Abstract
Chromium K-edge X-ray absorption spectra were collected to characterize Cr in forsterite (Mg2SiO4) as well as sulfides within the MAC 88136 EL3 chondrite to determine Cr valence and to see whether forsterite within this meteorite can be used as a Cr2+-silicate standard. Spectra were measured on several areas within a nearly pure 100 × 200 μm forsterite grain containing 0.13 wt% Cr. XANES findings indicate highly reduced Cr2+ species, with no clear evidence of Cr3+ or Cr6+. EXAFS data indicate an average 2.02 Å Cr-O nearest-neighbor distance, consistent with Cr-O distances found in square-planar Cr2+O4 sites observed in synthetic crystalline silicates, and an average 2.69 Å Cr-Si second-nearest neighbor distance, consistent with Cr2+ substituting for Mg2+ in the forsterite M(1) site. Nearest-neighbor Debye-Waller factor and coordination number parameters indicate Cr2+ is likely entering forsterite in disordered sites that are possible intermediates between M(1) and squareplanar Cr2+O4 configurations. Preliminary Cr XAS measurements on sulfides within this meteorite also indicate Cr2+ in CrS6 octahedra.
© 2014 by Walter de Gruyter GmbH & Co.
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Articles in the same Issue
- Shedding light on bone material
- Weddellite from renal stones: Structure refinement and dependence of crystal chemical features on H2O content
- Erionite and offretite from the Killdeer Mountains, Dunn County, North Dakota, U.S.A.
- Molecular water in nominally unhydrated carbonated hydroxylapatite: The key to a better understanding of bone mineral
- Precipitation and dissolution of chromite by hydrothermal solutions in the Oman ophiolite: New behavior of Cr and chromite
- Phase transitions and equation of state of forsterite to 90 GPa from single-crystal X-ray diffraction and molecular modeling
- Weathering of cobalt arsenides: Natural assemblages and calculated stability relations among secondary Ca-Mg-Co arsenates and carbonates
- Alburnite, Ag8GeTe2S4, a new mineral species from the Roşia Montana Au-Ag epithermal deposit, Apuseni Mountains, Romania
- Cathodoluminescence of alkali feldspars and radiation effects on the luminescent properties
- Thermochemistry of the alkali feldspars: Calorimetric study of the entropy relations in the low albite–low microcline series
- Thermal equation of state and spin transition of magnesiosiderite at high pressure and temperature
- Thermal diffusivities of MgSiO3 and Al-bearing MgSiO3 perovskites
- The sound velocity measurements of Fe3S
- PDF analysis of ferrihydrite: Critical assessment of the under-constrained akdalaite model
- Aluminum ion occupancy in the structure of synthetic saponites: Effect on crystallinity
- DFT investigation of structural and vibrational properties of type B and mixed A-B carbonated hydroxylapatite
- Chlorite topography and dissolution of the interlayer studied with atomic force microscopy
- The effect of XPS background removing method on the appraisal of Ti and Fe: The case of phlogopites and brookite
- Measurement of water contents in olivine using Raman spectroscopy
- Perbøeite-(Ce) and alnaperbøeite-(Ce), two new members of the epidote-törnebohmite polysomatic series: Chemistry, structure, dehydrogenation, and clue for a sodian epidote end-member
- Crystal structure and compressibility of lead dioxide up to 140 GPa
- A comparative analysis of the mechanical behavior of carbon dioxide and methane hydrate-bearing sediments
- Crystal structures and stabilities of cristobalite-helium phases at high pressures
- X-ray absorption characterization of Cr in forsterite within the MacAlpine Hills 88136 EL3 chondritic meteorite
- Monipite, MoNiP, a new phosphide mineral in a Ca-Al-rich inclusion from the Allende meteorite
- Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust
- Vanadio-oxy-dravite, NaV3(Al4Mg2)(Si6O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup
- XAS evidence for Ni sequestration by siderite in a lateritic Ni-deposit from New Caledonia
- Vladykinite, Na3Sr4(Fe2+Fe3+)Si8O24: A new complex sheet silicate from peralkaline rocks of the Murun complex, eastern Siberia, Russia
- New Mineral Names
- Memorial of James Burleigh Thompson, Jr., 1921–2011
- Book review: MANTLE CONVECTION FOR GEOLOGISTS by Geoffrey F. Davies
- Errata