Constraints on the thermal evolution of metamorphic core complexes from the timing of high-pressure metamorphism on Naxos, Greece
Metamorphic core complexes are classically interpreted to have formed during crustal extension, although many also occur in compressional environments. New U–(Th)–Pb allanite and xenotime geochronologic data from the structurally highest Zas Unit (Cycladic Blueschist Unit) of the Naxos metamorphic c...
| Príomhchruthaitheoirí: | , , , , , |
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| Formáid: | Journal article |
| Teanga: | English |
| Foilsithe / Cruthaithe: |
Geological Society of America
2023
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