| Classification |
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| Species: | Ilmenite |
| Formula: | Fe2+TiO3 |
| Confirmation |
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| Validity: | Confirmed |
| Confirmation Methods: | Visually Identified, SEM-EDS
Raman Spectroscopy |
| Data |
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| Mineral Data: | Click here to view Ilmenite data |
| Locality Data: | Click here to view Rothorn, Geisspfad area, Binn, Goms, Valais, Switzerland |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1246255 |
| Long-form Identifier: | 1:3:1246255:9 |
| GUID (UUID V4): | 152bfdb9-052b-4ffa-be5f-d23753211c63 |
| Nearest other occurrences of Ilmenite |
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| 0.3km (0.2 miles) | âPunta della Rossa (Rothorn), Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
| 0.9km (0.5 miles) | âGeisspfad pass, Geisspfad area, Binn, Goms, Valais, Switzerland |
| 1.0km (0.6 miles) | âRossa asbestos mine (Alpe Rossa Mine), Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
| 2.7km (1.7 miles) | âMonte Cervandone area, Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
| 2.8km (1.7 miles) | âWanni glacier - Scherbadung area (Monte Cervandone), Binn, Goms, Valais, Switzerland |
| 3.0km (1.9 miles) | âGorb, LĂ€rchultini, Binn, Goms, Valais, Switzerland |
| 3.4km (2.1 miles) | âFlesch lake, Binn, Goms, Valais, Switzerland |
| 3.5km (2.2 miles) | âWanni glacier REE-mineralization, Wanni glacier - Scherbadung area (Monte Cervandone), Binn, Goms, Valais, Switzerland |
| 3.9km (2.4 miles) | âGischi glacier REE-mineralization, Gischi glacier (incl. Gischihorn), Binn, Goms, Valais, Switzerland |
| 5.2km (3.2 miles) | âPasso di Cornera REE-mineralization, Pizzo Cornera-Passo di Cornera area (Gischihorn-Chriegalppass area), Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
| References |
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| Reference Search (possible matching items) |
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 | Pelletier, Laure, MĂŒntener, Othmar, Kalt, Angelika, Vennemann, Torsten W., Belgya, TamĂĄs (2008) Emplacement of ultramafic rocks into the continental crust monitored by light and other trace elements: An example from the Geisspfad body (Swiss-Italian Alps) Chemical Geology, 255 (1) 143-159 doi:10.1016/j.chemgeo.2008.06.024 | Journal (article/letter/editorial) | | and other trace elements: An example from the Geisspfad body (Swiss-Italian Alps) Laure Pelletier a,â...NeuchĂątel, Emile Argand 11, CP158, 2009 NeuchĂątel, Switzerland Institute of Mineralogy and Geochemistry, University...University of Lausanne, Anthropole, 1015 Lausanne, Switzerland Institute of Isotopes, Hungarian Academy of Sciences...composition of whole rock samples and minerals of the Geisspfad ultramaïŹc complex (Swiss-Italian Alps). This complex...of northern Syros (Greece) and Pfulwe Pass (Switzerland). The Syros serpentinites have Li (0.9â2.8 ”g/g) |  | | Journal (article/letter/editorial) | | UniversitĂ€t Basel, Bernoullistrasse 30, CH-4005 Basel, Switzerland 3 Mineralogisches Institut, UniversitĂ€t Basel...Basel, Bernoullistrasse 30, CH-4005 Basel, Switzerland 4 Institute of Mineralogy, University of Freiburg...same tectonic unit about 25 km south of the study area called for a new attempt to characterize the P-T...Zermatt-Saas ophiolite east of Zermatt in the RothornâPfulwe region (Fig. 1) described in this paper...also visible chemical zoning in Omp, (b) enlarged area of a showing the details of pyroxene + amphibole |  | Parker, R. L., Stalder, H. A., de Quervain, F., Niggli, E., Graeser, St. (1973) Die Mineralfunde Der Schweiz (2nd ed.) Verlag Wepf & Co., Basel. | Book (edition) | | 3-85977-002-0 Copyright by Wepf & Co., Basel Printed in Switzerland Buchdruckcrci Birkhauser AG, Basel inTIWNRI...Luzern; Jos. (t) und Anton Imhof, Ried b. Brig und Binn; P. Indergand, Goschenen; A. und 0. Jochum, Poschiavo;... . . . . . . . . Fundgebiet 5 : Baltschiedertal-Goms-Urserental (H. A. Stalder) Fundortgruppen 5 a bis...Reul3- und Urseren tal, von Guttannen und aus dem Goms bearbeitet worden, teilweise schon seit Jahrhunderten...lt mit dcr Bc zeichnung ,Quartz byalin, Viesch, Valais. Don General Bonaparte, 1797>. Im Sommer 1967 ist |  | | Journal (article/letter/editorial) | | non-uniform peak conditions over the âTrockener Stegâ area and the maximum pressures conditions reported from...2 to 2.4 GPa for eclogites in the wider Zermatt area (Angiboust et al., 2009), from 2.5 to 3.0 GPa for...1983). 3. Field aspects and rock associations The area of Trockener Steg has been geologically mapped in...lake in the Eastern part of the mapped area (Fig. 2). The study area is a plateau at about 3000 m a.s.l....biotiteâschist (Fig. 5f). In the northern parts of the mapped area, typical associations of the ZermattâSaas ophiolites |
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