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| ABsrRAcr The Climax pegmatite of the Micanite district in Colorado contains unusually large masses of...discussed. IurnooucttoN The Micanite pegmatite district iies acrossthe Park-Fremont County line in south-centralColorado...rocks that include granitic gneiss, muscovite gneiss, siliimanite gneiss, mica schist, and biotite granite...grinding quality muscovite were obtained. Within the district ten major quarriesand prospectsare recorded(Fig...Colorado, showing location of the Micanite pegmatite district and the Climax deposit. cordierite, pinite, hematite |
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| 1007/s00710-016-0427-5 ORIGINAL PAPER The Blaník Gneiss in the southern Bohemian Massif (Czech Republic):...Czech Republic. The rocks, known locally as Blaník gneiss, are strongly peraluminous and classify as phosphorus-rich...origin and the abundance of tourmaline, the Blaník gneiss is exotic within the spectrum of Early Palaeozoic...Monotonous Group represent zones of higher and lower heat flow within the Early Palaeozoic northern Gondwana...Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg, Austria helpful for terrane correlations and palaeogeographic |
 | Klein, T., Kiehm, S., Siebel, W., Shang, C.K., Rohrmüller, J., Dörr, W., Zulauf, G. (2008) Age and emplacement of late-Variscan granites of the western Bohemian Massif with main focus on the Hauzenberg granitoids (European Variscides, Germany) Lithos, 102 (3) 478-507 doi:10.1016/j.lithos.2007.07.025 | Journal (article/letter/editorial) |
| Hauzenberg granitoids (European Variscides, Germany) T. Klein a,⁎, S. Kiehm b , W. Siebel c , C.K. Shang c , J...different timing of HT metamorphism in northern Austria and the Bavarian Forest is interpreted as being...E-mail addresses: T.Klein@em.uni-frankfurt.de (T. Klein), skiehm@web.de (S. Kiehm), wolfgang.siebel@uni-tuebingen...emplacement of numerous granitoid plutons. In the T. Klein et al. / Lithos 102 (2008) 478–507 Bohemian Massif...reported from the Moldanubian unit in Germany and Austria (see Section 5). We greatly benefited from prior |
 | Finger, F., Gerdes, A., Janoušek, V., René, M., Riegler, G. (2007) Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo-Moldanubian tectonometamorphic phases. Journal of GEOsciences, 52 (1-2) 9-28 | Journal (article/letter/editorial) |
| Mineralogy, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; Friedrich.Finger@sbg.ac.at University of Frankfurt...southwards into eastern Bavaria and western Upper Austria (Mühl and Sauwald Zone), but are difficult to identify...migmatitic orthogneisses (often summarized as Gföhl Gneiss). The latter have been interpreted as a retrogressed...been suggested recently for an occurrence of Gföhl Gneiss in Moravia (Hasalová et al. 2007). Traditionally...original Ostrong Unit as defined by Fuchs (1976) in Austria (Fig. 1) is a matter of debate. Areas mapped as |
 | Staude, S., Mordhorst, T., Neumann, R., Prebeck, W., Markl, G. (2010) Compositional variation of the tennantite–tetrahedrite solid-solution series in the Schwarzwald ore district (SW Germany): The role of mineralization processes and fluid source. Mineralogical Magazine, 74 (2) 309-339 doi:10.1180/minmag.2010.074.2.309 | Journal (article/letter/editorial) |
| tetrahedrite solidsolution series in the Schwarzwald ore district (SW Germany): The role of mineralization processes...(‘fahlore’) from 78 locations in the Schwarzwald ore district of SW Germany. Electron microprobe analysis is...typically As- and Bi-rich (up to 22.2 wt.% Bi). Gneiss-hosted fahlore formed by fluid cooling is Ag-rich...Ni-arsenides. Although they have similar compositions, gneiss-hosted fahlores show systematic variations in Ag...stratigraphic levels (North) and Zn- and Ag-rich fahlore in lower stratigraphic levels (South). We show that fahlore |
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| et al. 1982), Zambia (áèek Vrána 2002) and Austria (Ertl et al. 1997, Kalt et al. 2001). They are...gave T ~ 670 °C and P ~ 14 kbar for migmatitic gneiss. Anatexis producing kyanite-bearing leucosome was...whole outcrop, cuts massive migmatized biotite gneiss. The veinlet is locally folded, generally WNW-trending...about 1 cm thick, crosscutting the host biotite gneiss. Pegmatite veinlets of the AB-BBe subclass from...occurrences in the Gföhl Unit in the Czech Republic and Austria, and position of studied localities Starkoè (ST) |
