A comparison of detrital U–Pb zircon, 40Ar/39Ar hornblende, 40Ar/39Ar biotite ages in marine sediments off East Antarctica: Implications for the geology of subglacial terrains and provenance studies

Author:

Pierce E.L.,Hemming S.R.,Williams T.,van de Flierdt T.,Thomson S.N.,Reiners P.W.,Gehrels G.E.,Brachfeld S.A.,Goldstein S.L.

Funder

NSF

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference153 articles.

1. 40Ar/39Ar dating of detrital micas from Oligocene–Pleistocene sandstones of the Olympic Peninsula, Klamath Mountains, and northern California Coast Ranges: provenance and palaeodrainage patterns;Aalto;Can. J. Earth Sci.,1998

2. Style of uplift of Paleozoic Terranes in Northern Victoria Land, Antarctica: evidence from K–Ar age patterns;Adams,2006

3. Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation;Andersen;Chem. Geol.,2005

4. Antarctic Marine Geology, Cambridge;Anderson,1999

5. K–Ar dating: Late Cenozoic McMurdo Volcanic Group and dry valley glacial history, Victoria Land, Antarctica;Armstrong;N. Z. J. Geol. Geophys.,1978

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