Fernando Cámara

Prof. Fernando Cámara

Università degli studi di Milano - Dipartimento di Scienze della Terra
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Research Focus & Metrics

Academic Career Length

29Years (1998-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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7 November 2015 in Acta crystallographica Section B, Structural science, crystal engineering and materials
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Journal Article
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LPLukáš Palatinus
Lukáš Palatinus
CCCinthia Antunes Corrêa
Cinthia Antunes Corrêa
GSGwladys Steciuk
Gwladys Steciuk
DJDamien Jacob
Damien Jacob
PRPascal Roussel
Pascal Roussel
VPVaclav Petricek
Vaclav Petricek

3 April 2010 in Contributions to Mineralogy and Petrology
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Journal Article
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MTMario Tribaudino
Mario Tribaudino
RARoss Angel
Ross Angel
FCFernando Cámara
Fernando Cámara
FNFabrizio Nestola
Fabrizio Nestola
DPD. Pasqual
D. Pasqual
IMI. Margiolaki
I. Margiolaki

1 August 1999 in American Mineralogist: Journal of Earth and Planetary Materials
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Journal Article
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LGLaurence A. J. Garvie
Laurence A. J. Garvie
BDBertrand Devouard
Bertrand Devouard
TGThomas L. Groy
Thomas L. Groy
FCFernando Cámara
Fernando Cámara
PBPeter R. Buseck
Peter R. Buseck
Kanemite was studied by single-crystal X-ray diffraction. The mineral, ideally NaHSi 2 O 5 .3H 2 O, is orthorhombic (space group Pbcn); unit-cell parameters are a = 4.946(3), b = 20.502(15), c = 7.275(3) Aa, with Z = 4. The structure is solved and refined to an R value of 0.058 for 825 independent reflections. The arrangement of atoms consists of alternating (010) sheets of corrugated [Si 2 O 4 OH] (super n-) n and hydrated Na. The silicate sheets contain six-membered rings of HOSiO 3 -SiO 4 units. Sodium atoms coordinate to six water molecules, forming layers of distorted octahedra. Residual electron densities were located that give reasonable positions for four H atoms. One H is part of a silanol group, and the other three H atoms are associated with water bonded to Na. Bonding between the silicate and Na sheets is through hydrogen bonding from H of the Na layer to O of the silicate sheet.

1 December 2017 in Mineralogical Magazine
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Journal Article
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ESE. Sokolova
E. Sokolova
FCFernando Cámara
Fernando Cámara
Here we report a nomenclature and classification for the seidozerite-supergroup minerals. The TS (Titanium-Silicate) block is the main structural unit in all seidozerite-supergroup structures; it consists of a central O (O = Octahedral) sheet and two adjacent H (H = Heteropolyhedral) sheets where Si2O7groups occur in the H sheets. The TS block is characterized by a planar minimal cell based on translation vectors, t1and t2, the lengths of these vectors are t1 ≈ 5.5 and t2 ≈ 7 Å, and t1 ^ t2 is close to 90°. The forty-five minerals of the sedozerite supergroup are divided into four groups based on the content of Ti and topology and stereochemistry of the TS block: in rinkite, bafertisite, lamprophyllite and murmanite groups, Ti (+ Nb + Zr + Fe3++Mg + Mn) = 1, 2, 3 and 4 apfu (atoms per formula unit), respectively. All TS-block structures consist either solely of TS blocks or of two types of block: the TS block and an I (Intermediate) block that comprises atoms between two TS blocks. Usually, the I block consists of alkali and alkaline-earth cations, H2O groups and oxyanions (PO4)3-, (SO4)2-and (CO3)2-.The general formula of the TS block is as follows AP2BP2MH2MO4(Si2O7)2X4+n, where MH2and MO4= cations of the H and O sheets; MH = Ti, Nb, Zr, Y, Mn, Ca + REE, Ca;MO = Ti, Zr, Nb, Fe3+, Fe2+, Mg, Mn, Zn, Ca, Na; AP and BP = cations at the peripheral (P) sites = Na, Ca + REE, Ca, Zn, Ba, Sr, K; X = anions = O, OH, F, H2O; XO4+n=XO4 +XPn, n = 0, 1, 1.5, 2, 4; XP= XPMand XPA= apical anions of MH and AP cations at the periphery of the TS block.

1 December 2006 in Geochimica et Cosmochimica Acta
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Journal Article
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IMI. Stewart McCallum
I. Stewart McCallum
MDM. Chiara Domeneghetti
M. Chiara Domeneghetti
JSJeffrey M. Schwartz
Jeffrey M. Schwartz
EMEmily K. Mullen
Emily K. Mullen
MZMichele Zema
Michele Zema
JGJibamitra Ganguly
Jibamitra Ganguly

1 October 2007 in Reviews in Mineralogy and Geochemistry
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Journal Article
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ROR. Oberti
R. Oberti
FHFrank Hawthorne
Frank Hawthorne
ECE. Cannillo
E. Cannillo
FCFernando Cámara
Fernando Cámara