The provenance of Late Ediacaran and Early Ordovician siliciclastic rocks in the
U–Pb geochronology of detrital zircon from Late Ediacaran (Beiras Group greywackes) and Early Ordovician (Sarnelhas arkosic quartzites and Armorican quartzites of Penacova) sedimentary rocks of the southwest Central Iberian Zone (SW CIZ) constrain the evolution of northern Gondwana active-passive ma...
Main Author: | |
---|---|
Other Authors: | , , , , , |
Format: | article |
Language: | por |
Published: |
2011
|
Subjects: | |
Online Access: | http://hdl.handle.net/10174/2984 |
Country: | Portugal |
Oai: | oai:dspace.uevora.pt:10174/2984 |