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Cuneo Italy

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Journal Article
Published: 01 January 1960
Bulletin de la Société Géologique de France (1960) S7-II (7): 951–960.
...Andre Guillaume Abstract The autochthonous formations of the Argentera massif form the base of the Col de Tende unit in Cuneo province, Italy. The Cretaceous beds of the unit are well developed to the northwest, but are absent to the southeast as a result of pre-Lutetian erosion. Toward...
Journal Article
Published: 07 April 2022
Mineralogical Magazine (2022) 86 (3): 447–458.
... of the arsenbrackebuschite group in the brackebuschite supergroup, discovered in Fe–Mn ore in metaquartzites of the abandoned mine of Valletta, Canosio, Val Maira, Cuneo Province, Piedmont, Italy. They occur as red–brown and orange brown, respectively, as subhedral crystals (< 0.5 mm) in thin masses, associated...
FIGURES
First thumbnail for: As-bearing new mineral species from Valletta mine,...
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Journal Article
Published: 01 January 1961
Bulletin de la Société Géologique de France (1961) S7-III (1): 50–58.
...Claude Lorenz Abstract The Bagnasco basin in Cuneo province, Italy, is filled largely by coarse detrital sediments overlain, in the vicinity of Bagnasco only, by a marly formation preserved in a small graben. These sediments are continental in character and poor in fossils; they can be attributed...
Journal Article
Published: 01 January 1994
Italian Journal of Geosciences (1994) 113 (3): 501–520.
...Alberto Lualdi Abstract Stratigraphy and sedimentology of the Rio di Nava Limestones (Bathonian) are here investigated. The Formation belongs to the Ligurian Brianconnais domain outcropping in the high Tanaro and Corsaglia valleys (Cuneo province, NW Italy). All the better out-cropping sequences...
Journal Article
Published: 28 November 2022
Mineralogical Magazine (2023) 87 (2): 204–217.
... of the Montaldo di Mondovì mine, Corsaglia Valley, Cuneo Province, Piedmont, Italy. It occurs as small and rare black crystals and aggregates hosted by a matrix of quartz, associated with calcite and berzeliite/manganberzeliite. It has been also found in the Valletta mine near Canosio, Maira Valley, Cuneo...
FIGURES
First thumbnail for: Piccoliite, NaCaMn 3+ 2 (AsO 4 ) 2 O(OH), a new ar...
Second thumbnail for: Piccoliite, NaCaMn 3+ 2 (AsO 4 ) 2 O(OH), a new ar...
Third thumbnail for: Piccoliite, NaCaMn 3+ 2 (AsO 4 ) 2 O(OH), a new ar...
Journal Article
Published: 01 January 1963
Bulletin de la Société Géologique de France (1963) S7-V (5): 657–661.
.... Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States 1963 Bagnasco Cenozoic Chattian Europe flora Italy Oligocene paleobotany paleoclimatology Paleogene paleontology Southern Europe Tertiary...
Journal Article
Published: 01 June 2014
Mineralogical Magazine (2014) 78 (3): 757–774.
...F. Cámara; M. E. Ciriotti; E. Bittarello; F. Nestola; F. Massimi; F. Radica; E. Costa; P. Benna; G. C. Piccoli Abstract The new mineral species grandaite, ideally Sr 2 Al(AsO 4 ) 2 (OH), has been discovered on the dump of Valletta mine, Maira Valley, Cuneo province, Piedmont, Italy. Its origin...
FIGURES
First thumbnail for: Arsenic-bearing new mineral species from Valletta ...
Second thumbnail for: Arsenic-bearing new mineral species from Valletta ...
Third thumbnail for: Arsenic-bearing new mineral species from Valletta ...
Journal Article
Published: 01 January 1964
Bulletin de la Société Géologique de France (1964) S7-VI (4): 573–575.
...Carla Gruas-Cavagnetto Abstract The Oligocene of the Bagnasco basin in the Piedmont of northwestern Italy is poor in microflora in general, but pollen spores from a bed of lignitic marl indicate the presence of a swampy forest of Taxodiaceae and Cupressaceae surrounded by mountainous terrain...
Journal Article
Published: 01 June 2016
European Journal of Mineralogy (2016) 28 (3): 687–696.
..., near Canosio, Cuneo, Piedmont, Italy. It crystallized from As- and Mn-rich hydrothermal fluids in an oxidizing environment. At Monte Nero, it is associated with coralloite, manganohörnesite, rhodochrosite, sarkinite, sterlinghillite, strashimirite and wallkilldellite. At Valletta, it is associated...
