Experimental studies of trace-element partitioning applicable to igneous petrogenesis — Sedona 16 years later

Green, Trevor H.

doi:10.1016/0009-2541(94)90119-8

Cited by 576 publications

(278 citation statements)

References 128 publications

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“…Crosses indicate the calculated trends using the major element results (at 25 8C intervals). Calculated trends (using major element modeling) use spinel/melt partition coefficient data from this study and partition coefficients for olivine from Green (1994). The variation can be ascribed to progressive liquid evolution during fractionation of 0.6% chromite, 8.4% olivine, 26.0% feldspar and 22.9% pyroxene.…”

mentioning

confidence: 98%

“…The variation can be ascribed to progressive liquid evolution during fractionation of 0.6% chromite, 8.4% olivine, 26.0% feldspar and 22.9% pyroxene. Trace element concentrations are calculated using the results of this study (for spinel) and published D's of Green (1994) and Roeder and Reynolds (1991) (Rhodes, 1996;Albarède, 1996). The calculated trends are those resulting from major element modeling using MELTS (Ghiorso and Sack, 1994), and assuming sample R091 as a parental liquid at 5 kb, QFM buffer, between 1500 and 1200 8C.…”

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confidence: 99%

“…The trends shown correspond to liquid evolution during fractionation of 11.6% olivine, 34.3% orthopyroxene and 0.53% spinel. Trace element concentrations are calculated using the results of this study (for spinel) and published D's of Green (1994) and Roeder and Reynolds (1991) . Solid lines with crosses are calculated liquid lines of descent for fractionation of DG30 basalt at 0.5 kb, FMQ-2, at 10 8C intervals (using MELTS of Ghiorso and Sack, 1994).…”

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confidence: 99%

“…The cumulative amount of phases fractionated is as follows: 11% olivine, 28% augite, 37% plagioclase and 6% magnetite. Trace element concentrations are calculated using the results of this study (for spinel) and published D's of Green (1994) …”

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Partitioning of Ni, Co and V between spinel-structured oxides and silicate melts: Importance of spinel composition

Righter¹,

Leeman²,

Hervig³

2006

Chemical Geology

124

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11Partitioning of Ni, Co and V between Cr-rich spinels and basaltic melt has been studied experimentally between 1150 and 1325 12 8C, and at controlled oxygen fugacity from the Co-CoO buffer to slightly above the hematite-magnetite buffer. These new results, 13 together with new Ni, Co and V analyses of experimental run products from Leeman [Leeman, W.P., 1974. Experimental 14 determination of the partitioning of divalent cations between olivine and basaltic liquid, Pt. II. PhD thesis, Univ. Oregon, 231-15 337.], show that experimentally determined spinel-melt partition coefficients (D) are dependent upon temperature (T), oxygen 16 fugacity ( fO 2 ) and spinel composition. In particular, partition coefficients determined on doped systems are higher than those in 17 natural (undoped) systems, perhaps due to changing activity coefficients over the composition range defined by the experimental 18 data. Using our new results and published runs (n = 85), we obtain a multilinear regression equation that predicts experimental

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confidence: 98%

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confidence: 99%

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confidence: 99%

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confidence: 99%

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Partitioning of Ni, Co and V between spinel-structured oxides and silicate melts: Importance of spinel composition

Righter¹,

Leeman²,

Hervig³

2006

Chemical Geology

124

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“…GRS-measured K, U, and Th Figure 1 Calculations of partitioning during partial melting were made using the mass balance The K-U-Th pattern for partial melts could be influenced by volatile components such as H20 and CO2. However, an attempt to allow for the role of volatiles in Venus petrogenesis would raise more questions than it answered because the abundances of volatile species in the Venus interior are poorly constrained (see Hess and Head [1990] for a summary), and necessary data on (low-density fluid)/melt, fluid/mineral partition coefficients, particularly for accessory minerals and for a range of fluid compositions, are among the suggestions for future work made by Green [1994] in his recent review. …”

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Geochemical constraints on petrogenic processes on Venus

Николаева¹,

Ariskin²

1999

J. Geophys. Res.

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Louisville Seamount Chain: Petrogenetic processes and geochemical evolution of the mantle source

Vanderkluysen

Mahoney

Koppers

et al. 2014

Geochem Geophys Geosyst

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The Louisville Seamount Chain is a 4300 km long chain of submarine volcanoes in the southwestern Pacific that spans an age range comparable to that of the Hawaiian-Emperor chain and is commonly thought to represent a hot spot track. Dredging in 2006 recovered igneous rocks from 33 stations on 22 seamounts covering some 49 Myr of the chain's history. All samples are alkalic, similar to previous dredge and drill samples, providing no evidence for a Hawaiian-type tholeiitic shield-volcano stage. Major and trace element variations appear to be predominantly controlled by small but variable extents of fractional crystallization and by partial melting. Isotopic values define only a narrow range, in agreement with a surprising long-term source homogeneity-relative to the length scale of melting-and overlap with proposed fields for the ''C'' and ''FOZO'' mantle end-members. Trace element and isotope geochemistry is uncorrelated with either seamount age or lithospheric thickness at the time of volcanism, except for a small number of lavas from the westernmost Louisville Seamounts built on young (<20 Ma old) oceanic crust. The Louisville hot spot has been postulated to be the source of the 120 Ma Ontong Java Plateau, but the Louisville isotopic signature cannot have evolved from a source with isotopic ratios like those measured for Ontong Java Plateau basalts. On the other hand, this signature can be correlated with that of samples dredged from the Danger Islands Troughs of the Manihiki Plateau, which has been interpreted as a rifted fragment of the ''Greater'' Ontong Java Plateau.

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Experimental studies of trace-element partitioning applicable to igneous petrogenesis — Sedona 16 years later

Cited by 576 publications

References 128 publications

Partitioning of Ni, Co and V between spinel-structured oxides and silicate melts: Importance of spinel composition

Partitioning of Ni, Co and V between spinel-structured oxides and silicate melts: Importance of spinel composition

Geochemical constraints on petrogenic processes on Venus

Louisville Seamount Chain: Petrogenetic processes and geochemical evolution of the mantle source

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