The final collision of the CAOB: Constraint from the zircon U–Pb
Por um escritor misterioso
Last updated 24 fevereiro 2025
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The Linxi Formation occupies an extensive area in the eastern Inner Mongolia in the Central Asian Orogenic Belt (CAOB). The Linxi Formation is compose…
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Full article: Sediment provenances of a Mesozoic intracontinental
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U–Pb dating of detrital zircons in the eastern Guangdong Basin
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Late Paleozoic Accretionary and Collisional Processes along the
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The final collision of the CAOB: Constraint from the zircon U–Pb
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Geochemistry and zircon U–Pb–Hf isotopic data for Permo
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History of collision between the Jiamusi and Songliao blocks: new
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Detrital zircon U–Pb geochronology and geochemistry of late
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Linking magmatism with collision in an accretionary orogen
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Petrogenesis, W metallogenic and tectonic implications of granitic
Ka'ena Volcano: First building block for O'ah
Late Magmatic Activity in the Tarim Large Igneous Province
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Final closure of the Paleo Asian Ocean basin in the early Triassic
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Triassic Collisional Structures and Post-Collisional Deformation
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Concordia diagrams of zircon U-Pb dating on the igneous rocks of
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Frontiers Geochemistry and geochronology of basic igneous rocks
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