A New Evaluation of Fluid Inclusion Data Based on Thermal Basin Modeling for the Drau Range, Eastern Alps
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Geological Excursion BASE-Line Earth
Geological Excursion BASE-LiNE Earth (Graz Paleozoic, Geopark Karavanke, Austria) 7.6. – 9.6. 2016 Route: 1. Day: Graz Paleozoic in the vicinity of Graz. Devonian Limestone with brachiopods. Bus transfer to Bad Eisenkappel. 2. Day: Visit of Geopark Center in Bad Eisenkappel. Walk on Hochobir (2.139 m) – Triassic carbonates. 3. Day: Bus transfer to Mezica (Slo) – visit of lead and zinc mine (Triassic carbonates). Transfer back to Graz. CONTENT Route: ................................................................................................................................... 1 Graz Paleozoic ...................................................................................................................... 2 Mesozoic of Northern Karavanke .......................................................................................... 6 Linking geology between the Geoparks Carnic and Karavanke Alps across the Periadriatic Line ....................................................................................................................................... 9 I: Introduction ..................................................................................................................... 9 II. Tectonic subdivision and correlation .............................................................................10 Geodynamic evolution ...................................................................................................16 Alpine history in eight steps ...........................................................................................17 -
Hummocky Karren Lukas Plan1, Christa Renetzeder2, Rudolf Pavuza3, and Wilfred Körner4
International Journal of Speleology 41 (1) 75-81 Tampa, FL (USA) January 2012 Available online at scholarcommons.usf.edu/ijs/ & www.ijs.speleo.it International Journal of Speleology Official Journal of Union Internationale de Spéléologie A new karren feature: hummocky karren Lukas Plan1, Christa Renetzeder2, Rudolf Pavuza3, and Wilfred Körner4 Abstract: Plan L., Renetzeder C., Pavuza R. and Körner W. 2012. A new karren feature: hummocky karren. International Journal of Speleology, 41(1), 75-81. Tampa, FL (USA). ISSN 0392-6672. http://dx.doi.org/10.5083/1827-806X.41.1.8. Karren are small-scale landforms on karst surfaces and many types have been described so far. Here we present an apparently new feature which was found on the Hochschwab karst massive in the Northern Calcareous Alps of Austria. So far only few outcrops each having less than 1 m² within a very restricted area have been found. Morphometric analysis reveals that the karren consist of a randomly distributed, dispersed assemblage of small hummocks and depressions in between. The mean distance between neighbouring hummocks is 4 to 5 cm and the mean height is 0.85 cm. Longitudinal sections are gently sinuous. The occurrences are delimited by thin soil cover with grassy vegetation and the karren continue below that vegetation cover. Therefore, it is clear that the features have formed subcutaneously. Corroded fissures where water could infiltrate into the epikarst are absent. The bedrock lithology is Middle Triassic limestone of the Wetterstein Formation in lagoonal facies. Geological structures do not govern the feature. The surface is not a bedding plane and small joints and fractures do not govern the arrangement of the hummocks. -
75 the Upper Triassic Events Recorded in Platform and Basin of the Austrian Alps. the Triassic/Jurassic GSSP and Norian/Rhaetian
