Search results for "Leucite"

showing 5 items of 5 documents

Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow dept…

2020

The Pleistocene (~460–265 ka) San Venanzo volcanic complex belongs to the IAP (Intra-Apennine Province) in central Italy, which comprises at least four small Pleistocene monogenetic volcanoes plus several unrooted pyroclastic deposits with peculiar mineralogical and whole-rock chemical compositions. San Venanzo products are strongly SiO2-undersaturated, CaO- and MgO-rich and show ultrapotassic serial character. The relatively common occurrence of calcite in the pyroclastic rocks and the overall high CaO content are interpreted in literature as primary mineral. The main rock facies at San Venanzo are calcite-rich scoria and lapilli tuffs, with minor massive lava flows, and a rare pegma…

010504 meteorology & atmospheric sciencesultrapotassicGeochemistryPyroclastic rockCarbonatite; Kamafugite; mantle plumes; noble gases; Roman comagmatic region; subduction; ultrabasic; ultrapotassicengineering.material010502 geochemistry & geophysicsKamafugite01 natural sciencesUltramafic rockCarbonatiteultrabasicRoman comagmatic region0105 earth and related environmental sciencesPeridotitegeographygeography.geographical_feature_categoryFractional crystallization (geology)Olivinemantle plumesVolcanic rockIgneous rocknoble gasesengineeringGeneral Earth and Planetary SciencesLeucitesubductionGeology
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Trace element partitioning in lamproitic magmas—the Gaussberg olivine leucitite

2004

Abstract Partition coefficients for compatible and incompatible trace elements for use in modelling the origin and evolution of lamproitic and other potassic rocks are reported. These are based on values obtained by in situ determination using laser ablation microprobe-inductively coupled plasma-mass spectrometry (LAM-ICP-MS) on mineral/glass pairs in examples of the Gaussberg olivine leucitite, a classic leucite lamproite. Leucite/melt partition coefficients for 32 elements show values above 1 only for Cs and Rb, whereas values for Ni, Ga and Co are 0.4–0.1. DLc/Lq for most other elements are in the range 0.07–0.0005, and delineate a gently sloping pattern to lower values for elements gene…

BasaltIncompatible elementMineralOlivineGeochemistryTrace elementMineralogyGeologyengineering.materialPeralkaline rockPartition coefficientGeochemistry and PetrologyengineeringLeuciteGeologyLithos
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Low-pressure fractionation of the Nyiragongo volcanic rocks, Virunga Province, D.R. Congo

2004

Abstract A new petrogenetic model for the Nyiragongo volcanics based on petrological and geochemical studies of a wide range of highly alkaline and silica-undersaturated fractionated rocks (Mg# 23–44) invokes low-pressure fractionation occurring mainly within the Nyiragongo volcanic edifice. The most primitive Nyiragongo rocks seem correspond to a pyroxene-nephelinitic melt which evolved to melilite nephelinite and melilitite by fractionation of leucite, together with varying amounts of nepheline. Leucite nephelinite, leucitite and leucite tephrite represent rock types originating partly by phenocryst accumulation. Mineral and bulk rock geochemistry of pyroxene nephelinites indicate an alre…

Basaltgeographygeography.geographical_feature_categoryNepheliniteGeochemistryMeliliteengineering.materialVolcanic rockIgneous rockGeophysicsGeochemistry and PetrologyTephriteengineeringPhenocrystLeuciteGeologyJournal of Volcanology and Geothermal Research
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Zirconolite-bearing ultra-potassic veins in a mantle-xenolith from Mt. Melbourne Volcanic Field, Victoria Land, Antarctica

1991

One mantle xenolith from a basanite host of the Mt. Melbourne Volcanic Field (Ross Sea Rift) is extraordinary in containing veins filled with leucite, plagioclase, clinopyroxene, nepheline, Mg-ilmenite, apatite, titaniferous mica, and the rare mineral zirconolite. These veins show extensive reaction with the dunitic or lherzolitic host (olivine+spinel+orthopyroxene+clinopyroxene). The reaction areas contain skeletal olivine and diopside crystals, plagioclase, phlogopite, aluminous spinel and ilmenite in a fine grained groundmass of aluminous spinel, clinopyroxene, olivine, plagioclase and interstitial leucite. The vein composition estimated from modal abundances and microprobe analyses is a…

PeridotiteOlivineGeochemistryengineering.materialBasanitechemistry.chemical_compoundGeophysicschemistryGeochemistry and PetrologyNephelineengineeringPlagioclaseXenolithMaficLeuciteGeologyContributions to Mineralogy and Petrology
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The analcime problem and its impact on the geochemistry of ultrapotassic rocks from Serbia

2004

AbstractTertiary ultrapotassic volcanic rocks from Serbia occasionally display low levels of K2O and K2O/ Na2O. In these rocks, analcime regularly appears as pseudomorphs after pre-existing leucite microphenocrysts. The process ofleucite transformation in Serbian ultrapotassic rocks is very thorough: fresh leucite survives only in ugandites from the Koritnik lava flows as well as in rare inclusions in Cpx. This paper focuses on the impact of ‘analcimization’ on the mineralogy and geochemistry ofthe Serbian ultrapotassic rocks, using the samples where leucite survived as a monitor for the process.Analcimization has had a great impact on the geochemistry of the rocks, but affects only a restr…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAnalcimeLavaGeochemistry550 - Earth sciencesengineering.material010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenVolcanic rockGeochemistry and PetrologyengineeringLithophileLoss on ignitionPseudomorphLeuciteGeology0105 earth and related environmental sciences
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