SVIBOR - Papers quoted in CC - project code: 1-09-016

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Papers quoted in Current Contents on project 1-09-016


Quoted papers: 10
Other papers: 21
Total: 31


Title: Tuzlaite, NaCaB5O8(OH)2*3H2O, a new mineral with a pentaborate sheet structure from the Tuzla salt mine, Bosnia and Herzegovina

Authors:
Bermanec, Vladimir (96490)
Armbruster, Thomas
Tibljaš, Darko (106871)
Šturman, Darko
Kniewald, Goran (85574)
Journal: American Mineralogist
ISSN: 0003-004X
Volume: 79
Year: 1994
Pages: from 562 to 569
Number of references: 30
Language: engleski
Summary: Tuzlaite, NaCa(B5O8)(OH)2)*3H2O, is a monoclinic sheet borate occuring in nearly monomineralic veinlets formed in the course dolomitic marl diagenesis at the Tuzla salt mine (Bosnia and Hercegovina. Tuzlaite possesses a new type of pentaborate sheet structure with fourfold- and threefold-coordinated B. Borate triangles and tetrahedra form ten-memberd rings. The sheets are connected by Na and Ca, which are cordinated to additional H2O. The new mineral is colorless to white. It is biaxial positive, optical orientation is Y=b. Z:a=14. Tuzlaite has perfect cleavage parallel to (001), H=2-3, Dmeas=2.21, Dcalc=2.23 gcm-3. The new mineral is named after town Tuzla, where it was found.
Keywords: tuzlaite, crystal structure, X-ray data, chemical composition, optical data, Tuzla, pentaborate

Title: Centro-symmetric tilasite from Nežilovo, Macedonia: A crystal structure refinement

Authors:
Bermanec, Vladimir (96490)
Journal: Neues Jahrbuch fuer Mineralogie
Volume: 7
Year: 1994
Pages: from 289 to 294
Number of references: 13
Language: engleski
Summary: The crystal structure of natural tilasite, CaMg(AsO4)F, a=6.681(2) A, b=8.950(2) A, c=7.573(2) A and beta=121.14(2), Z=4 from Nežilovo, Macedonia was refined from X-ray single cristal data in space group C2/c to R=2.79%. The reasults clearly indicate that this tilasite crystallizes in the centric space group C2/c and not in CC as assumed for the sample from Bisbee, Arizona.
Keywords: Tilasite, X-ray structural refinement, Nežilovo, Macedonia

Title: Crystal chemistry of Pb- and REE-rich piemontite from Nežilovo, Macedonia

Authors:
Bermanec, Vladimir (96490)
Armbruster, Thomas
Oberhaensli, Roland
Zebec, Vladimir (64534)
Journal: Schweiz. mineral. petrogr. Mitt.
Volume: 74
Year: 1994
Pages: from 321 to 328
Number of references: 29
Language: engleski
Summary: An unusual REE- and Pb-rich epidote group mineral related to piemontite was found at Nežilovo, Macedonia where a mica schist with red mica, quartz, ardennite, gahnite, franklinite(?) and piemontite occurs in a metamorphic complex. This mineral is an intermediate member between piemontite, hypothetical CaPbAl2Mn(Si2O7)(SiO4)O(OH,F)-related to hancockite and allanite. Piemontite from Nežilovo is deep red, nearly black, with admantine luster and greyish-pinkish streak. The unusual mineral is brittle, with uneven fracture and without observed cleavage. The mineral is pleochoic: X=yellow-brown, Y=brown-red and Z=purple-brown.
Keywords: piemontite, Pb, REE, electron microprobe analysis, crystal chemistry, structure refinement, X-ray single crystal data, Nežilovo, Macedonia

Title: Childrenite and crandalite from Stari Trg mine (Trepča), Kosovo: new data

Authors:
Bermanec, Vladimir (96490)
Šćavničar, Stjepan (46231)
Zebec, Vladimir (64534)
Journal: Mineralogy and Petrology
Volume: 52
Year: 1995
Pages: from 197 to 208
Number of references: 26
Language: engleski
Summary: Childrenite and crandallite are described as two new phosphate members in the paragenesis of the Stari Trg mine which comprises vivianite, ludlamite and struvite. Crandallite crystals with very simple rhombohedral habit grow on rhombohedral carbonate and childrenite crystals. The crystal morphology of childrenite is very similar to that at described from other localities. Following forms were measured: 100, 010, 110, 120, 121, 221, 342. The average chemical composition is Childrenite91Eosphorite9. Pseudo-orthorombic unit cell dimensions were calculated: a=10.390(4)A, b=13.390(4)A and c=6.920(2)A. Growth sectors and sector twins of childrenite are described.

Title: Nchwaningite, Mn2SiO3(Oh)2*H2O, a new pyroxene-related chain silicate from the N'chwaning mine, Kalahari manganese field, South Africa

Authors:
Nyfeler, Daniel
Armbruster, Thomas
Dixon, Roger
Bermanec, Vladimir (96490)
Journal: American Mineralogist
Number: 3-4
ISSN: 0003-004X
Volume: 80
Year: 1995
Pages: from 377 to 386
Number of references: 30
Language: engleski
Summary: Nchwaningite, Mn2SiO3(Oh)2*H2O, is an orthorombic chain silicate (space group Pca2, Z=4, a=12.672(9), b=7.217(3), c=5.341(2) A), occuring as aggregates shaped like pin cushions, together with calcite, bultfonteinite and chlorite at N'chwaning mine, located in the Kalahari manganese field, South Africa. The aggregats consist of light brown, transparent needles. Nchwaningite is biaxially negative, the optical orientation is X=b, Y=a and Z=c, has two perfect cleavages parallel to (010) and (100), Dcalc=3.202 gcm-3. The nchwaningite structures consist of double layers of laterally linked so-called truncated pyroxene-building units formed by double chain of octahedra, topped with a Zweier single chain of Si tetrahedra. Symmetry-equivalent units are linked laterally but turned upside down. This yields a double-layer structure with H bridges linking the layers. A striking feature of the structure is that one MnO6 corner is formed by a H2O molecule.
Keywords: nchwaningite, crystal structure, opical data, X-ray data, chemical composition, chain silicate, Kalahari

Title: The depositional environment of the evaporite mineral series at Tuzla, Bosnia and Hercegovina

Authors:
Kniewald, Goran (85574)
Bermanec, Vladimir (96490)
Tibljaš, Darko (106871)
Number: ort
ISSN: 0373-434X
Volume: Rapp
Year: 1995
Pages: from 105 to 105
Number of references: 106
Language: engleski


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