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt (ISSN 1017-8880), Band 111, Wien 2015 STRATI 2015 The Upper Triassic events recorded in platform and basin of the Austrian Alps. The Triassic/Jurassic GSSP and Norian/Rhaetian GSSP candidate Sylvain Richoz & Leopold Krystyn 47 figures Sylvain Richoz - Institute of Earth Sciences, Graz University, Heinrichstraße 26, 8010 Graz, Austria, [email protected] Leopold Krystyn - Department for Palaeontology, Vienna University, Geozentrum, Althansstr. 9, A-1090 Vienna, Austria; [email protected] Contents Abstract 1. Topics and area of the Field Trip 2. Introduction 2.1. The Northern Calcareous Alps 2.2. Principles of the structural evolution 2.3. Triassic depositional realms 2.3.1. General features 2.3.2. The Dachstein Mountains 2.3.3. The Zlambach facies – the deep shelf environment 2.3.4. The Hallstatt facies – the condensed deep shelf environment 2.3.5. The Eiberg Basin 3. The Field Trip 3.1. Shelf margin (Day 1) 3.1.1. Route 3.1.2. Locality 1 – Pötschenhöhe Quarry 3.1.3. Locality 2 – Großer Zlambach 3.1.4. Locality 3 – Steinbergkogel: Proposed Norian/Rhaetian GSSP section 3.1.5. Locality 4 – Gosausee: The Dachstein margin at Gosaukamm 3.2 Lagoon, fringing reef and Eiberg Basin (Day 2) 3.2.1. Route 3.2.2. Locality 5 – Pass Lueg: The classical Lofer cycle 3.2.3. Locality 6 – Adnet 3.2.4. Locality 7 – Steinplatte 3.2.5. Locality 8 – Eiberg 3.3. The Triassic/Jurassic GSSP (Day 3) 3.3.1. -
Jahrbuch Der Geologischen Bundesanstalt
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Jahrbuch der Geologischen Bundesanstalt Jahr/Year: 2018 Band/Volume: 158 Autor(en)/Author(s): Schönlaub Hans-Peter Artikel/Article: Review of the Devonian/Carboniferous boundary in the Carnic Alps 29- 47 JAHRBUCH DER GEOLOGISCHEN BUNDESANSTALT Jb. Geol. B.-A. ISSN 0016–7800 Band 158 Heft 1–4 S. 29–47 Wien, Dezember 2018 Review of the Devonian/Carboniferous boundary in the Carnic Alps HANS P. SCHÖNLAUB* 16 Text-Figures Österreichische Karte 1:50.000 Italy BMN / UTM Carnic Alps 197 Kötschach / NL 33-04-09 Oberdrauburg Devonian 197 Kötschach / NL 33-04-10 Kötschach-Mauthen Carboniferous Conodonts Hangenberg Crisis Contents Abstract ................................................................................................ 29 Zusammenfassung ........................................................................................ 30 Current knowledge ........................................................................................ 30 Review of sedimentary and tectonic history ..................................................................... 32 Important stratigraphic markers .............................................................................. 32 Middle and Upper Ordovician ............................................................................. 32 Silurian .............................................................................................. 32 Devonian............................................................................................ -
Age and Evolution of the Wetterstein Carbonate Platform in SW Serbia (Zlatibor Mountain)
Further research is necessary to understand the relationship between the gold-bearing mineralizations and their settings. Age and evolution of the Wetterstein Carbonate Platform in SW Serbia (Zlatibor Mountain) Missoni S.1, Sudar M.N.2, Gawlick H.-J.1, Jovanović D.3 and Lein R.4 1University of Leoben, Department for Applied Geosciences and Geophysics, Prospection and Applied Sedimentology, Peter-Tunner-Strasse 5, 8700 Leoben, Austria, [email protected]; [email protected] 2University of Belgrade, Faculty of Mining and Geology, Department of Palaeontology, Đušina 7, P.O. Box 62, 11000 Belgrade, Serbia, [email protected] 3Geological Institute of Serbia, Rovinjska 12, 11000 Belgrade, Serbia, [email protected] 4University of Vienna, Centre for Earth Sciences, Althanstrasse 14, 1090 Vienna, Austria, [email protected] Triassic shallow- and deep-water carbonates occur together with Triassic radiolarites widespread as olistoliths and slides in the Middle to early Late Jurassic mélange of the Dinaridic Ophiolite Belt in the Zlatibor Mountain. These slides occur tectonically on top of the Drina-Ivanjica Palaeozoic and the late Middle to early Late Jurassic ophiolitic mélange respectively the ophiolites and not below as interpreted before. These slides were interpreted to derive from the Drina-Ivanjica Unit, where they should have formed the original sedimentary cover, disintegrated in the Late Jurassic. According to our investigations the slides of this carbonate-clastic mélange differ in age, facies and palaeogeographic origin. The carbonate rocks are originated from a relatively broad shelf in the Triassic facing the Neotethys Ocean to the east, maybe also from the adjacent Drina-Ivanjica Unit and from further east. -