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| Printed in Austria Petrophysical investigations in the Southern Bohemian Massif (Austria): data-acquisition...Institute of Geophysics, Mining University, Leoben, Austria With 15 Figures Received January 24, 1996; accepted...generation of granitoids can be separated from an older, Lower Carboniferous group of intrusives (Frasl and Finger...and dip of orientated sample code of municipal district (0sterr. Stat. Zentralamt) resistivity (f~m) induced...4-5). The research project "Pre-alpine crust in Austria" (S 47) includes new detailed mineralogic and petrographic |
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| Gilgen Windows Alps-The Hallein District I . Alps-The Hallein District II . Alps-The Lammertal and Gosau...7: Schieferhulle and Gneiss-lamellae of the Molltal ... Day 8: The Central Gneiss Day 9: Altkristallin...eiss-lamella (4) at Raufen (Day 7) ... T he Central Gneiss nea r the Reisseck hut (Day 8) .. . The geology...Geologists' Association 1966 Field Meeting in Austria. The form of the orig inal Guide has been retained...of one of the numerous good tourist guides to Austria. The present Guide is intended for use in conjunction |
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| of the Riebeckite Gneiss from the Area near Gloggnitz in the Graywacke Zone of Austria With 3 text-figures...bestätigt diese Ansicht. Abstract The riebeckite gneiss occurring near Gloggnitz is the biggest of the...the 14 occurrences in the Graywacke Zone of Austria. This body occurs within the Silbersberg serie of the...the Graywacke Zone of Upper Eastalpine of Austria. The Silbersberg serie, together with the quartz porphyroids...the Noric Nappe (Norische Decke). The riebeckite gneiss shows a more or less concordant relation to the |
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| Novosedly Šebanov lda 20 km Český Krumlov Austria Mo N ath oli th České Budějovice Fig. 1...Mn-rich garnet–quartz rocks. 2. Geological setting gneiss and amphibolite, is assumed to be mainly Neoproterozoic...abundant layers of marble, calc-silicate gneiss, graphite gneiss, quartzite and amphibolite in addition...co-ordinates is given in Tab. 1. 3.1. Pacova hora quarry near Chýnov The Moldanubian Zone is a heterogeneous...al. 1995) and the Mesoproterozoic Dobra gneiss in Lower Austria (Gebauer and Friedl 1994; Friedl et al |
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| documented Devonian and low-grade metamorphosed Lower Palaeozoic basement (Grad et al. 2002). The Variscan...of dismembered Lower Cambrian to Lower Carboniferous sequences partly embedded in Lower Carboniferous...Collins et al. 2000; Seston et. al. 2000). The lower part of the Kaczawa succession, comprising Cambrian...Izera-Kowary Unit is composed mainly of the Upper Cambrian/Lower Ordovician (Borkowska et al. 1980; Oliver et al...the Izera/Kowary Granite Gneiss and Gneiss (equivalent to the Krkono~e Gneiss on the Czech side of the |
 | Chen, Yi-Xiang, Demény, Attila, Schertl, Hans-Peter, Zheng, Yong-Fei, Huang, Fang, Zhou, Kun, Jin, Qi-Zhen, Xia, Xiao-Ping (2020) Tracing subduction zone fluids with distinct Mg isotope compositions: Insights from high-pressure metasomatic rocks (leucophyllites) from the Eastern Alps. Geochimica et Cosmochimica Acta, 271. 154-178 doi:10.1016/j.gca.2019.12.025 | Journal (article/letter/editorial) |
| of samples from metagranite through transitional gneiss to leucophyllite in Hungary shows two trends in...values firstly decrease from -0.64‰ to -1.30‰ during gneiss formation, and then increase to 0.29‰ during leucophyllite...values firstly decrease from -0.29‰ to -0.89‰ during gneiss formation, and then remain constant during leucophyllite...leucophyllite formation. Two leucophyllites in Austria exhibit higher 26Mg values of 0.05 to 0.09‰ compared...the Austroalpine basement, which belong to the Lower Austroalpine nappes (Kisházi and Ivancsics 1985; |
