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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
Linking magmatism with collision in an accretionary orogen
The final collision of the CAOB: Constraint from the zircon U–Pb
Full article: Sedimentary response to the non-synchronous closure
The final collision of the CAOB: Constraint from the zircon U–Pb
Frontiers Intra-oceanic subduction in the southeastern Paleo
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
Frontiers New geochronological and provenance constraints on the
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
Final Assembly of the Southwestern Central Asian Orogenic Belt as
The final collision of the CAOB: Constraint from the zircon U–Pb
Minerals, Free Full-Text
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
Minerals, Free Full-Text
The final collision of the CAOB: Constraint from the zircon U–Pb
Final closure of the Paleo Asian Ocean basin in the early Triassic
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