FIGURES
First thumbnail for: Castellaroite, Mn 2+ 3 (AsO 4 ) 2 ·4.5H 2 O, a new...
Second thumbnail for: Castellaroite, Mn 2+ 3 (AsO 4 ) 2 ·4.5H 2 O, a new...
Third thumbnail for: Castellaroite, Mn 2+ 3 (AsO 4 ) 2 ·4.5H 2 O, a new...
Journal Article
Published: 03 July 2023
Mineralogical Magazine (2023) 87 (5): 741–747.
... = □, Ca, Na and Fe 2+ ; M = Mg, Fe 2+ , Fe 3+ , Al and Mn; T = Si and P; Ø = O and OH; Z = □, OH and F). It was found in cavities of a leucogranitic orthogneiss at the Casette quarry, Montoso, Bagnolo Piemonte, Cuneo Province, Piedmont, Italy. Crystals of aluminotaipingite-(CeCa) are light pink to pink...
FIGURES
First thumbnail for: Aluminotaipingite-(CeCa), (Ce 6 Ca 3 )Al(SiO 4 ) 3...
Second thumbnail for: Aluminotaipingite-(CeCa), (Ce 6 Ca 3 )Al(SiO 4 ) 3...
Third thumbnail for: Aluminotaipingite-(CeCa), (Ce 6 Ca 3 )Al(SiO 4 ) 3...
Journal Article
Published: 01 December 2021
Mineralogical Magazine (2021) 85 (6): 901–909.
..., Cuneo Province, Piedmont, Italy (~44°19'28“N, 7°51'8“E). Beginning in 1838 this mine worked an Fe–Mn ore deposit for iron (Sismonda, 1841a , 1841b ; Conti, 1873 ), though operations had definitely ceased by the mid 1950s. The deposit is hosted in metaquartzites and quartz-bearing marbles...
FIGURES
First thumbnail for: Armellinoite-(Ce), Ca 4 Ce 4+ (AsO 4 ) 4 ⋅H 2 O, a...
Second thumbnail for: Armellinoite-(Ce), Ca 4 Ce 4+ (AsO 4 ) 4 ⋅H 2 O, a...
Third thumbnail for: Armellinoite-(Ce), Ca 4 Ce 4+ (AsO 4 ) 4 ⋅H 2 O, a...
Journal Article
Published: 01 August 2017
Environmental & Engineering Geoscience (2017) 23 (3): 179–190.
... selected an area belonging to the Bagni di Vinadio municipality (Cuneo, NW Italy), which is part of the Argentera Massif (western Alps), as a test site. Data obtained from the code CurvaTool, developed by the authors, are successfully compared with literature information and with lineaments obtained from...
FIGURES
First thumbnail for: A New Application of Curvatool Semi-automatic Appr...
Second thumbnail for: A New Application of Curvatool Semi-automatic Appr...
Third thumbnail for: A New Application of Curvatool Semi-automatic Appr...
Journal Article
Published: 01 April 2017
Mineralogical Magazine (2017) 81 (2): 305–317.
...F. Cámara; E. Bittarello; M. E. Ciriotti; F. Nestola; F. Radica; F. Massimi; C. Balestra; R. Bracco Abstract T he new mineral species canosioite, ideally Ba 2 Fe 3+ (AsO 4 ) 2 (OH), has been discovered in the dump of Valletta mine, Maira Valley, Cuneo Province, Piedmont, Italy. Its origin...
FIGURES
First thumbnail for: As-bearing new mineral species from Valletta mine,...
Second thumbnail for: As-bearing new mineral species from Valletta mine,...
Third thumbnail for: As-bearing new mineral species from Valletta mine,...
Journal Article
Published: 01 February 2015
Mineralogical Magazine (2015) 79 (1): 171–189.
...Fernando Cámara; Erica Bittarello; Marco E. Ciriotti; Fabrizio Nestola; Francesco Radica; Marco Marchesini Abstract The new mineral species braccoite, ideally Na Mn 5 2 + [Si 5 AsO 17 (OH)](OH), has been discovered in the Valletta mine dumps, in Maira Valley, Cuneo province, Piedmont, Italy. Its...
FIGURES
First thumbnail for: As-bearing new mineral species from Valletta mine,...
