Casacaob

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

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Last updated 03 abril 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
Evolution of the Paleo–Asian Ocean in south‐eastern Inner Mongolia
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
Geochemistry and zircon U–Pb–Hf isotopic data for Permo
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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