| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Petrology and geothermometry of the Little Michiru Complex, Malawi |
|---|
| Journal | Mineralogical Magazine | ISSN | 0026-461X |
|---|
| Authors | Morel, S. W. | Author |
|---|
| Year | 1989 (June) | Volume | 53 |
|---|
| Issue | 371 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_53/53-371-285.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1989.053.371.02Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 1504 | Long-form Identifier | mindat:1:5:1504:6 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Morel, S. W. (1989) Petrology and geothermometry of the Little Michiru Complex, Malawi. Mineralogical Magazine, 53 (371) 285-291 doi:10.1180/minmag.1989.053.371.02 |
|---|
| Plain Text | Morel, S. W. (1989) Petrology and geothermometry of the Little Michiru Complex, Malawi. Mineralogical Magazine, 53 (371) 285-291 doi:10.1180/minmag.1989.053.371.02 |
|---|
| In | (1989, June) Mineralogical Magazine Vol. 53 (371) Mineralogical Society |
|---|
| Abstract/Notes | AbstractThe Little Michiru complex is a composite intrusion of pyroxenite and pyroxene syenite which is located at the boundary between amphibolite and granulite facies gneisses in the Shire rift valley. Pyroxene and feldspar chemistry shows that the intrusion consolidated from two magmatic fractions, one a pyroxenite cumulate that equilibrated at 870–1000 °C, the other a partly anatectic pyroxene syenite magma which metasomatized the surrounding gneisses during granulite-facies metamorphism and equilibrated at a temperature of 730–830 °C at 7 kbar. |
|---|
These are possibly similar items as determined by title/reference text matching only.
