The Koralm Connection
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The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Mitteilungen des naturwissenschaftlichen Vereins für Steiermark Jahr/Year: 2005 Band/Volume: 134 Autor(en)/Author(s): Sölva Helmuth, Stüwe Kurt, Strauss Phillip Artikel/Article: The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions. 45-55 © Naturwissenschaftlicher Verein für Steiermark; download unter www.biologiezentrum.at Mitt. naturwiss. Ver. Steiermark Band 134 S. 45–55 Graz 2005 The Drava River and the Pohorje Mountain Range (Slovenia): Geomorphological Interactions By Helmuth Sölva 1, Kurt Stüwe1 & Phillip Strauss2 With 6 figures Accepted on November, 16th, 2004 Zusammenfassung: Die Drau und das Bacher Gebirge in Slowenien: Geomorphologische Zusammenhänge. − In dieser geomorphologisch-tektonischen Studie untersuchen wir die domartige Struktur des slowenischen Bacher Gebirges (Pohorje) und seine Interaktion mit einem der bedeutendsten Flüsse der Alpen, der Drau. Geologisch befindet sich das Bacher Gebirge am südwestlichen Rand des steirischen Beckens und nahe einer tektonisch sehr aktiven Zone der Europäischen Alpen: das Periadri- atische Lineament. Etwa 10 km nordwestlich des Bacher Gebirges verlässt die Drau das Miozän-Pliozäne Klagenfurter Becken und verändert ihre Fliessrichtung von Ost nach Süd, der Lavanttal/Labot-Störung folgend. Am Nordwesteck der Antiform des Bacher Gebirges wird die Drau wieder in eine Ost-Richtung abgelenkt, anstatt dem tektonischen und geomorphologischen Lineament der Lavanttal-Störung weiter nach SE zu folgen. Ab diesem Knick fliesst die Drau parallel zur Längsachse durch den Dom nach Osten. Ge- omorphologische und sedimentologische Hinweise zeigen, dass das Flusstales der Drau im zentralen Bereich des Gebirges um 1 km nach Norden an seine heutige Position verlagert worden ist. -
Complex Segment Monitoring at Koralm Tunnel
TJ_0513_OUTSIDE_FNT_COVER_PLUS_SPINE_001.qxd:cover 22/4/13 20:22 Page 1 www.tunnellingjournal.com April/May 2013 TTheunne international journal for the tunnelling industry llingjournal SEE PAGE 18 SEE PAGE 34 SEE PAGE 40 SEGMENTAL PROJECT JUBILEE INNOVATION POLITICS REPAIRS TJ LOOKS AT NEW THE COMPLEX A FASCINATING TECHNOLOGIES WORLD OF INSIGHT INTO AVAILABLE TO THE PROJECT POLITICS AN INTRIGUING SEGMENTAL LINING EXAMINED GROUTING SECTOR PROBLEM TUNNELLING JOURNAL SEGMENTAL LININGS IN FOCUS APRIL/MAY 2013 APRIL/MAY THE KORALM’S SEGMENT TRACKING SYSTEM TJ_0513_KORALM_010_016.qxd:Feature 22/4/13 20:33 Page 10 SEGMENTAL LINING The Koralm Project at a glance Austria's new Koralm tunnel is one of the the west and the harder gneiss of the largest infrastructure projects in Europe outside mountains. Strabag did that work in 2005-07, of the three great Alpine pass crossings at making a small 45m2 cross-section bore. Brenner, the Swiss Gotthard and France's Fréjus. “It was thought this might be a difficult area At just under 33km long and with a maximum but in the end it was more straightforward than cover of nearly 1200m it is at least approaching thought,” says Lehner. the same kind of scale. The interface fixes two different types of The twin bores for high-speed rail trains will tunnelling for the project which uses form a critical link through Klagenfort in conventional excavation in hard clays to the southern Austria and on to the north east via west and switches to TBM for the longer hard Graz and Vienna. Another major tunnel, the rock. -
Koralm Tunnel
