Ediacaran to Lower Ordovician age for rocks ascribed to the Schist–Graywacke Complex (Iberian Massif, Spain): Evidence from detrital zircon SHRIMP U–Pb geochronology
New SHRIMP U–Pb ages of detrital zircon obtained from eight samples of Neoproterozoic to Lower Paleozoic graywackes, schists, microconglomerates and shales provide the maximum depositional age and a new zircon age pattern for the Schist–Graywacke Complex (SGC) from the Iberian Massif (SW Europe). Th...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2012
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/17864 |