Article
Licensed
Unlicensed
Requires Authentication
Reply to stoppa et.al. 2005. Wollastonite- anorthite- gehlenite-, and fassaite-bearing rocks: Igneous petrological oddity or paralavas?
Published/Copyright:
March 28, 2015
Abstract
We briefly review the petrological and geochemical features, and physical characteristics, of the Colle Fabbri and Ricetto rocks to discuss their possible paramagmatic origin, i.e., derived from complete melting, after devolatilization, of marly protoliths, without any orthomagmatic, ultimately mantle-derived, chemical or thermal input. Contrary to the various comments that have been made, the overall mineralogical, petrological, and geochemical data provided in the literature well agree with this finding.
Accepted: 2005-9-8
Published Online: 2015-3-28
Published in Print: 2005-11-1
© 2015 by Walter de Gruyter Berlin/Boston
You are currently not able to access this content.
You are currently not able to access this content.
Articles in the same Issue
- Electronic article. Getting the inside story: using computed X-ray tomography to study inclusion trails in garnet porphyroblasts
- Structure of framboidal pyrite: An electron backscatter diffraction study
- The mineralogical microstructure of shells: PART 2.1 The iridescence colors of abalone shells
- Electron probe (Ultrachron) microchronometry of metamorphic monazite: Unraveling the timing of polyphase thermotectonism in the easternmost Wyoming Craton (Black Hills, South Dakota)
- New mineral occurrences and mineralization processes: Wuda coal-fire gas vents of Inner Mongolia
- Synchrotron micro-X-ray fluorescence analysis of natural diamonds: First steps in identification of mineral inclusions in situ
- Speciation and distribution of sulfur in a mollusk shell as revealed by in situ maps using X-ray absorption near-edge structure (XANES) spectroscopy at the S K-edge
- Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420 °C and 1 GPa with controlled oxygen partial pressure
- Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions
- Etch pit coalescence, surface area, and overall mineral dissolution rates
- Crystal chemistry of the elbaite-schorl series
- Morphology of nanomagnetite crystals: Implications for formation conditions
- Fragmentation phenomena in populations of magmatic crystals
- Kinetics of Fe2+-Mg order-disorder in P21/c pigeonite
- First-principles studies on the elastic constants of a 1:1 layered kaolinite mineral
- Quantum mechanical calculations of trans-vacant and cis-vacant polymorphism in dioctahedral 2:1 phyllosilicates
- The stability and Raman spectra of ikaite, CaCO3·6H2O, at high pressure and temperature
- Model pyroxenes III: Volume of C2/c pyroxenes at mantle P, T, and x
- The kinetics and mechanisms of goethite and hematite crystallization under alkaline conditions, and in the presence of phosphate
- High-resolution 17O MAS NMR spectroscopy of forsterite (α-Mg2SiO4), wadsleyite (β-Mg2SiO4), and ringwoodite (γ-Mg2SiO4)
- Comparative study of equilibrated and unequilibrated eucrites: Subsolidus thermal histories of Haraiya and Pasamonte
- Origin and internal evolution of the Li-F-Be-B-P-bearing Pinilla de Fermoselle pegmatite (Central Iberian Zone, Zamora, Spain)
- Single-crystal X-ray diffraction of spinels from the San Carlos Volcanic Field, Arizona: Spinel as a geothermometer
- Letter. Direct observations of pseudomorphism: compositional and textural evolution at a fluid- solid interface
- Letter. Carbon oxides in cordierite channels: Determination of CO2 isotopic species and CO by single crystal IR spectroscopy
- Comment on Melluso et al. (2003) Reported data and interpretation of some wollastonite- and melilite-bearing rocks from the Central Apennines of Italy
- Reply to stoppa et.al. 2005. Wollastonite- anorthite- gehlenite-, and fassaite-bearing rocks: Igneous petrological oddity or paralavas?
- Comment on Melluso et.al. (2003). The Ricetto and Colle Fabbri wollastonite and melilite-bearing rocks of the central Apennines, Italy
- Reply to Capitanio 2005. Mineralogic and bulk rock composition of Italian wollastonite- and melilite-bearing paralava and clinker: Further evidence of their pyrometamorphic nature
Articles in the same Issue
- Electronic article. Getting the inside story: using computed X-ray tomography to study inclusion trails in garnet porphyroblasts
- Structure of framboidal pyrite: An electron backscatter diffraction study
- The mineralogical microstructure of shells: PART 2.1 The iridescence colors of abalone shells
- Electron probe (Ultrachron) microchronometry of metamorphic monazite: Unraveling the timing of polyphase thermotectonism in the easternmost Wyoming Craton (Black Hills, South Dakota)
- New mineral occurrences and mineralization processes: Wuda coal-fire gas vents of Inner Mongolia
- Synchrotron micro-X-ray fluorescence analysis of natural diamonds: First steps in identification of mineral inclusions in situ
- Speciation and distribution of sulfur in a mollusk shell as revealed by in situ maps using X-ray absorption near-edge structure (XANES) spectroscopy at the S K-edge
- Experimental study on diamond dissolution in kimberlitic and lamproitic melts at 1300-1420 °C and 1 GPa with controlled oxygen partial pressure
- Validation of LA-ICP-MS fluid inclusion analysis with synthetic fluid inclusions
- Etch pit coalescence, surface area, and overall mineral dissolution rates
- Crystal chemistry of the elbaite-schorl series
- Morphology of nanomagnetite crystals: Implications for formation conditions
- Fragmentation phenomena in populations of magmatic crystals
- Kinetics of Fe2+-Mg order-disorder in P21/c pigeonite
- First-principles studies on the elastic constants of a 1:1 layered kaolinite mineral
- Quantum mechanical calculations of trans-vacant and cis-vacant polymorphism in dioctahedral 2:1 phyllosilicates
- The stability and Raman spectra of ikaite, CaCO3·6H2O, at high pressure and temperature
- Model pyroxenes III: Volume of C2/c pyroxenes at mantle P, T, and x
- The kinetics and mechanisms of goethite and hematite crystallization under alkaline conditions, and in the presence of phosphate
- High-resolution 17O MAS NMR spectroscopy of forsterite (α-Mg2SiO4), wadsleyite (β-Mg2SiO4), and ringwoodite (γ-Mg2SiO4)
- Comparative study of equilibrated and unequilibrated eucrites: Subsolidus thermal histories of Haraiya and Pasamonte
- Origin and internal evolution of the Li-F-Be-B-P-bearing Pinilla de Fermoselle pegmatite (Central Iberian Zone, Zamora, Spain)
- Single-crystal X-ray diffraction of spinels from the San Carlos Volcanic Field, Arizona: Spinel as a geothermometer
- Letter. Direct observations of pseudomorphism: compositional and textural evolution at a fluid- solid interface
- Letter. Carbon oxides in cordierite channels: Determination of CO2 isotopic species and CO by single crystal IR spectroscopy
- Comment on Melluso et al. (2003) Reported data and interpretation of some wollastonite- and melilite-bearing rocks from the Central Apennines of Italy
- Reply to stoppa et.al. 2005. Wollastonite- anorthite- gehlenite-, and fassaite-bearing rocks: Igneous petrological oddity or paralavas?
- Comment on Melluso et.al. (2003). The Ricetto and Colle Fabbri wollastonite and melilite-bearing rocks of the central Apennines, Italy
- Reply to Capitanio 2005. Mineralogic and bulk rock composition of Italian wollastonite- and melilite-bearing paralava and clinker: Further evidence of their pyrometamorphic nature