Textural properties of iron-rich phases in H ordinary chondrites and quantitative links to the degree of thermal metamorphism

· by · in , , ,

J. Guignard, M.J. Toplis

Geochimica et Cosmochimica Acta
available online 13 November 2014

LINK

Related posts (automatically generated):

  1. Chemical and oxygen isotopic properties of ordinary chondrites (H5, L6) from Oman: Signs of isotopic equilibrium during thermal metamorphism.
  2. Metal phases in ordinary chondrites: Magnetic hysteresis properties and implications for thermal history
  3. Plagioclase alteration and equilibration in ordinary chondrites: Metasomatism during thermal metamorphism
  4. Evolution of hematite and/or magnetite iron phases with thermal heating in ordinary chondrites: A generic characteristic
  5. Response of silicate chemical composition variation on thermal metamorphism of ordinary chondrites and classification of petrologic types: the case of L chondrites from Grove Mountains, Antarctica
  6. Primordial, thermal, and shock features of ordinary chondrites: Emulating bulk X‐ray diffraction using in‐plane rotation of polished thin sections
  7. Relationships among physical properties as indicators of high temperature deformation or post-shock thermal annealing in ordinary chondrites
  8. Restriction of parent body heating by metal-troilite melting: Thermal models for the ordinary chondrites
  9. Hf-W chronology of ordinary chondrites
  10. The density, porosity and pore morphology of fall and find ordinary chondrites
Tags: , , , ,