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Pitchblende from
Le Fou, Les Mayens-de-Riddes, Riddes, Martigny, Valais, Switzerland


Classification
Species:Uraninite var: Pitchblende
Formula:UO2
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Pitchblende data
Locality Data:Click here to view Le Fou, Les Mayens-de-Riddes, Riddes, Martigny, Valais, Switzerland
Data Identifiers
Mindat Occurrence Record ID:559787
Long-form Identifier:1:3:559787:1
GUID (UUID V4):2f4dcd9d-d87e-4d04-9244-f72f9ebc946b
References
Stalder, H. A., Wagner, A., Graeser, S. and Stuker, P. (1998): "Mineralienlexikon der Schweiz", Wepf (Basel), p. 419.
Reference Search (possible matching items)
Dahlkamp, Franz J. (2016) Uranium Deposits of the World - Europe. Springer Berlin Heidelberg. doi:10.1007/978-3-540-78554-5
Book
Ball (UK), I. Benkovics (Hungary), F. Bianconi (Switzerland), J. R. Blaise (Spain), A. V. Boytsov (Russia).... . . . . . . . . . . 16.2 Lower Río Tajo-Cabeza De Araya Region, Western Cáceres Province . 16.2.1 Ceclavín-Acehuche... . . . . . . . . . . . . . 16.2.3 Central Cabeza De Araya Area . . . . . . . . . . . . . . . . . . ....Province . . . . . . . . . . . 16.4 La Jara-Sierra De Altamira Region, Northeastern Cáceres Province ....591 592 598 602 605 606 609 610 Chapter 18 Switzerland . . . . . . . . . . . . . . . . . . . . . .
(2013, July) Noble Gas Constraints on the Origin and Evolution of Earth’s Volatiles. Geochemical Perspectives Vol. 2 (2) European Association of Geochemistry
Journal (issue)
at the Institut de Physique du Globe de Paris. Manuel’s research focuses on the Earth’s origin and how...in 2006 and member of the Institut Universitaire de France in 2007. Volume 2, number 2 | July 2013 ...and acting like Jean-Paul Belmondo (in Pierrot le Fou) whilst learning to bake bread in the stone-oven...(Palmieri, 1881). Ramsay observed helium in pitchblende minerals in 1895. This helium is mainly the radiogenic...Allègre, 1980, 1983a, 1987; Cohen and O’Nions, 1982; De Paolo and Wasserburg, 1979; Dupré and Allègre, 1980;
 
Mineral and/or Locality  
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