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) | ⓘPunta della Rossa (Rothorn), Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
0.9km (0.5 miles) | ⓘGeisspfad pass, Geisspfad area, Binn, Goms, Valais, Switzerland |
1.0km (0.6 miles) | ⓘRossa asbestos mine (Alpe Rossa Mine), Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
2.7km (1.7 miles) | ⓘMonte Cervandone area, Devero Alp, Baceno, Verbano-Cusio-Ossola Province, Piedmont, Italy |
2.8km (1.7 miles) | ⓘWanni glacier - Scherbadung area (Monte Cervandone), Binn, Goms, Valais, Switzerland |
3.0km (1.9 miles) | ⓘGorb, Lärchultini, Binn, Goms, Valais, Switzerland |
3.4km (2.1 miles) | ⓘFlesch lake, Binn, Goms, Valais, Switzerland |
3.5km (2.2 miles) | ⓘWanni glacier REE-mineralization, Wanni glacier - Scherbadung area (Monte Cervandone), Binn, Goms, Valais, Switzerland |
3.9km (2.4 miles) | ⓘGischi glacier REE-mineralization, Gischi glacier (incl. Gischihorn), Binn, Goms, Valais, Switzerland |
5.2km (3.2 miles) | ⓘPasso 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, Müntener, Othmar, Kalt, Angelika, Vennemann, Torsten W., Belgya, Tamás (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,⁎...Neuchâtel, Emile Argand 11, CP158, 2009 Neuchâtel, 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 ultramafic complex (Swiss-Italian Alps). This complex...of northern Syros (Greece) and Pfulwe Pass (Switzerland). The Syros serpentinites have Li (0.9–2.8 µg/g) | | | Journal (article/letter/editorial) | Universität Basel, Bernoullistrasse 30, CH-4005 Basel, Switzerland 3 Mineralogisches Institut, Universität 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 Rothorn–Pfulwe 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 “Trockener Steg” 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....biotite–schist (Fig. 5f). In the northern parts of the mapped area, typical associations of the Zermatt–Saas ophiolites |
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