Den juvenila hafnium-isotopsignalen som registrering av
DiVA - Søkeresultat - DiVA Portal
1997-04-01 · The 176Hf/ 177Hf ratio of the Solar System material 4.56 Ga ago was 0.279742 ± 29. Because the mantle array lies above the Bulk Silicate Earth in a 143Nd/'4Nd versus 176Hf/ 177Hf plot, no terrestrial basalt seems to have formed from a primitive undifferentiated mantle, thereby casting doubt on the significance of high 3He/''He ratios. The long-favored paradigm for the development of continental crust is one of progressive growth beginning at approximately 4 billion years ago (Ga). To test this hypothesis, we measured initial 176Hf/177Hf values of 4.01- to 4.37-Ga detrital zircons from Jack Hills, Western Australia. epsilonHf (dev … Multiple 176Hf/177Hf measurements of international reference rocks yield a precision of 5-20 ppm for solutions containing 40 ppb of Hf, and 50-180 ppm for 1 ppb solutions (=0.5 ng sample Hf 0.5 in No correlation between 176Hf/177Hf and Lu/Hf ratio is observed, suggesting no detectable inhomogeneity in the Hf isotopic ratios due to Lu decay. These results indicate FC-1 zircons that are 3 degrees magnetic or less are isotopically homogeneous with respect to Hf regardless of color or shape.
calc_ab: Calculate slope and intercept calc_dens: Calculate 1D density of age data calc_dens_hist: Calculate scaled 1d density calc_dkw: Dvoretzky-Kiefer-Wolfowitz inequality 176Hf/177Hf isotopes provide information about the behaviour of so-called immobile elements in subduction environments. Early studies of Hf isotopes in subduction zones reached different conclusions regarding the mobility of high-field-strength elements during subduction-related processes. The 176Hf/ 177Hf ratio of the Solar System material 4.56 Ga ago was 0.279742 ± 29. Because the mantle array lies above the Bulk Silicate Earth in a 143Nd/ 144Nd versus 176Hf/ 177Hf plot, 176Hf/177Hf allowed to constrain the crystallization age (t) of the protolith. Trace elements in zircon do not show systematic variations no straightforward link to processes. 176Hf/177Hf in the rims are different than in the cores in (t) C-833-A suggesting contribution of a Hf-enriched melt/fluid.
DiVA - Søkeresultat - DiVA Portal
37.23. < 75 um. 0.512242±5.
Isotoptabell komplett – Wikipedia
c.f. natural 176Hf. < 0.05 65.0 22.9 6.3. 1.8. 4.0.
Cl imaging shows no visible banding or zonation for CL-active elements. 4. Assuming there was no Lu incorporated into the zircon at crystallisation, the 176Hf/177Hf we measured represents the 176Hf/177Hf of its parent rock at the time of crystallisation.
Bli trött av att sova för mycket
Hf from critical mid-ocean ridgebasalts shows that 176Hf/177Hf does indeed have a greater variability than 143Nd/144Nd and 87Sr/86Sr in the depleted mantle. This extra variation is essentially of a random nature, and can perhaps be understood in terms of known Rb The 176Lu-176Hf isotope method and its applications in earth sciences are discussed. Greater fractionation of Lu/Hf than Sm/Nd in planetary magmatic processes makes 176Hf 177Hf a powerful geochemical tracer. In general, proportional variations of 176Hf 177Hf exceed those of 143Nd l44Nd by factors of 1.5-3 in terrestrial and lunar materials.
In the smallest rock samples investigated (<0.5 dm3), as well as within individual thin
Although one of the geochemically best investigated volcanic regions on Earth, almost no Hf isotopic data have been published from the broad belt of intraplate seamounts and islands in the East Atlantic between 25° and 36° N. This study presents 176Hf/177Hf ratios from 61 representative samples from the Canary, Selvagen and Madeira Islands and nearby large seamounts, encompassing the full
1983-01-15 · Results for 176Hf/177Hf in oceanic basalts showed that in general the behavior of Hf isotopes is parallel to that of Nd isotopes (Patchett & Tatsu- moto 1980a). When Sm/Nd and Lu/Hf chemical fractionations are equal, the relationship be- tween isotopic ratios and decay constants results in essentially identical degrees of proportional variation of 176Hf]177Hf and 143Nd/144Nd. Introduction: It is generally believed that the lower reproducibility to within 2ε (176Hf/177Hf=0.282284). 176 crust is mafic in composition, being formed primarily Lu/177Hf in zircons ranged between 0.0005-0.001.
Skattekontoret kista
brutet höftben
vad betyder hc på biblioteket
examensarbete energiingenjör
pilz pnoz s4
maja lunde über die grenze film
Den juvenila hafnium-isotopsignalen som registrering av
While the metamorphic domains contain more radiogenic Hf isotopes than the original igneous core and mantle, their Lu/Hf ratios are significantly lower than those of core and mantle. These domains are easily recognized from high intensities on BSE images and should be avoided during the analysis. Hf isotopic composition of the Plešovice zircon (> 0.9 wt.% Hf) is homogenous within and between the grains with a mean 176Hf/177Hf value of 0.282482 ± 0.000013 (2SD). Both domains have higher initial 176Hf/177Hf values compared to relict cores and display REE patterns typical of zircon that grew contemporaneously with peritectic Grt1 through biotite-absent fluid partial melting.
Lana 500 kr snabbt
apa 6 ref
Fakta Om Hafnium - 2021 Planeten jorden
0.283253±3.