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Chenhall, B. E. (1976) Chemical variation of almandine and biotite with progressive regional metamorphism of the Willyama complex, broken hill, New South Wales. Journal of the Geological Society of Australia, 23 (3) 235-242 doi:10.1080/00167617608728937

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Reference TypeJournal (article/letter/editorial)
TitleChemical variation of almandine and biotite with progressive regional metamorphism of the Willyama complex, broken hill, New South Wales
JournalJournal of the Geological Society of Australia
AuthorsChenhall, B. E.Author
Year1976 (September)Volume23
Issue3
PublisherInforma UK Limited
DOIdoi:10.1080/00167617608728937Search in ResearchGate
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Mindat Ref. ID565582Long-form Identifiermindat:1:5:565582:7
GUID0
Full ReferenceChenhall, B. E. (1976) Chemical variation of almandine and biotite with progressive regional metamorphism of the Willyama complex, broken hill, New South Wales. Journal of the Geological Society of Australia, 23 (3) 235-242 doi:10.1080/00167617608728937
Plain TextChenhall, B. E. (1976) Chemical variation of almandine and biotite with progressive regional metamorphism of the Willyama complex, broken hill, New South Wales. Journal of the Geological Society of Australia, 23 (3) 235-242 doi:10.1080/00167617608728937
In(1976, September) Journal of the Geological Society of Australia Vol. 23 (3) Informa UK Limited

See Also

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Binns, R. A. (1964) Zones of progressive regional metamorphism in the Willyama complex, broken hill district, New South Wales. Journal of the Geological Society of Australia, 11 (2) 283-330 doi:10.1080/00167616408728577
(1987) The Geochemistry of the Lower Proterozoic Willyama Complex Volcanics, Broken Hill Block, New South Wales. Special Publication, 33. Geological Society of London. 395-408 doi:10.1144/gsl.sp.1987.033.01.27
Willis, I. L., Brown, R. E., Stroud, W. J., Stevens, B. P. J. (1983) The early Proterozoic Willyama supergroup: Stratigraphic subdivision and interpretation of high to low‐grade metamorphic rocks in the Broken Hill Block, New South Wales. Journal of the Geological Society of Australia, 30 (1) 195-224 doi:10.1080/00167618308729249
Tuckwell, K. D. (1978) Stratigraphic subdivision and correlation of the upper part of the Willyama Complex, New South Wales. Journal of the Geological Society of Australia, 25 (5) 295-308 doi:10.1080/00167617808729037
Mason, Brian (1973) Manganese silicate minerals from broken hill, New South Wales. Journal of the Geological Society of Australia, 20 (4) 397-404 doi:10.1080/00167617308728825
Birch, W. D. (1983) Zincian dolomite from broken hill, New South Wales. Journal of the Geological Society of Australia, 30 (1) 85-87 doi:10.1080/00167618308729238
Corbett, G.J., Phillips, G.N. (1981) Regional retrograde metamorphism of a high grade terrain: the Willyama Complex, Broken Hill, Australia. Lithos, 14 (1) 59-73 doi:10.1016/0024-4937(81)90037-2
Williams, P. F. (1967) Structural analysis of the little Broken Hill area, New South Wales. Journal of the Geological Society of Australia, 14 (2) 317-331 doi:10.1080/00167616708728669
Vernon, R. H., Ransom, D. M. (1971) Retrograde Schists of the Amphibolite Facies at broken hill, New South Wales. Journal of the Geological Society of Australia, 18 (3) 267-277 doi:10.1080/00167617108728766
Manganese silicate minerals from Broken Hill, New South Wales By Brian Mason: Journal of the Geological Society of Australia Volume 20, Issue 4, 1973
Binns, R. A. (1965) The mineralogy of metamorphosed basic rocks from the Willyama Complex, Broken Hill district, New South Wales. Part I. Hornblendes. Mineralogical Magazine and Journal of the Mineralogical Society, 35 (270) 306-326 doi:10.1180/minmag.1965.035.270.05
 
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