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Fayalite from
Smålands Taberg, Månsarp, Jönköping, Jönköping County, Sweden


Locality type:Mine
Classification
Species:Fayalite
Formula:Fe22+SiO4
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Fayalite data
Locality Data:Click here to view Smålands Taberg, Månsarp, Jönköping, Jönköping County, Sweden
Data Identifiers
Mindat Occurrence Record ID:272954
Long-form Identifier:1:3:272954:1
GUID (UUID V4):54f61b13-3a88-4d26-84f2-06a67931f230
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
Oxygen fugacity is normalized to that of the fayalite–magnetite–quartz (FMQ) buffer, where log fO2 (ΔFMQ)...expressed in terms of log units relative to the fayalite–magnetite–quartz (FMQ) buffer. If Vmagma is fixed...et al., 1998). The ∼ 1.2 Ga Smålands Taberg Fe–Ti oxide deposit (Sweden) is contemporaneous with a widespread...example from a Fe–Ti mineralization at Smålands Taberg, southern Sweden. Chemical Geology 224, 201–211. Lee...Xinjie V–Ti–Magnetite Ore District in the Miyi county, Sichuan Province, pp. 15–35. in Chinese. Qi, L
Journal (article/letter/editorial)
531 ◦ C and from +0.1 to −11.1 (relative to the fayalite-magnetite-quartz (FMQ) buffer), and do not suggest...temperature (◦ C) versus ∆log f O2 (relative to the fayalite–magnetite–quartz (FMQ) buffer) showing the equilibrium...genetical aspects of the Smålands Taberg Fe-Ti-V ore, Protogine Zone of southern Sweden. GFF 2000, 122, 351–358
Book
1998–2000. Per Enghag Stortorget 17 70211 Örebro Sweden All books published by Wiley-VCH are carefully...Forgeable 189 Steel Manufacture from Wrought Iron 190 Sweden and England – Cooperation and Competition 191 Iron...Iron Ores With and Without Phosphorus 191 England–Sweden in Cooperation 192 The Puddling Process – An English...Brittleness 538 Del Rio’s Lost Element Appears in Sweden 538 A Scientific Triangle Drama 540 Vanadium Metal...Dr. Sven Arvidsson at The Geological Survey of Sweden. They have commented on the manuscript, critically
 
Mineral and/or Locality  
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