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| Salzburg, Hellbrunnerstrasse 34, A-5020 Salzburg, Austria Received February 12, 1993 / Accepted May 3, 1993...Bohemian Batholith; quarry at Gloxwald near Waldhausen, southcastern M/ihlviertel, Upper Austria Biptite-(monzo)granite;...Bohemian Batholith; quarry at Plochwald near Sandl, northeastern Miihlviertel, Upper Austria Biotite ( _+muscovite)...on the Danube, southwestern Mfihlviertel, Upper Austria Biotite-hornblende-granodiorite; coarse-grained...Batholith; quarry at Aalfang near Heidenreichstein, northwestern Waldviertel, Lower Austria Biotite-muscovite-granite; |
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| Mountains: BK Brennberg, Kovács árok; OQ Oromveg Quarry; Br Brennberg; V€o V€or€oshid; SR SR-1 borehole;...Deákkut; Vá Váris; Kh Kopháza; VQ Vashegy Quarry Argon and fission track dating 193 Variscan...the same crystalline slab (sometimes in the same quarry) a completely Alpine mineral paragenesis was formed...are related to the ‘‘Grobgneis’’ series of the Lower Austroalpine nappe complex. The crystalline schists...schists are mostly made up of orthogneisses (Sopron Gneiss Formation, SGF) and mica schists (Sopron Micaschist |
 | Kobayashi, Tomoyuki, Hirajima, Takao, Kawakami, Tetsuo, Svojtka, Martin (2011) Metamorphic history of garnet-rich gneiss at Ktiš in the Lhenice shear zone, Moldanubian Zone of the southern Bohemian Massif, inferred from inclusions and compositional zoning of garnet. Lithos, 124 (1) 46-65 doi:10.1016/j.lithos.2010.11.003 | Journal (article/letter/editorial) |
| l i t h o s Metamorphic history of garnet-rich gneiss at Ktiš in the Lhenice shear zone, Moldanubian...equilibrium stages were identified from garnet-rich gneiss at Ktiš in the Lhenice shear zone of the southern...located outside of higher-Grs (Xgrs = 0.27)- and lower-Prp (Xprp = 0.03)-content contours. These observations...bodies surrounded by the Gföhl granulite/ migmatitic gneiss, which has no HP/UHP evidence in their matrix,...Wang et al., 1989; Zhang et al., 1995; Western Gneiss Region in Norway: Smith, 1988; Wain, 1997). Petrological |
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| . . . . . . . Bohemia (Central), JOK~LY on the Gneiss and Granite of . . . . . . . . BR~ITHAUPT. On a... . . . . . . . . . . . . . . . Fossil Fish of Austria, HECKEL on the . . . . . . . . . . . . . . . ....North-Eastern part of Carinthia, LIPOLD on the . . . . . . Gneiss and Granite of Central Bohemia, JOK~LY on the ...e r Austria, HINGERAU on the Lignites of the . . . . . . IIECKEL. On the Fossil Fish of Austria . . ...HIN6ERAU. On the Lignites of the Hausruck, Upper Austria . . . . HOCHST~.TT~R. On the Geology of the Environs |
 | Kröner, A., O'Brien, P. J., Nemchin, A. A., Pidgeon, R. T. (2000) Zircon ages for high pressure granulites from South Bohemia, Czech Republic, and their connection to Carboniferous high temperature processes. Contributions to Mineralogy and Petrology, 138 (2) 127-142 doi:10.1007/s004100050013 | Journal (article/letter/editorial) |
| clinopyroxene. A further high temperature overprint at lower pressure (ca. 4 kbar) is re¯ected in the development...prevalent. These conditions can be those of a stable lower crustal geotherm or, alternatively, those attained...information pertaining to conditions and processes in the lower continental crust. The most voluminous of the scattered...bodies, like their counterparts in neighbouring Lower Austria, comprise part of the GfoÈhl Unit, the tectonically...contains a polydeformed, migmatitic, granitic gneiss (GfoÈhl gneiss, probably overprinted granulite) and variegated |
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| Wechsel and Molz Valley Areas (Semmering Window), Lower Austria With 1 plate, 18 figures and 2 tables By A....and Long. 15° 56' and 16° 0 1 ' East, in the Lower Austria (NiederÖsterreich). It is bounded to the north...metamorphic rocks belonging to two major series, Grob Gneiss serie and Wechsel serie, account for the most of...the two above series is that they belong to the Lower East Alpine elements of the Central Alpine zone...work is carried out at the Geological Survey of Austria and at the Petrographic Institute of the University |
