Browsing ELibrary by Author "Halliday A.N."
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Browsing ELibrary by Author "Halliday A.N."
Now showing items 1-20 of 32
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Snyder G.A.; Neal C.R.; Taylor L.A.; Halliday A.N. (1997)In an effort to elucidate the processes of lunar mantle melting, and the magma evolution of mare basalts within Oceanus Procellarum on the western lunar near-side, we have analyzed seven fine-grained to vitrophyric Apollo ...
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Leya I.; Wieler R.; Halliday A.N. (2000)Excesses and deficiencies in 182W in meteorites and lunar samples relative to the terrestrial 182W atomic abundance have been assigned to the decay of 182Hf (t1/2=9 Ma) and have been used to date metal-silicate fractionation ...
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Lee D.C.; Halliday A.N.; Leya I.; Wieler R.; Wiechert U. (2002)The decay of formerly live 182Hf with a half-life of 9 Myr results in variations in the abundance of 182W in early solar system objects. Here we demonstrate that major excesses in 182W in some lunar samples are the results ...
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Pettke T.; Halliday A.N.; Hall C.M.; Rea D.K. (2000)The silicate fractions of recent pelagic sediments in the central north Pacific Ocean are dominated by eolian dust derived from central Asia. An 11 Myr sedimentary record at ODP Sites 885/886 at 44.7 degrees N, 168.3 degrees ...
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Amelin Y.; Lee D.C.; Halliday A.N. (2000)We report detailed high precision combined single grain U-Pb and Lu-Hf studies of early zircons to obtain more reliable indications of the extent of mantle depletion and crustal recycling in the Archean. Despite the ...
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Lee D.C.; Halliday A.N. (2000)Three ordinary chondrites, Forest Vale (H4), Ste. Marguerite (H4) and Richardton (H5) have been studied with 182Hf-182W system (t1/2=9 million years [m.y.]) in order to provide constraints on the initial 182Hf/180Hf for ...
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Snyder G.A.; Lee D.C.; Ruzicka A.M.; Prinz M.; Taylor L.A.; Halliday A.N. (2001)We report the first Sm-Nd and Rb-Sr isotopic analyses of silicate inclusions in four IIE iron meteorites: Miles, Weekeroo Station A and B, and Watson. We also report the Hf-W isotopic composition of a silicate inclusion ...
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Stirling C.H.; Lee D.C.; Christensen J.N.; Halliday A.N. (2000)We have developed a method for the rapid, in situ measurement of U-Th isotopic compositions at the semimicro scale using laser ablation sampling, combined with multiple collector ICP magnetic sector mass spectrometry ...
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Halliday A.N.; Porcelli D. (2001)The depletion of moderately volatile elements in planetesimals and planets is generally considered to be a result of removal of hot nebula gases. This theory can be tested with Sr isotopes. The calculated initial 87Sr/86Sr ...
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Wen Y.; Halliday A.N.; Der-Chuen L.; Christensen J.N. (1995)The geochemistry of In and Sn are poorly understood, in part, because of difficulties in obtaining accurate concentrations for these elements in geological materials. Furthermore, In/Sn ratios in sulfides could be sufficiently ...
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Rehkämper M.; Halliday A.N.; Lee D.C.; Fitton J.G.; Wieneke M.; Arndt N.T. (1999)The concentrations of the platinum-group elements (PGE) Ir, Ru, Pt, and Pd were determined in 18 mantle-derived basalts from a variety of tectonic settings and six komatiites from three locations. All analyses were performed ...
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Poitrasson F.; Halliday A.N.; Lee D.-C.; Levasseur S.; Teutsch N. (2004)The iron isotope compositions of Shergotty–Nakhla–Chassigny (SNC) meteorites thought to come from Mars, eucrites and diogenites assumed to sample asteroid 4 Vesta, and rocks from the Moon and Earth have been measured using ...
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Cohen B.A.; Levasseur S.; Zanda B.; Hewins R.H.; Halliday A.N. (2006)Iron isotopic compositions measured in chondrules from various chondrites vary between ?57Fe/54Fe = +0.9? and -2.0?, a larger range than for igneous rocks. Whether these compositions were inherited from chondrule precursors, ...
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Nielsen S.G.; Rehk?mper M.; Halliday A.N. (2006)Lead-205 decays to 205Tl with a half-life of 15 Myr and should have been present in the early solar system according to astrophysical models. However, despite numerous attempts, Tl isotopic measurements of meteorites have ...
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Dong H.; Hall C.M.; Halliday A.N.; Peacor D.R. (1997)Laser 40Ar-39Ar ages were obtained from a series of replicate illite samples ranging in mass from 14 to 77 μg using vacuum-encapsulated irradiation, and the results were compared with earlier analyses of the same material ...
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van de Flierdt T.; Frank M.; Halliday A.N.; Hein J.R.; Hattendorf B.; Günther D.; Kubik P.W. (2003)The sources of non-anthropogenic Pb in seawater have been the subject of debate. Here we present Pb isotope time-series that indicate that the non-anthropogenic Pb budget of the northernmost Pacific Ocean has been governed ...
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Snyder G.A.; Jerde E.A.; Taylor L.A.; Halliday A.N.; Sobolev V.N.; Sobolev N.V. (1993)Nd and Sr isotopic data from diamond-bearing eclogites found in the Udachnaya kimberlite, Yakutia, Siberia, are interpreted as indicating an early (⩾ 4 Ga) differentiation event, whereby the mantle split into complementary ...
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van de Flierdt T.; Frank M.; Lee D.C.; Halliday A.N.; Reynolds B.C.; Hein J.R. (2004)The behavior of dissolved Hf in the marine environment is not well understood due to the lack of direct seawater measurements of Hf isotopes and the limited number of Hf isotope time-series obtained from ferromanganese ...
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Schönbächler M.; Rehkämper M.; Fehr M.A.; Halliday A.N.; Hattendorf B.; Günther D. (2005)Stepwise dissolutions of the carbonaceous chondrites Orgueil (CI), Murchison (CM) and Allende (CV) reveal large nucleosynthetic anomalies for Zr isotopes that contrast with the uniform compositions found in bulk meteorites. ...
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Pettke T.; Lee D.C.; Halliday A.N.; Rea D.K. (2002)The inorganic silicate fraction extracted from bulk pelagic sediments from the North Pacific Ocean is eolian dust. It monitors the composition of continental crust exposed to erosion in Asia. 176Lu/177Hf ratios of modern ...
Now showing items 1-20 of 32
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