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- W2393326517 abstract "Baimashan pluton in the southeastern of Xuefeng orogen is mainly composed of Caledonian granites with minor Indosinian and Yanshanian granites.The Caledonian granites are mainly located in the central and eastern of Baimashan pluton,which can be divided into four periods.U-Pb zircon dating of the second-intruded fine-grained to medium-grained porphyritic amphibole biotite granodiorite(γδSb) was carried out and yield weighted average age of 411±4.5 Ma,which indicates one magmatic event in late episode of Silurian to the early stage of Devonian.Geochemical characteristics indicate it belongs to S-type granitiod and suggest that it should come from acid rocks of middle crust.The first-intruded tonalite(γδοSa) is a little intrusion,which relicted in the third intrusion.It indicates that Baimashan granites hadn't experienced earlier large-scale magmatism,so we can inferred that Caledonian Baimashan granites was a product of the late Silurian deformation Guangxi Movement.The west of Chengbu-Xinhua Fault was a foreland basin regionally,which deposited sand and muddy sediments.The east part of this fault of the southeastern of Hunan Province was lack of Silurian sedimentary.It suggested the east part of Chengbu-Xinhua Fault had been thrust uplift and denudation,while the west part formed foreland basin." @default.
- W2393326517 created "2016-06-24" @default.
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- W2393326517 date "2015-01-01" @default.
- W2393326517 modified "2023-09-23" @default.
- W2393326517 title "Zircon SHRIMP U-Pb dating and Geochemistry of Caledonian Baimashan pluton and its tectonic significance" @default.
- W2393326517 hasPublicationYear "2015" @default.
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