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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
PDF) Evolution from Oceanic Subduction to Continental Collision: a
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
Evolution of the Paleo–Asian Ocean in south‐eastern Inner Mongolia
The final collision of the CAOB: Constraint from the zircon U–Pb
U–Pb dating of detrital zircons in the eastern Guangdong Basin
The final collision of the CAOB: Constraint from the zircon U–Pb
U–Pb geochronology and Lu–Hf isotopes of zircons from newly
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
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 Geochronological Constraint on the Evolution of the
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
Zircon U-Pb-Hf isotopes and geochemistry of Jurassic igneous rocks
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
Zircon: Mineral information, data and localities.
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