Modal mineralogy of carbonaceous chondrites by X‐ray diffraction and Mössbauer spectroscopy

By P. Bland, G. Cressey, O. Menzies. 2004

210 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Geophysics

View Paper: https://www.semanticscholar.org/paper/176a18f6a12422cd260110a9278590136d2cc51f

How researchers see this paper

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In Astronomy and Astrophysics

1. Edward A. Cloutis
2. Paul Mann
3. P. Schofield
4. A. King
5. K. Howard
6. W. Hartmann
7. M. Gaffey
8. S. Russell

In Geophysics

1. P. Schofield
2. Paul Mann
3. A. King
4. K. Howard
5. Edward A. Cloutis
6. M. Gaffey
7. S. Russell

Citations in the corpus

• Modal mineralogy of CI and CI-like chondrites by X-ray diffraction (2015, methodology): “We also note that dolomite was not observed in any of our Orgueil samples, nor those analysed by Bland et al. (2004).”
• Very low strengths of interplanetary meteoroids and small asteroids (2011, background): “The Tagish Lake material has a very high porosity of about 40% (Table 2) (Bland et al. 2004; Consolmagno and Britt 2004; Hildebrand et al. 2006), and its largest fragment constitutes only about 10)5 of its initial mass.”
• Spectral reflectance properties of carbonaceous chondrites: 1. CI chondrites (2012, background): “Modal mineralogy of the Orgueil CI1 carbonaceous chondrite (Bland et al., 2004).”