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THE SOURCE OF THE ESPINHAÇO DIAMONDS: EVIDENCES FROM SHRIMP U-PB ZIRCON AGES OF THE SOPA CONGLOMERATE AND PB-PB ZIRCON EVAPORATION AGES OF METAVOLCANIC ROCKSTHE SOURCE OF THE ESPINHAÇO DIAMONDS: EVIDENCES FROM SHRIMP U-PB ZIRCON AGES OF THE SOPA CONGLOMERATE AND PB-PB ZIRCON EVAPORATION AGES OF METAVOLCANIC ROCKS
(Sociedade Brasileira de Geologia, 2017)
U–Pb SHRIMP detrital zircon dating of metamorphic rocks in north–central Chile (28°–33°S): Evidence for Carboniferous and Triassic metamorphism in a subduction setting
(Elsevier, 2020)
U-Pb SHRIMP detrital zircon dating of ten samples of metamorphic "basement" rocks in north-central Chile and one granitic rock, improve knowledge of sedimentary, metamorphic and plutonic events in this segment of the Andean ...
Provenance variations in the Late Paleozoic accretionary complex of central Chile as indicated by detrital zircons
(Elsevier, 2013)
We present detrital zircon U\Pb SHRIMP age patterns for the central segment (34–42°S) of an extensive accretionary
complex along coastal Chile together with ages for some relevant igneous rocks. The complex consists
of ...
Detrital zircons U-Pb SHRIMP ages and provenance of La Modesta Formation, Patagonia Argentina
(Elsevier, 2013)
This paper summarizes the geology of the Paleozoic La Modesta Formation in Patagonia, Argentina, and
presents new SHRIMP UePb dating of detrital zircons from muscovite-chlorite schist and tourmalinite.
Also complementary ...