2016
DOI: 10.1016/j.lithos.2015.11.024
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Petrogenesis and geochemistry of the Late Carboniferous rear-arc (or back-arc) pillow basaltic lava in the Bogda Mountains, Chinese North Tianshan

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Cited by 58 publications
(59 citation statements)
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“…In this study, the volcanics of the Upper Carboniferous Liushugou Formation are not bimodal in composition, but their generation is related to bimodal magma (basaltic and rhyolitic magmas), indicating an extensional environment. Occurrence of the Bogda high-Al basalt (HAB) and pillow basalt suggests a back-arc (or rear-arc) setting for the Bogda belt in the Late Carboniferous (Xie et al, 2016a(Xie et al, , 2016b. Therefore, an alternative setting for the Bogda belt is that it was a back-arc extensional environment in the Carboniferous (Fig.…”
Section: Tectonic Implicationmentioning
confidence: 99%
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“…In this study, the volcanics of the Upper Carboniferous Liushugou Formation are not bimodal in composition, but their generation is related to bimodal magma (basaltic and rhyolitic magmas), indicating an extensional environment. Occurrence of the Bogda high-Al basalt (HAB) and pillow basalt suggests a back-arc (or rear-arc) setting for the Bogda belt in the Late Carboniferous (Xie et al, 2016a(Xie et al, , 2016b. Therefore, an alternative setting for the Bogda belt is that it was a back-arc extensional environment in the Carboniferous (Fig.…”
Section: Tectonic Implicationmentioning
confidence: 99%
“…Therefore, an alternative setting for the Bogda belt is that it was a back-arc extensional environment in the Carboniferous (Fig. 13A) (Chen et al, 2013;Zhang et al, 2016;Xie et al, 2016aXie et al, , 2016b.…”
Section: Tectonic Implicationmentioning
confidence: 99%
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