(2012). Detrital zircon provenance from the Neuquén Basin (south-central Andes): Cretaceous geodynamic evolution and sedimentary response in a retroarc-foreland basin.
Cita Chicago Style (17a ed.)Detrital Zircon Provenance from the Neuquén Basin (south-central Andes): Cretaceous Geodynamic Evolution and Sedimentary Response in a Retroarc-foreland Basin. 2012.
Cita MLA (8a ed.)Detrital Zircon Provenance from the Neuquén Basin (south-central Andes): Cretaceous Geodynamic Evolution and Sedimentary Response in a Retroarc-foreland Basin. 2012.
Precaución: Estas citas no son 100% exactas.