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Hydrothermal episyenitic bodies located in the east of the Pedriza Massif. East Pedriza Massif (Central System, Spain), Link to MinDat Location Data. Try searching images.google …
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Named for its monoclinic crystal structure and relationship with holmsquisite. Approved IMA 1985, Discredited IMA 2005 as being fluoro-sodic-pedrizite. Comments: Dark blue fibrous clinoholmquistite with radiating structure, variety magnesioclinoholmquistite. Clinoholmsquitite may be a new aphibole, fluoro-sodic-pedrizite..
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Dimorphous with magnesioholmquistite, forms a series with clinohomquistite and ferroclinoholmquistite. Unspecified locality in Siberia, Russia. Link to MinDat Location …
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Investigation of the holotype material of clino-holmquistite (Ginzburg, 1965) showed it to be a mixture of two distinct amphibole compositions, tremolite and a new amphibole end-member, then named fluoro-sodic-pedrizite (Oberti et al. 2005; IMA 2004-002). The latter was subsequently renamed fluoro-pedrizite.
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Named for its monoclinic crystal structure and relationship with holmsquisite. Approved IMA 1985, Discredited IMA 2005 as being fluoro-sodic-pedrizite. Comments: Dark blue fibrous …
WhatsApp: +86 18221755073
The original material used to describe clino-ferri-holmquistite (IMA1995-045) by Caballero et al (1998) (originally named by them as "ferri-clinoholmquistite") was renamed "sodic-ferri-clinoholmquistite" and finally became Clino-ferro-ferri-holmquistite, its current valid name.
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Clino-ferri-holmquistite mineral data, information about Clino-ferri-holmquistite, its properties and worldwide locations.
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magnesio-clinoholmquistite and ferro-clinoholmquistite. Mineral Group: Amphibole (Fe{Mn{Mg) group: 0.1 · Mg=(Mg+Fe2+) · 0.89; (Ca+Na) B < 1.34; Li ¸ 1.0. Occurrence: Partly replaced by holmquistite. Association: Holmquistite, calcite. Distribution: From the Tastyg spodumene deposit, Tuva, Siberia, Russia.
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Investigation of the holotype material of clino-holmquistite (Ginzburg, 1965) showed it to be a mixture of two distinct amphibole compositions, tremolite and a new amphibole end-member, …
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The relative intensities of these bands show that there is almost complete Mg-Fe 2+ substitution at M(1,3) in ferri-clinoholmquistite and that there is no significant short-range ordering (cluster and/or anti-clustering) between these two cations at the M(1,3) sites.
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Hydrothermal episyenitic bodies located in the east of the Pedriza Massif. East Pedriza Massif (Central System, Spain), Link to MinDat Location Data. Try searching images.google or Mindat Picture Gallary for mineral pictures. Caution: …
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The relative intensities of these bands show that there is almost complete Mg-Fe 2+ substitution at M(1,3) in ferri-clinoholmquistite and that there is no significant short-range …
WhatsApp: +86 18221755073
The original material used to describe clino-ferri-holmquistite (IMA1995-045) by Caballero et al (1998) (originally named by them as "ferri-clinoholmquistite") was renamed "sodic-ferri …
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The root-name mineral, clino-holmquistite are defined with Mg, Al and (OH) as the dominant elements. Minerals with other dominant elements are named with pre-fixes in accordance with the guidelines establised in the 2012 amphibole nomenclature. nd. Lithium Amphibole Subgroup > w (OH, F, Cl)-dominant Amphibole Group > Amphibole Supergroup.
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The root-name mineral, clino-holmquistite are defined with Mg, Al and (OH) as the dominant elements. Minerals with other dominant elements are named with pre-fixes in accordance with …
WhatsApp: +86 18221755073
Dimorphous with magnesioholmquistite, forms a series with clinohomquistite and ferroclinoholmquistite. Unspecified locality in Siberia, Russia. Link to MinDat Location Data. Named for its composition, monoclinic crystal structure, and relationship with holmsquisite. Discredited as clinoholmquistite (1997). Clinohomsquisite discredited (2005).
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