Dasycladaceen-Assoziationen Aus Triadischen Seichtwasserkarbonaten Des Ostabschnittes Der Nördlichen Kalkalpen
Jubiläumsschrift 20 Jahre Geologische Zusammenarbeit A 20 eves magyar-osztrak Österreich - Ungarn földtaniegyüttmüködesjubileumi kötete Redaktion: Harald Lobitzer, GezaCsäszär& Albert Daurer Szerkesztette: Lobitzer Harald, Csäszär Geza & Daurer Albert Teil 2 S. 343-362 Wien, November 1994 2. resz pp.343-362 Bees, 1994. november ISBN 3-900312-92-3 Dasycladaceen-Assoziationen aus triadischen Seichtwasserkarbonaten des Ostabschnittes der Nördlichen Kalkalpen Von OLGA PIROS, GERHARD W. MANDL, RICHARD LEIN, WOLFGANG PAVLIK, ANIKÖ BERCZI-MAKK, MILOS SIBLIK & HARALD LOBITZER*) Mit 4 Abbildungen und 3 Tafeln Österreich Steiermark Niederösterreich Nördliche Kalkalpen Trias Seichtwasserkarbonate Steinalmkalk Wettersteinkalk Waxeneckkalk Dachsteinkalk Dasycladaceen Foraminiferen Brachiopoden Österreichische Karte 1:50.000 Mürzalpendecke Blätter 74, 75, 76, 103, 104, 105 Schneebergdecke Inhalt Zusammenfassung 344 Összefoglaläs 344 Abstract 344 1. Einleitung 344 2. Steinalmkalk (Anis) 345 2.1. Türnitzer Kalkvoralpen 345 2.2. Östliche Kalkhochalpen 345 2.2.1. HoherStudent 345 2.2.2. Fallensteingruppe-Lärchsteinwand 347 2.2.3. Gösing- Dachenstein 348 3. Wetterstein kalk (Ladin bis Unterkam) 348 3.1. Kalkhochalpine Fazies mit Teutloporella herculea 349 3.1.1. Derstratigraphische Rahmen des Rax-und Schneeberggebietes 349 3.1.2. Faziesgliederung und Organismenverteilung der Plattformkarbonate 351 3.1.2.1. Dasycladaceen 351 3.1.2.2. Foraminiferen 351 3.1.2.3. Brachiopoden 352 4. Waxeneckkalk (Kam) 352 5. Dachsteinkalk (Nor-Rhät) 352 Dank 353 Tafeln 1-3 354 Literatur 360 Anschriften der Verfasser: Dr. OLGA PIROS, Ungarische Geologische Landesanstalt, Stefänia üt 14, H-1442 Budapest; Dr. GERHARD W. MANDL, Dr. WOLFGANG PAVLIK, Dr. HARALD LOBITZER, Geologische Bundesanstalt, Rasumofskyg. 23, A-1031 Wien; Univ.-Doz.Dr. RICHARD LEIN, Universität Wien, Geologisches Institut, Universitätsstraße 7/III, A-1010 Wien; Dr. -
Field Trip 8 Innsbruck´S Geology in a Nutshell: from the Hafelekar to the Hötting Breccia 215-228 Geo.Alp, Vol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Geo.Alp Jahr/Year: 2016 Band/Volume: 013 Autor(en)/Author(s): Krainer Karl, Meyer Michael Artikel/Article: Field trip 8 Innsbruck´s geology in a nutshell: from the Hafelekar to the Hötting Breccia 215-228 Geo.Alp, Vol. 13 2016 215 - 228 Field trip 8 Innsbruck´s geology in a nutshell: from the Hafelekar to the Hötting Breccia Karl Krainer1 and Michael Meyer1 1 Institute of Geology, University of Innsbruck, Innrain 52, 6020 Innsbruck 1 Introduction Alpen, southwest of Innsbruck Stubaier Alpen and north of Innsbruck Karwendel as part of the Hafelekar Spitze provides an excellent panora- Northern Calcareous Alps. mic overview of the main geologic units around The excursion starts at the cable railway station Innsbruck. The city of Innsbruck is located on an Hungerburgbahn next to the Innsbruck Congress alluvial fan which was formed by the Sill river at Centre (Fig. 1). The Hungerburgbahn will bring us its confluence with the Inn river. The mountain onto the Hungerburg terrace (868 m), from there group southeast of Innsbruck is termed Tuxer we continue with a cablecar (Seegrubenbahn ) to Fig. 1: Map showing excursion route to Hafelekar Spitze (Wetterstein Reef Complex) and Hungerburg – Alpenzoo (Hötting Breccia). 215 Figure 1 Seegrube (1905 m) and ascend Hafelekar (2260 m) composed of the famous Höttinger Breccie (see . via a second cablecar. From the top station of the excursion route part 2 – the Hötting Breccia) Hafelekarbahn the excursion route follows the The Valley which extends from Innsbruck to the trail to Hafelekar Spitze and continues East where Brennerpass in the south (Silltal-Wipptal) repre- the trail meets the Goetheweg, one of the most sents a big west-dipping normal fault (Brenner spectacular panoramic trails around Innsbruck. -
Official Journal C 195 of the European Union
