Zobrazeno 1 - 10
of 20
pro vyhledávání: '"W J Dunlap"'
Publikováno v:
Alcheringa: An Australasian Journal of Palaeontology. 32:129-147
MENZIES, J., DAVIES, H.L., DUNLAP, W.J. & GOLDING, S.D., June, 2008. A possible early age for a diprotodon (Marsupialia: Diprotodontidae) fossil from the Papua New Guinea highlands. Alcheringa 32, 129–147. ISSN 0311-5518. A fossil diprotodon jawbon
Autor:
W J Dunlap, Roberto F. Weinberg
Publikováno v:
Tectonophysics. 340:265-268
Autor:
A. K. Kronenberg, W. J. Dunlap
Publikováno v:
Contributions to Mineralogy and Petrology. 141:174-185
The role of internal deformation in resetting argon ages of micas has been investigated by measuring 40Ar/39Ar ratios of biotite and muscovite, before and after experimentally deforming them. Neither mica crushed cataclastically at room temperature o
Autor:
W. J. Dunlap
Publikováno v:
Geology. 28:139-142
Publikováno v:
Geological Society, London, Special Publications. 170:253-275
Autor:
Haakon Fossen, W. J. Dunlap
Publikováno v:
Tectonics. 17:604-620
Southern Norway was subjected to contractional orogenesis and subsequent extensional collapse during the early to middle Paleozoic when Baltica collided with Laurentia, resulting in the Caledonian Orogen. The largely unknown post-Caledonian Paleozoic
Publikováno v:
Tectonics. 16:983-1000
The thermomechanical evolution of a midcrustal ductile duplex in central Australia has been reconstructed through space and time using 40Ar/39Ar thermochronology, flow stress estimates, cross-sectional restoration of dislocation creep microstructures
Publikováno v:
Tectonics. 31
[1] New 40Ar/39Ar ages from detrital K-feldspars and metamorphic white micas from the Eastern Province terranes of New Zealand have been used to investigate the thermo-tectonic history of different parts of an exhumed Mesozoic forearc basin and accre
Publikováno v:
Tectonics. 27
[1] Integration of in situ and conventional ion microprobe U-Th-Pb zircon and monazite geochronology with 40Ar/39Ar hornblende, biotite, and muscovite thermochronology provides a temporal record of metamorphism, partial melting, fluids, and cooling o
Autor:
Noel C. White, Peter W. Reiners, David R. Cooke, W. J. Dunlap, Charlotte M. Allen, Ian H. Campbell, Anthony C. Harris
Publikováno v:
Mineral Deposit Research: Meeting the Global Challenge ISBN: 9783540279457
Dacitic rocks at the Bajo de la Alumbrera porphyry Cu-Au deposit (NW Argentina) preserve textures that suggest volatiles streamed upwards through intrusions temporally related to ore formation and hydrothermal alteration. There is evidence that volat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6fe719e7da0bb573fffbdd8d51f46656
https://doi.org/10.1007/3-540-27946-6_103
https://doi.org/10.1007/3-540-27946-6_103