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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
The final collision of the CAOB: Constraint from the zircon U–Pb
The final collision of the CAOB: Constraint from the zircon U–Pb
Zircon U-Pb geochronology, Hf isotopes, and geochemistry
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
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The final collision of the CAOB: Constraint from the zircon U–Pb
Large-number detrital zircon U-Pb ages reveal global cooling
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
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The final collision of the CAOB: Constraint from the zircon U–Pb
PDF) A-type granites from the Pan-African orogenic belt in south
The final collision of the CAOB: Constraint from the zircon U–Pb
History of collision between the Jiamusi and Songliao blocks: new
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
a) U-Pb concordia diagram of all zircon data for sample HC-1; (b
The final collision of the CAOB: Constraint from the zircon U–Pb
Concordia U–Pb diagrams (a) and (c), chondrite‐normalized REE
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