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Fanning, Christopher
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Fanning, Christopher
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Cretaceous oblique extensional deformation and magma accumulation in the Fosdick...
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Hf- and O-isotope data from detrital and granitoid zircons reveal characteristic...
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Evolution of provenance in the NE Atlantic rift: The Early-Middle Jurassic succe...
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Geochronological constraints on the Late Proterozoic to Cambrian crustal evoluti...
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Provenance and age constraints of Paleozoic siliciclastic rocks from the Ellswor...
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Chronological study of the pre-Permian basement rocks of southern Patagonia
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Ross Sea Mylonites and the timimg of intracontinental extension within the West...
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Siliciclastic record of rapid denudation in response to convergent-margin orogen...
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Chronological study of the pre-Permian basement rocks of southern Patagonia
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Mid-Cretaceous oblique rifting of West Antarctica: Emplacement and rapid cooling...
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Siliciclastic record of rapid denudation in response to convergent-margin orogen...
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Ross Sea Mylonites and the timimg of intracontinental extension within the West...
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Detrital zircon age constraints on the provenance of sandstones on Hatton Bank a...
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Oblique dilation, melt transfer, and gneiss dome emplacement
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Detrital zircon age constraints on the provenance of sandstones on Hatton Bank a...
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Oblique dilation, melt transfer, and gneiss dome emplacement
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Zircon O- and Hf-isotope constraints on the genesis and tectonic significance of...
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The Permo-Triassic Gondwana sequence, central Transantarctic Mountains, Antarcti...
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Maximum depositional age and provenance of the Uinta Mountain Group and Big Cott...
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From passive margin to volcano-sedimentary forearc: the Tonian to Cryogenian evo...
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Related Subjects
Antarctica
zircon
Gondwana
Proterozoic
uranium-lead dating
SHRIMP dating
geochronology
granite
Zircon
orogeny
East Antarctica
Keywords: basement rock
provenance
tectonic evolution
isotopic composition
Geochronology
Paleozoic
U-Pb SHRIMP
West Antarctica
detrital deposit
Cambrian
Geochemistry
Keywords: Archean
Permian
Rodinia
article
geochemistry
sandstone
Jurassic
Eurasia
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