Second thumbnail for: As-bearing new mineral species from Valletta mine,...
Third thumbnail for: As-bearing new mineral species from Valletta mine,...
Image
TEM image of a ‘daisy-like’ microstructure made of almost compact chrysotile (chr) surrounded by polygonal sectors (PS) overgrown on peripheral tubules. Cuneo Province, Western Alps, Italy.
Published: 01 October 2002
F ig . 15. TEM image of a ‘daisy-like’ microstructure made of almost compact chrysotile (chr) surrounded by polygonal sectors (PS) overgrown on peripheral tubules. Cuneo Province, Western Alps, Italy.
Image
TEM images of ‘mixing-unmixing’ phenomena between chrysotile and polygonal serpentine. (a) axial microtexture of perfect mixing of PS fibrils into disordered chrysotile. Cuneo Province, Western Alps, Italy. (b) Segregation between PS fibrils and compact chrysotile (chr) inclined to the electron beam. Piedmont zone, Western Alps, Italy.
Published: 01 October 2002
F ig . 16. TEM images of ‘mixing-unmixing’ phenomena between chrysotile and polygonal serpentine. ( a ) axial microtexture of perfect mixing of PS fibrils into disordered chrysotile. Cuneo Province, Western Alps, Italy. ( b ) Segregation between PS fibrils and compact chrysotile (chr) inclined
Image
TEM images of ‘mixing-unmixing’ phenomena between chrysotile and polygonal serpentine. (a) axial microtexture of perfect mixing of PS fibrils into disordered chrysotile. Cuneo Province, Western Alps, Italy. (b) Segregation between PS fibrils and compact chrysotile (chr) inclined to the electron beam. Piedmont zone, Western Alps, Italy.
Published: 01 October 2002
F ig . 16. TEM images of ‘mixing-unmixing’ phenomena between chrysotile and polygonal serpentine. ( a ) axial microtexture of perfect mixing of PS fibrils into disordered chrysotile. Cuneo Province, Western Alps, Italy. ( b ) Segregation between PS fibrils and compact chrysotile (chr) inclined
Image
(a) Photomicrograph (PPL) of Na-pyroxenite (TC6-1/3 from Valgrana-Tetto Chiapello, Cuneo Province, northern Italy) with a typical pseudomorph of paragonite and epidote after former lawsonite. (b) Photomicrograph (PPL) of quartz–jadeite rock (OF 3039: from Monviso massif, Western Alps, northern Italy) deriving from HP recrystallization of an original igneous trondhjemite of oceanic affinity. (online version in colour)
Published: 01 October 2014
Fig. 9 (a) Photomicrograph (PPL) of Na-pyroxenite (TC6-1/3 from Valgrana-Tetto Chiapello, Cuneo Province, northern Italy) with a typical pseudomorph of paragonite and epidote after former lawsonite. (b) Photomicrograph (PPL) of quartz–jadeite rock (OF 3039: from Monviso massif, Western Alps
Image
TEM image of the cross-section of an asbestiform composite made of axially-textured carlosturanite (cst) transforming into chrysotile and then into polygonal serpentine (PS). The larger the size of the PS, the earlier they nucleated: first at triple-grain junctions, then at interfaces and more rarely inside cst grains themselves. [010]cst//[100]PS//fibre axis. Cuneo Province, Western Alps, Italy.
Published: 01 October 2002
and more rarely inside cst grains themselves. [010] cst //[100] PS //fibre axis. Cuneo Province, Western Alps, Italy.
Image
Chemical composition of clinopyroxenes in Na-pyroxenites and eclogites used to produce Neolithic axes from Alba (near Cuneo) and Finale Ligure (near Savona, northern Italy), plotted in the compositional diagram jadeite (Jd) – aegirine (Ae) – Ca-Mg-Fe pyroxenes (Wo, En, Fs) of Morimoto et al. (1988). (a) Cumulative diagram of spot analyses of Na-pyroxenite (8 samples). (b) Cumulative diagram of spot analyses of eclogites (5 samples).
Published: 01 October 2014
Fig. 5 Chemical composition of clinopyroxenes in Na-pyroxenites and eclogites used to produce Neolithic axes from Alba (near Cuneo) and Finale Ligure (near Savona, northern Italy), plotted in the compositional diagram jadeite (Jd) – aegirine (Ae) – Ca-Mg-Fe pyroxenes (Wo, En, Fs) of Morimoto et