Abstract
Detailed electron- and ion-microprobe analysis of diopsides extracted from a block of marble collected in the Mt. Marcy anorthosite massif (Adirondack Highlands, New York) shows that single crystals have preserved Al-Si zoning features from early contact metamorphism later modified by regional metamorphism. Diopsides show Al and Si complementary zoning from core to rim; average Al concentration in rims is constant (0.11 pfu), but values in the cores vary with crystals from 0.06 to 0.14 pfu. A δ18O profile measured with the ion microprobe shows no zoning. Modeling of the Al-diffusion profiles affected by regional metamorphism of the Grenville orogeny shows that original Al zoning was sharp and corresponds to a rapid change of crystal-growth conditions during early contact metamorphism: (1) diopside cores crystallized with variable Al contents due to restricted fluid circulation or differing sedimentary composition, (2) then pervasive fluid infiltration crystallized the homogeneous rim of diopside, and (3) core to rim Al zoning was later smoothed by granulite-facies metamorphism. Homogeneity of δ18O in core and mantle (near rim) of diopsides suggests that the crystals were isotopically homogeneous prior to and during regional metamorphism. Values of Al-Si diffusion coefficient deduced from modeling are in agreement with low-temperature extrapolation of experimental data.
© 2015 by Walter de Gruyter Berlin/Boston
Articles in the same Issue
- New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and δ18O profiles
- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
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- In-situ measurement of dissolution of anorthite in Na-Cl-OH solutions at 22 °C using phase-shift interferometry
- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
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- An infrared spectroscopic study of the OH stretching frequencies of talc and 10-Å phase to 10 GPa
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- Single-crystal elasticity of zoisite Ca2Al3Si3O12(OH) by Brillouin scattering
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Articles in the same Issue
- New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and δ18O profiles
- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
- Magnetic excitations and heat capacity of fayalite, Fe2SiO4
- The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
- In-situ measurement of dissolution of anorthite in Na-Cl-OH solutions at 22 °C using phase-shift interferometry
- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
- Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by fluid-cell micro-Raman spectroscopy
- An infrared spectroscopic study of the OH stretching frequencies of talc and 10-Å phase to 10 GPa
- Co2+-Cu2+ substitution in bieberite solid-solution series, (Co1-xCux)SO4·7H2O, 0.00 ≤ x ≤ 0.46: Synthesis, single-crystal structure analysis, and optical spectroscopy
- Clinoenstatite exsolution in diopsidic augite of Dabieshan: Garnet peridotite from depth of 300 km
- Heat-pulse calorimetry measurements on natural chlorite-group minerals
- Low-temperature behavior of NaGaSi2O6
- Single-crystal elasticity of zoisite Ca2Al3Si3O12(OH) by Brillouin scattering
- The effect of valence state and site geometry on Ti L3,2 and O K electron energy-loss spectra of TixOy phases
- Characterization of defects and the local structure in natural and synthetic alunite (K, Na, H3O)Al3(SO4)2(OH)6 by multi-nuclear solid-state NMR spectroscopy
- Using a mineral lifetime diagram to evaluate the persistence of olivine on Mars
- Complexity in 15- and 30-sectors polygonal serpentine: Longitudinal sections, intrasector stacking faults and XRPD satellites
- Light-induced alteration of arsenic sulfides: A new product with an orthorhombic crystal structure
- Transmission electron microscopy study of magnetites in a freshwater population of magnetotactic bacteria
- Anomalous behavior at the I2/a to Imab phase transition in SiO2-moganite: An analysis using hard-mode Raman spectroscopy
- The system Ag-Au-Se: Phase relations below 405 K and determination of standard thermodynamic properties of selenides by solid-state galvanic cell technique
- Rhombohedral (9R) and hexagonal (6H) perovskites in barium silicates under high pressure
- Structural effects of pressure on monoclinic chlorite: A single-crystal study
- Neptunium incorporation in sodium-substituted metaschoepite
- The effect of H2O on olivine crystallization in MORB: Experimental calibration at 200 MPa
- Symmetry and crystal structure of biaxial elbaite-liddicoatite tourmaline from the Transbaikalia region, Russia
- Letter: Onion morphology and microstructure of polyhedral serpentine
- Letter: Ion microprobe analysis of (231Pa)/(235U) and an appraisal of protactinium partitioning in igneous zircon
- Letter: Structural investigation of Mg local environments in silicate glasses by ultra-high field 25Mg 3QMAS NMR spectroscopy
- Letter: Entropies of mixing and subsolidus phase relations of forsteritefayalite (Mg2SiO4Fe2SiO4) solid solution