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Cima Pal

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Journal Article
Published: 01 March 2003
European Journal of Mineralogy (2003) 15 (2): 357–363.
... 0.25 ) ∑2.01 (Si 3.47 Al 0.53 ) ∑4 O 10 (OH) 2 , from Cima Pal (western Alps) are presented and discussed. They have been obtained by a synergic approach based on neutron powder diffraction from 293 K to 873 K, and on Mössbauer spectroscopy at ambient conditions, of the sample before and after heating...
FIGURES
Journal Article
Published: 01 November 2001
European Journal of Mineralogy (2001) 13 (6): 1025–1034.
...Gabriella IVALDI; Giovanni FERRARIS; Nadia CURETTI; Roberto COMPAGNONI Abstract Randomly oriented phengite flakes, up to 15 cm across and 5 cm thick, occur in a metamorphic dyke at Cima Pal (upper Val Savenca, western Alps). The phengite formed in the Sesia zone at quartz-eclogite-facies conditions...
FIGURES
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Flake of the <b>Cima</b> <b>Pal</b> zoned phengite (plain light transmission optical micr...
Published: 01 November 2001
Fig. 1. Flake of the Cima Pal zoned phengite (plain light transmission optical microscopy). The two large areas of 2 M 1 and 3 T (extinct in between crossed polarizers) polytypes are separated by a white line.
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Selected bond lengths (Å) for the <b>Cima</b> <b>Pal</b> polytypes;  esd&#x27;s  in parenthes...
Published: 01 November 2001
Table 5. Selected bond lengths (Å) for the Cima Pal polytypes; esd's in parentheses.
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Principal distortion parameters in the structures of the <b>Cima</b> <b>Pal</b> polytypes...
Published: 01 November 2001
Table 7. Principal distortion parameters in the structures of the Cima Pal polytypes.
Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.9
EISBN: 9781862393899
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.178.01.12
EISBN: 9781862394261
..., on the inner platform, rudist lithosome formation was restricted by the lack of an adequate substrate and by higher sedimentation rates. On the outer platform, the Cima delle Murelle Formation is dominated by metre-scale cycles composed of coarse, cross-bedded bioclastic lime rudstones...
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Miscellaneous data collection and structure refinement information for the ...
Published: 01 November 2001
Table 2. Miscellaneous data collection and structure refinement information for the 2 M 1 and 3 T -polytypes of the Cima Pal phengite.
Series: Geophysical Developments Series
Published: 01 January 1997
EISBN: 9781560802099
.../s) Lower Cret. platform (Morrone di Pacentro Fm) 0 4 1.6 2.69 6315 “mid”-Cretaceous unconformity (breccias) 1 6 3.7 2.70 6160 “mid”-Cretaceous unconformity (bauxites) 1 3 12.5 2.81 4754 Up. Cretaceous platform (Cima delle Murelle Fm) 1 21 4.6 2.64 6044 Up. Cret...
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Average and range of microprobe analyses (wt %) on yellow (Y) and greenish ...
Published: 01 November 2001
Table 1. Average and range of microprobe analyses (wt %) on yellow (Y) and greenish (G) parts of the 2 M 1 and 3 T polytypes occurring in the Cima Pal phengite.
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Effective Coordination Number (ECoN), Charge Distribution ( Q ) and Bond-Va...
Published: 01 November 2001
Table 6. Effective Coordination Number (ECoN), Charge Distribution ( Q ) and Bond-Valence ( s ) for the best refined 2M1Y and 3TY polytypes of Cima Pal (the values of the other two samples are not significantly different).
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Electron contents ( el , when refined), atom positions ( xyz ) and isotropi...
Published: 01 November 2001
Table 3. Electron contents ( el , when refined), atom positions ( xyz ) and isotropic equivalent displacement factors ( U eq ) (x 10 4 ) for two samples of Cima Pal 2 M 1 Y (line 1) and 2 M 1 G (line 2) phengitic polytypes; esd's in parentheses.
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Electron contents ( el , when refined), atomic content, atom positions ( xy...
Published: 01 November 2001
Table 4. Electron contents ( el , when refined), atomic content, atom positions ( xyz ) and isotropic equivalent displacement factors ( U eq ) for two samples of Cima Pal 3TY (line 1) and 3TG (line 2) phengitic polytypes; esd's in parentheses.
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Structural interpretation of the eastern Southern Alps. Denomination of the...
Published: 01 June 2009
); Valsugana S. (VV); Val di Sella L. (VS); Colombarone klippe (C); Belluno L. (BL); Civetta L. (CI); Duron-Fedaia L. (VDF); Foiana-Mezzocorona S. (FMZ); Trento-Cles L. (TC); Calisio L. (CAL); Val d’Astico L. (VAS); Schio-Vicenza L. (SCHV); Rovereto-Riva-Arco transfer zone (R); Recoaro zone (RE); Cima Marana L
Journal Article
Published: 01 February 2008
American Mineralogist (2008) 93 (2-3): 451–455.
... of phengite from Cima Pal (Val Savenca, western Alps): Chemical and polytypic zoning and structural characterization . European Journal of Mineralogy , 13 , 1025 – 1034 . Ivaldi , G. , Curetti , N. , and Gula , A. ( 2002 ) Caratterizzazione strutturale dei politipi 3 T e 2 M 1 della...
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Published: 01 January 2013
DOI: 10.1180/DHZ.22
EISBN: 9780903056434
.... Muscovite 2M 1 , peraluminous granite, Sardinia, Italy (Brigatti M.F., Frigieri, P. & Poppi, L., 1998, Amer. Min ., 83 , 775–85). 3. Phengite 3T, metamorphic glaucophane-, phengite- and quartz-rich layered dyke rock. UHP Seisa zone (quartz eclogite facies), Cima Pal, Val Savenca, western Alps...
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Journal Article
Published: 01 August 2010
American Mineralogist (2010) 95 (8-9): 1182–1191.
.... , Ferraris , G. , Curetti , N. , and Compagnoni , R. ( 2001 ) Coexisting 3 T and 2 M 1 polytypes in a phengite from Cima Pal (Val Savenca, western Alps): Chemical and polytypic zoning and structural characterisation . European Journal of Mineralogy , 13 , 1025 – 1034 . Kihara , K...
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Journal Article
Published: 01 February 2013
The Canadian Mineralogist (2013) 51 (1): 5–14.
... N. Compagnoni R. ( 2001 ) Coexisting 3T and 2M 1 polytypes of phengite from Cima Pal (Val Savenca, western Alps): chemical and polytypic zoning and structural characterization . European Journal of Mineralogy 13 , 1025 – 1034 . doi: 10.1127/0935-1221/2001/0013-1025 Klapetek P...
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Journal Article
Published: 01 July 2007
American Mineralogist (2007) 92 (7): 1158–1164.
... reactions as a function of temperature in a phengite 3T (Cima Pal, western Aps) by neutron diffraction and Mössbauer spectroscopy. European Journal of Mineralogy , 15 , 357 –363. Proyer, A. ( 2003 ) Metamorphism of pelites in NKFMASH—a new petrogenetic grid with implications for the preservation...
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Journal Article
Published: 01 April 2005
Clays and Clay Minerals (2005) 53 (2): 190–197.
... phlogopite and annite . American Mineralogist , 58 , 889 – 900 . Ivaldi , G. , Ferraris , G. , Curetti , N. and Compagnoni , R. ( 2001 ) Coexisting 3T and 2M 1 polytypes of phengite from Cima Pal (Val Savenca, western Alps): chemical and polytypic zoning and structural...
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