Casacaob

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

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Last updated 28 março 2025
The final collision of the CAOB: Constraint from the zircon U–Pb
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
Zircon U–Pb geochronology and Sr–Nd–Hf–O isotopic constraints on
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
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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
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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
PDF) The final collision of the CAOB: Constraint from the zircon U
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
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The final collision of the CAOB: Constraint from the zircon U–Pb
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Origin and Palaeozoic reworking of the Central Tianshan Block
The final collision of the CAOB: Constraint from the zircon U–Pb
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