Binns, R. A. (1962) Metamorphic pyroxenes from the Broken Hill district, New South Wales. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (259) 320-338 doi:10.1180/minmag.1962.033.259.06
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Metamorphic pyroxenes from the Broken Hill district, New South Wales | ||
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society | ||
| Authors | Binns, R. A. | Author | |
| Year | 1962 (December) | Volume | 33 |
| Issue | 259 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_33/33-259-320.pdf+ | ||
| DOI | doi:10.1180/minmag.1962.033.259.06Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 5704 | Long-form Identifier | mindat:1:5:5704:6 |
| GUID | 0 | ||
| Full Reference | Binns, R. A. (1962) Metamorphic pyroxenes from the Broken Hill district, New South Wales. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (259) 320-338 doi:10.1180/minmag.1962.033.259.06 | ||
| Plain Text | Binns, R. A. (1962) Metamorphic pyroxenes from the Broken Hill district, New South Wales. Mineralogical Magazine and Journal of the Mineralogical Society, 33 (259) 320-338 doi:10.1180/minmag.1962.033.259.06 | ||
| In | (1962) Mineralogical Magazine Vol. 33 (259) Mineralogical Society | ||
| Abstract/Notes | SummaryThe Archean rocks of the Barrier Ranges, New South Wales, show zones of progressive regional metamorphism of which the highest is characterized by orthopyroxene-bearing basic granulites. Within this zone, further increase in metamorphic grade results in a detectable change in distribution of ferrous iron and magnesium between coexisting orthopyroxene and clinopyroxene, the latter becoming relatively richer in iron. Mutual solid solution between the two pyroxene phases also appears to increase. The value of coexisting pyroxenes as indicators of metamorphic grade is thus established. There are some points of disagreement between the Broken Hill results and previously advanced theories of cation distribution in pyroxenes. | ||
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