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Szklary Massif

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Journal Article
Published: 01 July 2019
American Mineralogist (2019) 104 (7): 1043-1050.
...Adam Pieczka; Mark A. Cooper; Frank C. Hawthorne 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...
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Image
Geological sketch of the <b>Szklary</b> <b>massif</b>(after  Niśkiewicz, 1967 ,  Michali...
Published: 01 April 2011
F ig . 1. Geological sketch of the Szklary massif(after Niśkiewicz, 1967 , Michalik, 2000 ).
Journal Article
Published: 01 August 2007
The Canadian Mineralogist (2007) 45 (4): 901-914.
... pegmatite occurring within serpentinites of the Szklary massif in Lower Silesia, Poland. This pegmatite is a representative of the MSREL–REE subclass of the muscovite – rare-element pegmatites. The beusite usually occurs there as a Mn-dominant, (Ca,Fe)-bearing, Mg-enriched phase devoid of the typical...
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Journal Article
Published: 01 April 2011
Mineralogical Magazine (2011) 75 (2): 303-315.
...F ig . 1. Geological sketch of the Szklary massif(after Niśkiewicz, 1967 , Michalik, 2000 ). ...
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Journal Article
Published: 01 October 2010
American Mineralogist (2010) 95 (10): 1478-1492.
...) columbite-(Mn) tantalite-(Mn) stibiocolumbite stibiotantalite holtite fersmite pyrochlore-group minerals fractionation trends Szklary pegmatite Lower Silesia Poland A pegmatite dike hosted by serpentinite in the Szklary massif is exposed over a small area (about 4 × 1 m), but can...
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Journal Article
Published: 01 August 2013
Mineralogical Magazine (2013) 77 (6): 2841-2856.
... granitic pegmatite in the Szklary serpentinite massif, ~60 km south of Wrocław, Lower Silesia, SW Poland (latitude 50°39.068′; longitude 16°49.932′), in the southern part of the Mississippian Niemcza shear zone that extends along the eastern edge of the Sowie Mountains block in the northeastern part...
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Journal Article
Published: 01 June 2009
The Canadian Mineralogist (2009) 47 (3): 557-572.
... during the processing of sulfide ore. The slags studied occur on a dump in the area of the Szklary serpentinite massif in Lower Silesia, 50°38′51″ N, 16°50′33″ E; Fig. 1 ). The Szklary serpentinites belong to a tectonically dismembered Paleozoic ophiolitic sequence ( Pin et al. 1988 ). During...
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Map showing the location and geology of the <b>Szklary</b> serpentinite <b>massif</b> (af...
Published: 01 October 2010
F igure 1. Map showing the location and geology of the Szklary serpentinite massif (after Niskiewicz 1967 ; Michalik 2000 ).
Journal Article
Published: 28 February 2018
Mineralogical Magazine (2018) 82 (4): 913-928.
... al ., 2004 ) and Piława Górna (Pieczka et al ., 2010 ). Additionally, a dark blue dravite was described from a small lens of a LCT-type pegmatite hosted by serpentinite of the Szklary massif (Pieczka, 2007 ), considered to be an external representative of the Góry Sowie pegmatitic melts intruded...
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Journal Article
Published: 01 October 2014
American Mineralogist (2014) 99 (10): 2008-2017.
... is the late-magmatic to early hydrothermal accessory component of the nepheline syenite in the alkaline Mariupol massif in Ukraine. It represents partly metamict, patchy-zoned, A -cation depleted, REE-, U-, and Th-bearing fluornatropyrochlore, locally exceptionally rich in SiO 2 (up to 13.01 wt...
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Journal Article
Published: 01 July 2015
The Canadian Mineralogist (2015) 53 (4): 653-672.
...Matthieu Harlaux; Christian Marignac; Michel Cuney; Julien Mercadier; Rémi Magott; Bernard Mouthier The Puy-les-Vignes deposit, located in the northwestern part of the French Massif Central, is a remarkable occurrence in the West European Variscan belt of hydrothermal tungsten mineralization...
