Casacaob

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

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Last updated 03 maio 2024
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
The timing of final closure along the Changchun–Yanji suture zone
The final collision of the CAOB: Constraint from the zircon U–Pb
Origin and Palaeozoic reworking of the Central Tianshan Block
The final collision of the CAOB: Constraint from the zircon U–Pb
Central Asian Orogenic Belt - Wikipedia
The final collision of the CAOB: Constraint from the zircon U–Pb
U-Pb concordia diagrams and mean age histogram of zircons from
The final collision of the CAOB: Constraint from the zircon U–Pb
Full article: Middle Jurassic–Early Cretaceous tectonic evolution
The final collision of the CAOB: Constraint from the zircon U–Pb
Late Magmatic Activity in the Tarim Large Igneous Province
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
Central Asian Orogenic Belt - Wikipedia
The final collision of the CAOB: Constraint from the zircon U–Pb
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