Classification |
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Species: | Chromite |
Formula: | Fe2+Cr23+O4 |
Confirmation |
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Validity: | Believed Valid |
Data |
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Mineral Data: | Click here to view Chromite data |
Locality Data: | Click here to view Serpentine Saddle, Queenstown-Lakes District, Otago Region, New Zealand |
Data Identifiers |
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Mindat Occurrence Record ID: | 93638 |
Long-form Identifier: | 1:3:93638:9 |
GUID (UUID V4): | b21dee61-bd29-4450-b478-005debae2a27 |
Nearest other occurrences of Chromite |
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29.9km (18.6 miles) | ⓘAnita Bay, Milford Sound, Fiordland National Park, Southland District, Southland Region, New Zealand |
39.6km (24.6 miles) | ⓘRed Mountain (Big Red Hill), Westland District, West Coast Region, New Zealand |
50.8km (31.6 miles) | ⓘJerry River, Westland District, West Coast Region, New Zealand |
52.7km (32.8 miles) | ⓘGorge River, Westland District, West Coast Region, New Zealand |
References |
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Reference Search (possible matching items) |
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| Tarling, Matthew S., Smith, Steven A. F., Scott, James M., Rooney, Jeremy S., Viti, Cecilia, Gordon, Keith C. (2019) The internal structure and composition of a plate-boundary-scale serpentinite shear zone: the Livingstone Fault, New Zealand. Solid Earth, 10 (4). 1025-1047 doi:10.5194/se-10-1025-2019 | Journal (article/letter/editorial) | serpentinite shear zone: the Livingstone Fault, New Zealand Matthew S. Tarling1 , Steven A. F. Smith1 , James...University of Otago, 360 Leith Street, 9016 Dunedin, New Zealand of Chemistry, University of Otago, Union Place...Place West, 9016 Dunedin, New Zealand 3 Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente...tectonic settings. The Livingstone Fault in New Zealand is a terrane-bounding structure that separates...µm) fibrous chrysotile and lizardite–polygonal serpentine, but infrequent (< 1 % vol) lenticular relicts |
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