KORALM TUNNEL – DEVELOPMENT OF TUNNEL SYSTEM DESIGN AND SAFETY CONCEPT Christof Neumann, Florian Diernhofer, ILF Consulting Engineers, Austria Gerhard Harer, Josef Koinig, OEBB Infrastruktur Bau AG 1 ABSTRACT The 32.8-km-long Koralm tunnel requires additional measures to guarantee a sufficient safety level. The methodology applied to define safety measures for this very long tunnel is on the one hand based on a set of guidelines and on the other hand based on the specific boundary conditions of this tunnel. These tunnel-specific conditions are considered by establishing customized safety targets. As a result of an investigation into the construction and operating phase, the tunnel system was determined to consist of two single-tube tunnels, an emergency station, no crossover and cross- passages every 500 m. The emergency station in the centre of the tunnel, which incorporates various considerations, was designed to accommodate staggered platforms and a refuge room with a length of 800 m. With a view to the incident management strategy to be adopted, characteristic operating scenarios were analysed to realistically reflect the sequence of events in case of an emergency. 2 THE KORALM TUNNEL PROJECT The Koralm tunnel is one of the key elements of the Koralm high-capacity railway line, which connects the cities of Graz and Klagenfurt in the south of Austria. The Koralm railway line is part of the Baltic-Adriatic Axis, which represents the easternmost crossing of the Alps and links several Eastern European countries Koralm line with Koralm tunnel and Vienna with southern Austria and northern Italy. The Koralm line is a 130- km-long high-capacity railway line engineered for a design speed of 200 km/h. -
Documentation Austrian Wine 2006
DOCUMENTATION AUSTRIAN W INE 2006 Table of contents 1 Austria œ the wine country 1.1 Austria‘s wine-gr wing regi ns and wine-gr wing areas 1 1.2 Grape varieties in Austria 5 1.2.1 Breakd wn by share of area in percent 5 1.2.2 Grape varieties - Brief descripti n .1 1.2.. Devel pment f the area under cultivati n until 1111 .5 1.. Devel pment of the climate 1161-2002 .6 1.2 W ine-gr wers in Austria - A current overall view .1 1.5 The 2006 harvest 22 1.6 The 2005 vintage 25 1.3 Brief characterisati n of the vintages 2002 back t 1160 23 1.8 Assessment of the 2005-111. vintages 55 2 The Austrian wine industry 2.1 Ec n mic imp rtance of the wine industry in Austria 56 2.2 The harvest 2006 (Status Oct ber 20066 51 2.. 7arvests 1160-2005 61 2.2 8ualit9tswein (8uality wine6 in Austria 2005 65 2.5 Austria‘s wine supply 2005 68 2.6 Devel pment f grape and wine prices 31 2.3 General regulati ns f r wine pr ducti n 32 2.8 EU-Measures f r the Restructuring and C nversi n of Vineyards 32 2.1 The Austrian W ine B ards 80 2.10 The :alue f Origin 8. 2.11 DAC: the l gical key t Austrian wine 82 2.12 8uesti ns and Answers - a Guide 86 3 The Austrian market ..1 C nsumpti n of D mestic Wine and Sparkling W ine 81 ..1.1 C nsumpti n of D mestic Wine 81 ..1.2 D mestic C nsumpti n f Sparkling Wine 1110-2005 10 ..1. -
Koralm, Railway Line, Wettmannstätten
SUBSOIL EXPLORATION•• GEOMECHANICS GEOHYDROLOGY Prof. DI Dr. techn. Peter Waibel, State Certified Civil Engineer KORALM,GRAZ - KLAGENFURT RAILWAY LINE, WETTMANNSTÄTTEN - ST. ANDRÄ SECTION Client: ÖBB-Infrastruktur Bau AG (Austrian Railways Infrastructure Construction AG) Development Period: since 1996 THE PROJECT OUR FUNCTION With the new Koralm Railway Line BGG was commissioned with the hydro- Paierdorf exploration shaft: between Graz and Klagenfurt, an geological and geotechnical workman- For this 120 m deep shaft, that has essential section of the european railway ship of the tertiary tunnel sections and already been completed, a particularly system will be implemented. open areas. During the planning phases intensive geological and hydrogeological Within the 43.8 km long Wettmann- (route selection, environmental impact supervision was essential during the stätten - St. Andrä section (the core of assessment, and the tender for the design and execution phases. This was the line) the Koralm Tunnel, with a length exploration structures), the following necessary due to the predominant of 32.8 km, is situated. tasks were carried out: subsoil and groundwater situation: The double-tube tunnel cuts through q Hydrogeological field mapping Granular soil, with varying grain sizes, polymetamorphic crystalline rock of the q Planning and handling of several and several groundwater storeys exist all Koralpe and has an overburden of up to subsoil exploration campaigns the way to the bottom of the shaft. 