| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Mineralogical and chemical evolution of white micas and chlorites, from diagenesis to low-grade metamorphism; data from various size fractions of greywackes (Middle Cambrian, Morocco) |
|---|
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
|---|
| Authors | Wybrecht, E. | Author |
|---|
| Duplay, J. | Author |
| Piqué, A. | Author |
| Weber, F. | Author |
| Year | 1985 (June) | Volume | 49 |
|---|
| Issue | 352 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_49/49-352-401.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1985.049.352.11Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 3746 | Long-form Identifier | mindat:1:5:3746:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Wybrecht, E., Duplay, J., Piqué, A., Weber, F. (1985) Mineralogical and chemical evolution of white micas and chlorites, from diagenesis to low-grade metamorphism; data from various size fractions of greywackes (Middle Cambrian, Morocco) Mineralogical Magazine, 49 (352) 401-411 doi:10.1180/minmag.1985.049.352.11 |
|---|
| Plain Text | Wybrecht, E., Duplay, J., Piqué, A., Weber, F. (1985) Mineralogical and chemical evolution of white micas and chlorites, from diagenesis to low-grade metamorphism; data from various size fractions of greywackes (Middle Cambrian, Morocco) Mineralogical Magazine, 49 (352) 401-411 doi:10.1180/minmag.1985.049.352.11 |
|---|
| In | (1985, June) Mineralogical Magazine Vol. 49 (352) Mineralogical Society |
|---|
| Abstract/Notes | AbstractFour size fractions have been separated and studied in eight samples of Cambrian greywackes, ranging from non-metamorphic to low metamorphic grade. Chemical study included analyses of each size fraction and comparison with the whole rock analysis. Mineralogical study involved analyses of individual crystals using microprobe (> 6 µm) and STEM (< 6 µm). This showed that in each fraction, a progressive homogenization of the mineralogical composition occurred during the development of metamorphism; that chemical transfers especially of Fe-Mg and K-Na, occurred between fine and coarse fractions and that recrystallization in fine and coarse fractions was simultaneous. |
|---|
These are possibly similar items as determined by title/reference text matching only.