Official Journal C 195 of the European Union Volume 61 English edition Information and Notices 7 June 2018 Contents I Resolutions, recommendations and opinions RECOMMENDATIONS Council 2018/C 195/01 Council Recommendation of 22 May 2018 on promoting common values, inclusive education, and the European dimension of teaching ........................................................................................ 1 II Information INFORMATION FROM EUROPEAN UNION INSTITUTIONS, BODIES, OFFICES AND AGENCIES European Commission 2018/C 195/02 Non-opposition to a notified concentration (Case M.8887 — Platinum Equity/LifeScan) (1) ................ 6 2018/C 195/03 Non-opposition to a notified concentration (Case M.8771 — Total/Engie (Part of Liquefied Natural Gas Business)) (1) .................................................................................................................. 6 EN (1) Text with EEA relevance. IV Notices NOTICES FROM EUROPEAN UNION INSTITUTIONS, BODIES, OFFICES AND AGENCIES Council 2018/C 195/04 Council conclusions on moving towards a vision of a European Education Area .............................. 7 2018/C 195/05 Council conclusions on the role of young people in building a secure, cohesive and harmonious society in Europe ............................................................................................................................... 13 European Commission 2018/C 195/06 Euro exchange rates ............................................................................................................. -
Nota Lepidopterologica
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Nota lepidopterologica Jahr/Year: 2010 Band/Volume: 33 Autor(en)/Author(s): Cupedo Frans Artikel/Article: A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) 85-106 ©Societas Europaea Lepidopterologica; download unter http://www.biodiversitylibrary.org/ und www.zobodat.at Nota lepid.33 (1): 85-106 85 A revision of the infraspecific structure of Erebia euryale (Esper, 1805) (Nymphalidae: Satyrinae) Frans Cupedo Processieweg 2, NL-6243 BB Geulle, Netherlands; [email protected] Abstract. A systematic analysis of the geographic variation of both valve shape and wing pattern reveals that the subspecies ofErebia euryale can be clustered into three groups, characterised by their valve shape. The adyte-group comprises the Alpine ssp. adyte and the Apenninian brutiorum, the euryale-group in- cludes the Alpine subspecies isarica and ocellaris, and all remaining extra- Alpine occurrences. The third group (kunz/-group), not recognised hitherto, is confined to a restricted, entirely Italian, part of the south- ern Alps. It comprises two subspecies: ssp. pseudoadyte (ssp. n.), hardly distinguishable from ssp. adyte by its wing pattern, and ssp. kunzi, strongly melanistic and even exceeding ssp. ocellaris in this respect. The ssp. pseudoadyte territory is surrounded by the valleys of the rivers Adda, Rio Trafoi and Adige, and ssp. kunzi inhabits the eastern Venetian pre-Alps, the Feltre Alps and the Pale di San Martino. The interven- ing region (the western Venetian pre-Alps, the Cima d'Asta group and the Lagorai chain) is inhabited by intermediate populations. -
Abstracts & Field Guides
Berichte der Geologischen Bundesanstalt, 99 11th Workshop on Alpine Geological Studies & th 7 European Symposium on Fossil Algae Abstracts & Field Guides Schladming, Sept. 2013 Redaktion: Ralf Schuster Cover image: Sölk marble from the base of the Weiße Wand, Walchental (Styria, Austria) Impressum: ISSN 1017-8880 Alle Rechte für das In- und Ausland vorbehalten © Geologische Bundesanstalt (GBA) A-1030 Wien, Neulinggasse 38 www.geologie.ac.at Wien, September 2013 Medieninhaber, Herausgeber und Verleger: GBA, Wien Redaktion: Ralf Schuster (Geologische Bundesanstalt) Technische Redaktion; Christoph Janda (Geologische Bundesanstalt) Umschlag Monika Brüggemann-Ledolter Druck: Riegelnik, Offsetschnelldruck, Piaristengasse 19, A-1080 Wien Ziel der „Berichte der Geologischen Bundesanstalt“ ist die Verbreitung wissenschaftlicher Ergebnisse durch die Geologische Bundesanstalt. Die „Berichte der Geologischen Bundesanstalt“ sind im Handel nicht erhältlich. Berichte Geol. B.-A., 99 11th Workshop on Alpine Geological Studies & 7th IFAA Content Organisation & Time Schedule 4 Abstracts Emile Argand Conference (11th Workshop on Alpine Geological Studies) Editorial: Ralf Schuster 9 Abstracts 7th European Symposium on Fossil Algae Editorial: Sigrid Missoni & Hans-Jürgen Gawlick 107 Field guide: General Introduction in the Geology of the Easter Alps Ralf Schuster 121 Field guide Excursion A1: Southern Alps of Slovenia in a nutshell: paleogeography, tectonics, and active deformation Bogomir Celarc, Marko Vrabec, Boštjan Rožič, Polona Kralj, Petra Jamšek Rupnik, -