1,200 m. Near the tunnel entrances, q Interpretation of aerial photographs Already during the planning stage of the tertiary sediments of different grain sizes and geophysical investigations tender, BGG established a detailed and rock with minor strength exists. -
Fluid and Solid Inclusions in Host Minerals of Permian Pegmatites from Koralpe (Austria): Deciphering the Permian Fluid Evolution During Pegmatite Formation
minerals Article Fluid and Solid Inclusions in Host Minerals of Permian Pegmatites from Koralpe (Austria): Deciphering the Permian Fluid Evolution during Pegmatite Formation Kurt Krenn *, Martina Husar and Anna Mikulics NAWI Graz Geocenter, Institute of Earth Sciences, University of Graz, 8010 Graz, Austria; [email protected] (M.H.); [email protected] (A.M.) * Correspondence: [email protected] Abstract: Fluid inclusions (FIs) and associated solids in host minerals garnet, tourmaline, spodumene, and quartz from six pegmatite fields of Permian origin at Koralpe (Eastern Alps) have been investi- gated. Although pegmatites suffered intense Eoalpine high-pressure metamorphic overprint during the Cretaceous period, the studied samples originate from rock sections with well-preserved Permian magmatic textures. Magmatic low-saline aqueous FIs in garnet domains entrapped as part of an unmixed fluid together with primary N2-bearing FIs that originate from a host rock-derived CO2-N2 dominated high-grade metamorphic fluid. This CO2-N2 fluid is entrapped as primary FIs in garnet, tourmaline, and quartz. During host mineral crystallization, fluid mixing between the magmatic and the metamorphic fluid at the solvus formed CO2-N2-H2O–rich FIs of various compositional degrees Citation: Krenn, K.; Husar, M.; that are preserved as pseudo-secondary inclusions in tourmaline, quartz, and as primary inclusions Mikulics, A. Fluid and Solid in spodumene. Intense fluid modification processes by in-situ host mineral–fluid reactions formed a Inclusions in Host Minerals of high amount of crystal-rich inclusions in spodumene but also in garnet. The distribution of different Permian Pegmatites from Koralpe types of FIs enables a chronology of pegmatite host mineral growth (garnet-tourmaline/quartz- (Austria): Deciphering the Permian Fluid Evolution during Pegmatite spodumene) and their fluid chemistry is considered as having exsolved from the pegmatite parent Formation. -
Celotno Besedilo (Pdf)
Arheološki vestnik 70, 2019, 353–380 353 Poselitev doline reke Solbe v pozni bronasti in starejši železni dobi – nove raziskave graškega Joanneuma Settlements in the Sulm River valley during the Late Bronze Age and Early Iron Age – new research of the Universalmuseum Joanneum, Graz Marko MELE (prispevek / contribution: Branko Mušič, Barbara Horn) Izvleček Najdišče Kleinklein pri Großkleinu z okolico v dolini reke Solbe (Sulm) je že skoraj 175 let sinonim za eno najslav- nejših najdišč iz starejše železne dobe v Evropi. Najdbe, kot so bronasta maska in roke, zvončasti oklepi in bronaste posode s punciranim okrasom, sodijo med najpomembnejše eksponate arheološke zbirke v Joanneumu. Leta 2010 so sodelavci Joanneuma začeli nove raziskave arheološke krajine v porečju reke Solbe (Sulm), ki obsegajo analize lidarskih posnetkov in zračnih fotografij, geofizikalne raziskave, terenske