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The final collision of the CAOB: Constraint from the zircon U–Pb

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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…
The final collision of the CAOB: Constraint from the zircon U–Pb
Detrital zircon U–Pb geochronology and geochemistry of late
The final collision of the CAOB: Constraint from the zircon U–Pb
Relative probability plot of the zircon U-Pb ages for the Mesozoic
The final collision of the CAOB: Constraint from the zircon U–Pb
Distribution of zircon TDM2 (Hf) ages (blue bars) and U-Pb ages
The final collision of the CAOB: Constraint from the zircon U–Pb
PDF) Evolution from Oceanic Subduction to Continental Collision: a
The final collision of the CAOB: Constraint from the zircon U–Pb
Final closure of the Paleo Asian Ocean basin in the early Triassic
The final collision of the CAOB: Constraint from the zircon U–Pb
Zircon U-Pb-Hf isotopes and geochemistry of Jurassic igneous rocks
The final collision of the CAOB: Constraint from the zircon U–Pb
U–Pb geochronology and Lu–Hf isotopes of zircons from newly
The final collision of the CAOB: Constraint from the zircon U–Pb
Petrogenesis and tectonic setting of the Chaheilingashun pluton
The final collision of the CAOB: Constraint from the zircon U–Pb
Frontiers Geochemistry and geochronology of basic igneous rocks
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