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Coombs, D. S., Zhao, G., Peacor, D. R. (2000) Manganoan berthierine, Meyers Pass, New Zealand: occurrence in the prehnite-pumpellyite facies. Mineralogical Magazine, 64 (6) 1037-1046 doi:10.1180/002646100550038

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Reference TypeJournal (article/letter/editorial)
TitleManganoan berthierine, Meyers Pass, New Zealand: occurrence in the prehnite-pumpellyite facies
JournalMineralogical Magazine
AuthorsCoombs, D. S.Author
Zhao, G.Author
Peacor, D. R.Author
Year2000 (December)Volume64
Issue6
PublisherMineralogical Society
DOIdoi:10.1180/002646100550038Search in ResearchGate
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Mindat Ref. ID243239Long-form Identifiermindat:1:5:243239:1
GUID0
Full ReferenceCoombs, D. S., Zhao, G., Peacor, D. R. (2000) Manganoan berthierine, Meyers Pass, New Zealand: occurrence in the prehnite-pumpellyite facies. Mineralogical Magazine, 64 (6) 1037-1046 doi:10.1180/002646100550038
Plain TextCoombs, D. S., Zhao, G., Peacor, D. R. (2000) Manganoan berthierine, Meyers Pass, New Zealand: occurrence in the prehnite-pumpellyite facies. Mineralogical Magazine, 64 (6) 1037-1046 doi:10.1180/002646100550038
Abstract/NotesAbstractManganoan berthierine, sometimes only a few layers thick, is preserved interlayered with manganoan chlorite (chamosite) in small recrystallized patches in cherty metapelagites matamorphosed in the prehnite–pumpellyite facies at Meyers Pass, Torlesse Terrane, South Canterbury, New Zealand. The Mn occupies 11–12% of the octahedral sites, making this the most Mn–rich berthierine reported so far. The ratio (Fe+Mn)(Fe+Mn+Mg), 0.67–0.70, is at the lower end of those of previously reported occurrences, making these amongst the most Mg-rich berthierines known. Manganoan berthierine and interlayered manganoan chlorite also make up ~11–13% of the cryptocrystalline groundmass in which the berthierine is believed to have crystallized under early diagenetic conditions near a deep-ocean–sediment interface. The occurrence of berthierine in the recrystallized patches lends support to the possibility of a stability field at the temperature of prehnite-pumpellyite facies recrystallization in association with chlorite of similar but not identical composition.


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