SIMS analysis of REE in pyroxenes and amphiboles from the Proterozoic Ikasaulak intrusive complex (SE Greenland): implications for LREE enrichment processes during post-orogenic plutonism
References (47)
- et al.
Solar system abundances of the elements
Geochim. Cosmochim. Acta
(1982) - et al.
Petrogenesis of layered pyroxenites from the Lherz, Freychinede and Prades ultramafic bodies (Ariege, French Pyrenees)
Geochim. Cosmochim. Acta
(1987) - et al.
Geochemistry and petrogenesis of Eastern Pyrenean peridotites
Geochim. Cosmochim. Acta
(1988) - et al.
Evolution of the upper mantle beneath southeast Australia: geochemical evidence from peridotite xenoliths in Mont Leura basanite
Earth Planet. Sci. Lett.
(1989) - et al.
Rare earth elements in igneous rocks of the continental crust: predominantly basic and ultrabasic rocks
Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization
Earth Planet. Sci. Lett.
(1981)General geochemical properties and abundances of the rare earth elements
- et al.
Trace element abundances in megacrysts and their host basalts: constraints on partition coefficients and megacryst genesis
Geochim. Cosmochim. Acta
(1984) - et al.
Nagssugtoqidian mobile belt of West Greenland: a kryptic 1850 Ma suture between two Archaean continents—chemical and isotopic evidence
Earth Planet. Sci. Lett.
(1987) - et al.
Mafic and ultramafic pods with eclogitic relics from the Proterozoic Nagssugtoqidian mobile belt of East Greenland
Lithos
(1990)
Clinopyroxene-orthopyroxene major and rare earth elements partitioning in spinel peridotite xenoliths from assab (Ethiopia)
Geochim. Cosmochim. Acta
Petrogenetic implications of some new geochemical data on eclogitic and ultrabasic inclusions
Geochim. Cosmochim. Acta
Fractionation of uranium, thorium and rare earth elements in a vertically zoned granodiorite: implications for heat production distributions in the Sierra Nevada batholith, California, U.S.A.
Geochim. Cosmochim. Acta
Rare earth element partitioning between minerals from anhydrous spinel peridotite xenoliths
Geochim. Cosmochim. Acta
Geochemistry and mineralogy of two spinel peridotite suites from Dreiser Weiher, West Germany
Geochim. Cosmochim. Acta
Geochemical characteristics of Proterozoic post-orogenic magmatism in the Nagssugtoqidian Mobile Belt of southeast Greenland
Lithos
Origin of amphibole in recrystallized and porphyroclastic mantle xenoliths from the Rhenish Masif: implications for the nature of mantle metasomatism
Earth Planet. Sci. Lett.
A SIMS application to petrogenetic problems: the 1500 Ma post-orogenic plutonism of SE Greenland
Quantitative SIMS analysis of Rare Earth elements in maficultramafic rock samples
Nagssugtoqidian mobile belt in East Greenland
Outline of the Nagssugtoqidian mobile belt of East Greenland
Rapp. Grønl. Geol. Unders.
The geochemical characteristics of granitoids in contrasting arcs and comments on magma sources
J. Geol. Soc. London
Experimental data at 3 Kbars pressure on parental magma to the Bushveld Complex
Contrib. Mineral. Petrol.
Cited by (13)
Early Cretaceous subduction-modified lithosphere beneath the eastern Qinling Orogen revealed from the Daying volcanic sequence in central China
2019, Journal of Asian Earth SciencesCitation Excerpt :Decreasing MgO and FeOt with increasing SiO2 contents, along with the positive correlation between MgO and V suggest fractional crystallization of olivine, clinopyroxene and hornblende. Apatite and Fe-Ti oxide crystal fractionation are revealed from the negative correlations of SiO2 with TiO2 and P2O5, and negative P-Ti anomalies (e.g., Vannucci et al., 1991; Francis, 1995). The lack of Sr and Eu negative anomalies suggests limited plagioclase fractionation (Fig. 9).
Trace element variations in clinopyroxene and amphibole from alkaline to peralkaline syenites and granites: Implications for mineral-melt trace-element partitioning
2004, Chemical GeologyCitation Excerpt :Zr, Hf and Sn develop a preference for clinopyroxene as the system evolves towards Ca–Na and Na-rich compositions, but absolute DZr and DHf values >1 only occur in the Ca–Na system (Grønnedal-Ika). For Zr and Hf, literature data are contradictory, indicating similar compatibilities in andesitic rocks (Brenan et al., 1995), variable behavior (Vannucci et al., 1991) or a preference for amphibole (Chazot et al., 1996) in ultramafic rocks. The Dcpx–amph values of the REE are continuously increasing from the LREE towards the HREE in the Ilímaussaq and Grønnedal-Ika rocks.
Late Mesozoic calc-alkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains, northeastern China
2003, Journal of Volcanology and Geothermal ResearchTrace element partition coefficients for clinopyroxene and phlogopite in an alkaline lamprophyre from Newfoundland by LAM-ICP-MS
1996, Geochimica et Cosmochimica Acta