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Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.12
EISBN: 9781862394490
... overprint), with analogues elsewhere in the Bohemian Massif, Massif Central and Armorica; (3) Moldanubian (Gföhl) Terrane comprising the Orlica-Śnieżnik and Kamieniec massifs, affected by Early Carboniferous high-grade metamorphism and exhumation and (4) Brunovistulian Terrane in the East Sudetes, set up...
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Journal Article
Published: 01 August 1998
Journal of the Geological Society (1998) 155 (4): 711-724.
... (Nova Ruda massif, Sm Nd whole-rock crystal- lization age 351&16 Ma, Pin et al. 1988b), and in the east (Braszowice and Szklary massifs). Their detritus is found in the Upper Devonian of the Swiebodzice Depression and in the autochthonous segment of the adjacent Góry Bardzkie suc- cession (Franke et al...
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.06
EISBN: 9781862394278
...–collision. There is no conclusive evidence of an Ordovician orogenic event. Tectonic units in the Sudetes are shown to be related to terranes defined in western parts of the Bohemian Massif. The Lausitz–Izera Block, the Orlica–Śnieżnik Unit and the Staré Město Belt represent easterly continuations...
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Journal Article
Published: 01 September 2005
Journal of the Geological Society (2005) 162 (5): 841-855.
...-facies country rock of the Góry Sowie Block ( Zakowa 1963 ), and places stratigraphic constraints on the surface exposure of the massif during that period (320–300 Ma). The Góry Sowie Block is also bordered by numerous ophiolitic complexes (Sleza, Nowa Ruda, Braszowice and Szklary units), which have...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2008
DOI: 10.1144/CEV2P.9
EISBN: 9781862393899
... et al. 1999 ; von Raumer et al. 2002 , 2003). Evidence of Precambrian metallogenesis can be found mainly in the Bohemian Massif. In the Teplá-Barrandian Zone of the Bohemian Massif the Neoproterozoic/Cambrian boundary is marked by an angular unconformity between Neoproterozoic basement rocks...
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Geological sketch of the Góry Sowie Mountains block and adjacent units: th...
Published: 01 August 2007
F ig . 1. Geological sketch of the Góry Sowie Mountains block and adjacent units: the Szklary serpentinite massif is located inside a box. Units: 1) Fragments of the Sudetic ophiolite, 2) Neogene basalts, 3) amphibolites, 4) gneisses and migmatites of the Góry Sowie complex, 5) mylonites
Journal Article
Published: 30 September 2019
The Canadian Mineralogist (2019) 57 (5): 807-810.
...: the high-grade metamorphic complex of the Góry Sowie Block (GSB) in the west, interpreted as a fragment of the lower continental crust, and the Szklary serpentinite massif (SZM) in the east that is a part of the dismembered Central-Sudetic Ophiolite. Imprecise geochronometric data suggest that the Szklary...
FIGURES
Journal Article
Published: 01 February 2004
Clays and Clay Minerals (2004) 52 (1): 55-65.
... map of ultramafic massifs adjacent to the eastern and northern borders of the Góry Sowie Mts. Block (SW Poland). The sample from Szklary is a soft and brittle, bright green schist that is similar to garnierite as defined by Brindley and Hang (1973) . The coarse-grained fraction (ϕ >5 μm...
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Journal Article
Published: 01 August 2013
Mineralogical Magazine (2013) 77 (6): 2825-2839.
... pegmatites, having been reported from three other localities: Voron'i Tundry, Kola Peninsula, Russia (Voloshin et al. , 1977 ; 1987 ; Voloshin and Pakhomovskiy, 1988 ); Szklary, Lower Silesia, Poland ( Pieczka and Marszałek, 1996 ; Pieczka et al. , 2011 ), and Virorco, San Luis range, Argentina...
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