REFERENCES
Zinc- and manganese-bearing chromites and associated grossular from Zimbabwe ZINC-RICH chromites have been reported from relatively few localities, and some of these have been discredited in the light of modern analytical techniques. Moore (I977), for example, showed by detailed electron microprobe...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.8982 http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.629.8982 2023-05-15T16:34:08+02:00 REFERENCES C. M. Jantzen The Pennsylvania State University CiteSeerX Archives 1979 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.8982 http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.8982 http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf text 1979 ftciteseerx 2016-01-08T15:24:01Z Zinc- and manganese-bearing chromites and associated grossular from Zimbabwe ZINC-RICH chromites have been reported from relatively few localities, and some of these have been discredited in the light of modern analytical techniques. Moore (I977), for example, showed by detailed electron microprobe analysis of Donath's original samples that the supposed zinc-rich (up to 2.6 ~o) chromites from the Helgeland area, Norway (Donath, i93i) contain only up to o.3~o ZnO. Moore suggested, therefore, that the Outokumpu deposit of Finland might be a unique location for zinc-rich chromites, and emphasized that a very unusual geochemical environment must have been necessary for their formation. Text Helgeland Unknown Helgeland Norway |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| description |
Zinc- and manganese-bearing chromites and associated grossular from Zimbabwe ZINC-RICH chromites have been reported from relatively few localities, and some of these have been discredited in the light of modern analytical techniques. Moore (I977), for example, showed by detailed electron microprobe analysis of Donath's original samples that the supposed zinc-rich (up to 2.6 ~o) chromites from the Helgeland area, Norway (Donath, i93i) contain only up to o.3~o ZnO. Moore suggested, therefore, that the Outokumpu deposit of Finland might be a unique location for zinc-rich chromites, and emphasized that a very unusual geochemical environment must have been necessary for their formation. |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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C. M. Jantzen |
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C. M. Jantzen REFERENCES |
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C. M. Jantzen |
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C. M. Jantzen |
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REFERENCES |
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REFERENCES |
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REFERENCES |
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REFERENCES |
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REFERENCES |
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references |
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1979 |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.8982 http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf |
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Helgeland Norway |
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Helgeland Norway |
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Helgeland |
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Helgeland |
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http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.629.8982 http://www.minersoc.org/pages/Archive-MM/Volume_43/43-330-811.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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