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| coupled with decrease of Na and Fe contents from the gneiss to the leucophyllite. Minor elements and REE do...observation of gradual mineralogical changes from the gneiss to the leucophyllite. The metasomatic origin was...1985 a, 1987, 1989) belonging to the Grob gneiss unit of the Lower Austroalpine nappe-system. Draganits (1998)...metamor- 4 K. Török phism was recorded in the Lower Austroalpine Unit in the eastern end of the Eastern...fluid inclusions. Gradual alteration of the host gneiss towards the leucophyllite-bearing shear zones was |
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| discovery in 1967 of the Felbertal deposit in Austria, currently now the world's 3rd biggest tungsten...scheelite deposits in Australia (Mt. Isa district, Qld.; Broken Hill district, N.S.W.; Olary Block, S.A.; Yilgarn...occurred in Precambrian regional calc-silicate gneiss and amphibolite, this association of two principal...herein are throughout regionally metamorphosed Lower-Middle Proterozoic calc-silicate horizons which...Austroalpine Crystalline Complex (Eastern Alps, Austria) in carbonaceous pelitic, psammopelitic, psammitic |
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| muscovite – plagioclase – quartz and crosscutting gneiss veins were studied in the Sopron Mountains near...textural domains from both the micaschist and the gneiss veins. Thermobarometry of subsequent garnet generations...orthogneisses of the area. Gneiss veins crosscutting the micaschist show slightly lower peak pressures between...words: high-pressure metamorphism, micaschist, gneiss vein, geothermobarometry, P –T path. Introduction...Draganits 1998) and form the easternmost outcrop of the Lower Austroalpine Unit (Fig. 1 a). The reconstruction |
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| or rutile. Concurrent reactions in calc-silicate gneiss interbands resulted in replacement of diopside...Variegated Unit comprises 9 samples from the Pilát quarry near Sobìslav 10 59.98 0.90 18.93 0.75 3.98 0...environment of Èeský Krumlov, including a calc-silicate gneiss. This set was compared with two sets of paragneisses...paragneisses, with quartzite and calc-silicate gneiss intercalations, forms northwestern roof of the...47 T a b l e 3 . Location of muscovite-biotite gneiss samples from the Kaplice Unit. Sample No. 1 2 3 |
 | Putz, H., Paar, W.H., Topa, D., Horner, J., L�ders, V. (2003) Structurally controlled gold and sulfosalt mineralization: the Altenberg example, Salzburg Province, Austria. Mineralogy and Petrology, 78 (1) 111-138 doi:10.1007/s00710-002-0230-3 | Journal (article/letter/editorial) |
| mineralization: the Altenberg example, Salzburg Province, Austria H. Putz1 , W. H. Paar1, D. Topa1 , J. Horner2,...Mineralogie, Universit€at Salzburg, Austria RECON-STRUCT Geologic Consulting, Austria 3 GeoForschungsZentrum Potsdam...Formation and in the underlying Variscan Central gneiss. During the Alpine otogeny both lithologies were...‘‘Tauerngoldgang’’ type occur within the Central gneiss. Three different marble-hosted ore types following...C mean) for the second stage within the Central gneiss and temperatures between 310 and 230 C for the |
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| Montanuniversität Leoben, Peter-Tunner-Straße 5, 8700 Leoben, Austria Am 11. April 2014 fand an der Montanuniversität...pegmatitic melts. In particular, fluxes considerably lower melt viscosity and solidus temperature, allowing...pegmatitic melt. Solubility products are systematically lower where both minerals are dissolved together compared...Montanuniversität Leoben, Peter-Tunner-Straße 5, 8700 Leoben, Austria Abstract The occurrence and chemistry of Nb-Ta...columbite-tantalite and tapiolite. Zr/Hf ratios in wodginite are lower (1 to 4) than in coexisting columbite-tantalite |
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| 1996 / Accepted: 24 February 1997 Abstract The lower Austroalpine orthogneiss-micachist complex of the...isocon plots with Mg-enrichment even in sheared gneiss not in contact with leucophyllite. The metasomatic...about the metasomatic alteration of the overlying gneiss-micaschist complexes. Introduction A. DemeÂny...macroscopic appearance is what would be expected for a lower grade equivalent, they are usually formed in (or...(or associated with) shear zones in micaschist-gneiss complexes, they are strongly enriched in Mg compared |
