Differences in Geochemical Signatures and Petrogenesis between the Van Canh and Ben Giang-Que Son Granitic Rocks in the Southern Kontum Massif, Vietnam

Permian Ben Giang-Que Son and Triassic Van Canh granitic rocks are widely distributed across the southern Kontum Massif, the basement of which consists mainly of metasedimentary rocks. The Ben Giang-Que Son granitic rocks are classified as I- to S-type and ilmenite-series granitic rocks, while the V...

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Bibliographic Details
Published in:	Geosciences (Basel) Vol. 13; no. 11; p. 341
Main Authors:	Uchida, Etsuo, Yonezu, Ko, Yokokura, Takumi, Mori, Nasuka
Format:	Journal Article
Language:	English
Published:	Basel MDPI AG 01-11-2023
Subjects:	Aluminum Ben Giang-Que Son granitic rocks Biotite Carbon Continental crust Earth science Environmental aspects geochemical signatures Geochemistry Geological research Granite Graphite High temperature Ilmenite Isotope ratios Isotopes Kontum Massif Lava Magma magnetic susceptibility Magnetite Massifs Mechanical properties Metamorphic rocks Metamorphism Minerals Oceanic crust Oceans Paleoceanography Permian Petrogenesis Ratios Sedimentary rocks Signatures Strontium isotopes Subduction Triassic Van Canh granitic rocks Japan Vietnam China Indochina
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