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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
Concordia U–Pb diagrams (a) and (c), chondrite‐normalized REE
The final collision of the CAOB: Constraint from the zircon U–Pb
Evolution of the Paleo–Asian Ocean in south‐eastern Inner Mongolia
The final collision of the CAOB: Constraint from the zircon U–Pb
Zircon U–Pb and Hf isotopic study of Neoproterozoic granitic
The final collision of the CAOB: Constraint from the zircon U–Pb
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The final collision of the CAOB: Constraint from the zircon U–Pb
Frontiers Geochronological Constraint on the Evolution of the
The final collision of the CAOB: Constraint from the zircon U–Pb
Final Assembly of the Southwestern Central Asian Orogenic Belt as
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
Zircon U-Pb chronology, geochemistry and geological significance
The final collision of the CAOB: Constraint from the zircon U–Pb
The final collision of the CAOB: Constraint from the zircon U–Pb
The final collision of the CAOB: Constraint from the zircon U–Pb
Full article: Zircon U-Pb-Hf isotopes and geochemistry of Jurassic
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