45 citation statements)
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“…According to the new age data from this study for the Tuerhong, Keshikusite, Aleretuobie, Tuoputieke, and Tasitake plutons in the southern Chinese Altai, the five granitic intrusions were emplaced from 497.8 ± 3.9 Ma to 397.7 ± 5.7 Ma. This conclusion is comparable with previous studies on ages of peraluminous and S-type granites based on zircon U-Pb dating (507-392 Ma; Tong et al, 2007;Cai et al, 2011aCai et al, , 2011bZhang et al, 2017). In addition, synchronous felsic volcanism is also apparent in the form of peraluminous rhyolites in the Chinese Altai, with ages ranging from 412 to 406 Ma.…”
Section: Peraluminous Granitic Magmatism In the Chinese Altaisupporting
confidence: 90%
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“…According to the new age data from this study for the Tuerhong, Keshikusite, Aleretuobie, Tuoputieke, and Tasitake plutons in the southern Chinese Altai, the five granitic intrusions were emplaced from 497.8 ± 3.9 Ma to 397.7 ± 5.7 Ma. This conclusion is comparable with previous studies on ages of peraluminous and S-type granites based on zircon U-Pb dating (507-392 Ma; Tong et al, 2007;Cai et al, 2011aCai et al, , 2011bZhang et al, 2017). In addition, synchronous felsic volcanism is also apparent in the form of peraluminous rhyolites in the Chinese Altai, with ages ranging from 412 to 406 Ma.…”
Section: Peraluminous Granitic Magmatism In the Chinese Altaisupporting
confidence: 90%
“…Zircon U-Pb dating in the igneous rocks suggests widespread ages of magmatism in the Altai orogenic belt, especially in the Chinese Altai, continuously from the early Paleozoic to the early Mesozoic ( Fig. 1; Han et al, 1997;Chen and Arakawa, 2005;Zhu et al, 2006;Briggs et al, 2007;Long et al, 2007;Yuan et al, 2007;Sun et al, 2008;Cai et al, 2011aCai et al, , 2011bCai et al, , 2012Ren et al, 2011;Lv et al, 2012;Zhang et al, 2017). Previous studies also pinpointed the sequential emplacement of early Paleozoic I-type, S-type, and volcanic-arc granites in the Chinese Altai, which reached a peak in the Devonian.…”
Section: Geological Settingmentioning
confidence: 90%
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“…The Central Asian Orogenic Belt (CAOB) is one of the largest and best‐preserved Proterozoic‐to‐Phanerozoic accretionary orogenic belts on Earth. The CAOB preserve evidence for the addition of significant amounts of juvenile crust (Du et al, ; He, Klemd, Yan, & Zhang, ; Jahn, ; Li et al, ; Şengör et al, ; Zhang, Liu, Santosh, Luo, & Zhang, ). It is characterized by large volumes of Palaeozoic and Mesozoic granitic intrusions as well as basaltic to rhyolitic rocks, with positive εNd ( t ) and εHf ( t ) values and low initial Sr isotopic ratios (Hu et al, ; Jahn, ; Li et al, ; Su et al, ; Windley et al, ).…”
Section: Introductionmentioning
confidence: 96%