Relevant bibliographies by topics / Massif de Szklary (Pologne)

Contents

  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Massif de Szklary (Pologne)'

Author: Grafiati
Published: 4 May 2024

Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles

Select a source type:

Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Massif de Szklary (Pologne).'

Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.

You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.

Journal articles on the topic "Massif de Szklary (Pologne)"

1

Pieczka, Adam, Mark A. Cooper, and Frank C. Hawthorne. "Lepageite, Mn32+(Fe73+Fe42+)O3[Sb53+As83+O34], a new arsenite-antimonite mineral from the Szklary pegmatite, Lower Silesia, Poland." American Mineralogist 104, no. 7 (2019): 1043–50. http://dx.doi.org/10.2138/am-2019-6903.

Full text
Abstract:
Abstract Lepageite, a new arsenite-antimonite mineral, was discovered in a granitic pegmatite hosted by serpentinites of the Szklary massif, Lower Silesia, southwest Poland. Lepageite is a primary mineral formed during injection of an evolved LCT-type melt related to anatectic processes within the metasedimentary-metavolcanic complex of the nearby Góry Sowie Block, ~380 Ma, into serpentinite of the Szklary massif and its contamination by fluid-mobile serpentinite-hosted elements, among others As and Sb, transported in the form of H2AsO3− and HSbO2 species at pH ≈ 9–11 and a low redox potential
APA, Harvard, Vancouver, ISO, and other styles
2

Cieślik, Błażej, Jakub Kierczak, and Anna Pietranik. "Mineralogical and geochemical evidence for two-stage silicification of serpentinized peridotites from the Szklary Massif (NE Bohemian Massif)." Mineralogia 53, no. 1 (2022): 20–35. http://dx.doi.org/10.2478/mipo-2022-0003.

Full text
Abstract:
Abstract Previously unknown exposures of silicified serpentinites have been documented within the Szklary Massif, which is a fragment of the tectonically dismembered Central Sudetic Ophiolite (NE Bohemian Massif). On the basis of textural, mineralogical and chemical differences, two types of silicified serpentinites have been distinguished in this study (Type I and Type II). Type I is characterized by well-preserved primary minerals cut by numerous veinlets filled with microscale euhedral quartz crystals. Studied samples of Type I are enriched in silica (from 62 to 69 wt.% SiO2) and depleted i
APA, Harvard, Vancouver, ISO, and other styles
3

Kaczan, Wojciech, Jan Kudełko, and Herbert Wirth. "Szklary nickel deposit — a review and introduction to attempts in hydrometallurgical processing." Mineral Economics 34, no. 2 (2021): 315–22. http://dx.doi.org/10.1007/s13563-021-00269-0.

Full text
Abstract:
AbstractSzklary Massif is situated about 60 km from Wrocław (southwestern Poland) and around 7 km from Ząbkowice Śląskie. The history of raw materials in this region started in the fifteenth century with the discovery of precious minerals like chrysoprase, chalcedony, and opal. The exploitation of nickel ore in this region started in the nineteenth century and was conducted with few stops until 1983. The remaining 17.21 mln mg of ore with 125,000 mg of nickel might be a chance to satisfy rising demand for raw materials used to develop electromobility. One of the crucial aspects regarding possi
APA, Harvard, Vancouver, ISO, and other styles
4

Nieuwazny, Andrzej. "Patriotes ou mercenaires ?" Revue Historique des Armées 260, no. 3 (2010): 26–36. http://dx.doi.org/10.3917/rha.260.0026.

Full text
Abstract:
L’échec de l’insurrection de Kosciuszko (1794) et le troisième partage de la Pologne, effectué une année plus tard par la Russie, l’Autriche et la Prusse, provoquèrent l’émigration des dirigeants de l’insurrection et de militaires polonais. Paris devint alors le centre d’attraction d’une grande majorité de ces émigrés qui, divisés en factions, se disputèrent les faveurs du Directoire. La majorité rêvait d’une force militaire capable de recommencer la lutte pour l’indépendance. Les légions polonaises au service de la France (1797-1807) marquèrent le commencement du phénomène de service massif d
APA, Harvard, Vancouver, ISO, and other styles
5

Gadas, Petr, Milan Novák, Michaela Vašinová Galiová, et al. "Secondary Beryl in Cordierite/Sekaninaite Pseudomorphs from Granitic Pegmatites – A Monitor of Elevated Content of Beryllium in the Precursor." Canadian Mineralogist, December 17, 2020. http://dx.doi.org/10.3749/canmin.2000014.

Full text
Abstract:
Abstract Cordierite-group minerals (cordierite and sekaninaite) from granitic pegmatites are often strongly to completely altered to a fine- or coarse-grained mixture of muscovite, chlorite and/or, biotite, along with several less common secondary minerals, including mainly paragonite, tourmaline, and secondary beryl. The mixture is a common product of early subsolidus hydrothermal alteration at the examined pegmatites of the beryl-columbite subtype – Věžná I and Drahonín (Moldanubian Zone, Czech Republic) and Mount Begbie (Shuswap Complex, Canada); of the beryl-columbite-phosphate subtype – S
APA, Harvard, Vancouver, ISO, and other styles

Dissertations / Theses on the topic "Massif de Szklary (Pologne)"

1

Kierczak, Jakub. "Spéciation solide du nickel et du chrome dans un site minier et industriel à usage agricole (Szklary, Pologne)." Limoges, 2007. https://aurore.unilim.fr/theses/nxfile/default/9a2fbfbb-1238-4d3e-af9f-c2d3e533d23f/blobholder:0/2007LIMO4034.pdf.

Full text
Abstract:
Dans le site étudié du Massif de Szklary (Pologne), Ni et Cr sont présents à des concentrations élevées dans deux environnements d’origine distincte : naturelle (sols développés sur serpentinites) et industrielle (haldes de déchets pyrométallurgiques issus de l’exploitation du Ni). L’objectif de cette étude est de localiser les minéraux porteurs d’éléments potentiellement toxiques (EPT), principalement de Ni et Cr, dans ces divers environnements et de comparer leur mobilité dans les conditions actuelles d’altération (climat tempéré transitionnel de Pologne). Ces travaux s’intéressent également
APA, Harvard, Vancouver, ISO, and other styles
2

Brassinnes, Stéphane. "Relations cumulat-liquide dans les massifs alcalins et carbonatitiques: les cas des massifs de Vuoriyarvi (Péninsule de Kola, Russie) et de Tajno (N.E. Pologne)." Doctoral thesis, Universite Libre de Bruxelles, 2006. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/210796.

Full text
Abstract:
Les carbonatites sont des roches magmatiques essentiellement composées de carbonates (calcite et/ou dolomite) d'origine magmatique. Leur statut pétrographique en tant que liquide magmatique ou cumulat reste à l'heure actuelle fort contreversé. Cette thèse de doctorat à pour objectif une étude pétrographique fine de ces roches couplée à des microanalyses in-situ des éléments en trace des principaux minéraux (carbonate, apatite).<br>Doctorat en sciences, Spécialisation géologie<br>info:eu-repo/semantics/nonPublished
APA, Harvard, Vancouver, ISO, and other styles
We offer discounts on all premium plans for authors whose works are included in thematic literature selections. Contact us to get a unique promo code!

To the bibliography