Facies and Sedimentary Environments of the Upper Scythian–Carnian
Annales Societatis Geologorum Poloniae (2005), vol. 75: 155-169. FACIES AND SEDIMENTARY ENVIRONMENTS OF THE UPPER SCYTHIAN-CARNIAN SUCCESSION FROM THE BELANSKE TATRY MTS., SLOVAKIA Tomasz RYCHLIŃSKI & Joachim SZULC Institute o f Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Krakow, Poland; e-mail: [email protected], [email protected] Rychliński, T. & Szulc, J., 2005. Facies and sedimentary environments of the Upper Scythian-Camian succession from the Belanske Tatry Mts., Slovakia. Annales Societatis Geologorum Poloniae, 155-169. Abstract: The Triassic Fatricum basin studied in the Belanske Tatry Mts. (Slovakia) was a relatively stable and restricted platform area influenced by eustatic and climatic fluctuations. During the early Triassic the platform was influenced by continental clastic sedimentation intermittent with shallow marine transgressions when carbonate sediments formed. Common occurrence of carbonized plat debris suggests relatively humid climatic conditions dominating during this interval (Werfenian facies). Significant climate aridisation was concurrent with the beginning of the Middle Triassic transgression as indicated by evaporitic fabrics common within the entire Middle Triassic carbonate succession. The Middle Triassic has been divided into several lithofacies complexes reflecting the interplays between the eustatic and climatic fluctuations. The lower Middle Triassic complex (lower-middle Anisian?) displays dominance of calcareous sediments indicating free communication with the open ocean. The subsequent intervals are rather uniform facies assemblage composed by dolomites and evaporites formed in a restricted and stagnant basin. The basin has been strongly influenced by subtropical storms, particularly common in the late Anisian. Transgression pulse in the early Ladinian involved growth of microbial colonies building thrombolitic biostromes. Final shallowing by the end of Ladinian led to replacement of carbonate sediments by continental clastics of the Carpathian Keuper. -
Geology of the Eastern Alps (An Excursion Guide) 103-170 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 1980 Band/Volume: 34 Autor(en)/Author(s): Matura Alois, Summesberger Herbert Artikel/Article: Geology of the Eastern Alps (An Excursion Guide) 103-170 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Abh. Geol. B.-A. 34 p. 103—170 52 figs., 10 tables 26" C. G. I. Wien 1. 5. 1980 International Geological Congress 26tl) Session Excursion 034 A Geology of the Eastern Alps (An Excursion Guide) - by ALOIS MATURA and HERBERT SUMMESBERGER with contributions from ALOIS FENNINGER, WOLFGANG FRISCH, VOLKER HOCK, HEINZ KOLLMANN, ARTHUR KRÖLL, OTTO MALZER, JULIAN PISTOTNIK, BENNO PLÖCHINGER, ALFRED RÖGL, REINHARD ROETZEL, WOLFGANG SCHNABEL, HANS PETER SCHÖNLAUB and GODFRID WESSELY. 52 figures and 10 tables Address of the authors: Dr. ALOIS MATURA, Geologische Bundesanstalt, A-1031 Wien, Rasumofskygasse 23; Dr. HERBERT SUMMESBERGER, Naturhistorisches Museum Wien, A-1014 Wien, Burgring 7. ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at 4 03 N RSIO Z> H p uX w t < LU ^ h LL LL h- Q ~ r r t O U 3 ve ou LU XC < H ir LU U U \ • D RO ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at Acknowledgments drillings we know that the Molasse sediments continue The authors express their gratitude to F. FLIRI, D. VAN far below the Eastern Alps towards south. The crystal HUSEN, G. NIEDERMAYR, R. OBERHAUSER, A. RÖGL and line complex of the Bohemian Massif with a thin Palaeo A. TOLLMANN for their constructive comments.