izmere ter arheološka izkopavanja z arheobotaničnimi in arheozoološkimi analizami. V okviru teh raziskav so leta 2015 ob rigolanju na južnem pobočju Burgstallkogla pri Großkleinu odkrili in raziskali zgorelo ruševino stavbe iz starejše železne dobe. S tem odkritjem so pridobili nove podatke o načinu gradnje na Burgstallkoglu. Od leta 2017 se posvečajo raziskavam okoliške krajine, še posebej na približno 4,5 km zračne črte oddaljeni utrjeni naselbini na Königsbergu pri Heimschuhu. Ključne besede: Štajerska, Großklein, Kleinklein, Burgstallkogel, Königsberg, starejša železna doba, naselbine, gomile Abstract For almost 175 years, the site Kleinklein near Großklein in the valley of the Sulm River has been synonymous as one of the most famous sites from the Early Iron Age in Europe. The bronze mask and hands, bell-shaped armour, and figural decorated vessels with punctuation are masterpieces of the archaeological collection in the Joanneum, which has been conducting diverse research since the very discovery of the site. -
Bands at 465 Cm-1 Dia- Gnostic of Quartz
MITT.ÖSTERR.MINER.GES. 150 (2005) ECLOGITES FROM THE KORALPE AND SAUALPE TYPE-LOCALITIES, EASTERN ALPS, AUSTRIA by Ch. Miller1, M. Thöni2, J. Konzett1, W. Kurz3 & R. Schuster4 1Institute of Mineralogy and Petrography University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria 2Institute of Geological Sciences University of Vienna, Geocenter, Althanstrasse 14, 1090 Vienna, Austria 3Institute of Applied Geosciences University of Technology, Rechbauerstrasse 12, 8010 Graz, Austria 4Geological Survey of Austria Neulinggasse 38, 1030 Vienna, Austria 1. Geology of the Saualpe-Koralpe region The area of interest is located in the Carinthia and Styria districts of Austria. Geographically it is dominated by two approximately N-S oriented mountain ridges: (i) the westerly ridge of the Saualpe and Seetaler Alps and (ii) the Koralpe and Stubalpe ridge that continues north-eastwards into the Gleinalpe and south-eastwards into the Pohorje Mountains. These two ridges are separated by the Lavant valley. The terrain morphology is characterized by valleys and basins at altitudes between 500 and 700 m, and by gently sloping mountains up to 2150 m high. Outcrops are few and restricted to rocky cliffs (“Öfen”). The area is bordered to the east by the Styrian basin, to the north by the Knittelfeld basin, to the southeast by the Klagenfurt basin and to the west by the Gurktaler Alps. Tectonically the Saualpe-Koralpe region is an assembly of Austroalpine units (part of the Apulian microplate) with medium to high-grade metamorphic units, low-grade Paleozoic units with remnants of unmetamorphosed transgressive Permotriassic sediments in places, and unmeta- morphosed Upper Cretaceous sediments. According to the nomenclature of SCHMID et al. -
Tectonic Interpretation of the Metamorphic Field
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Austrian Journal of Earth Sciences Jahr/Year: 2018 Band/Volume: 111 Autor(en)/Author(s): Herg Alexandra, Stüwe Kurt Artikel/Article: Tectonic interpretation of the metamorphic field gradient south of the Koralpe in the Eastern Alps 155-170 download https://content.sciendo.com/view/journals/ajes/ajes-overview.xml Austrian Journal of Earth Sciences Vienna 2018 Volume 111/2 155 - 170 DOI: 10.17738/ajes.2018.0010 Tectonic interpretation of the metamorphic field gradient south of the Koralpe in the Eastern Alps Alexandra HERG*) & Kurt STÜWE Institute of Earth Sciences, University of Graz, Universitätsplatz 2, A-8010, Graz, Austria; *) Corresponding author: Alexandra Herg, [email protected] KEYWORDS Pohorje; Koralpe; slab extraction; Plattengneis-Plankogel shear zone Abstract In order to constrain tectonic models for the nature of the Eoalpine high pressure belt at the eastern end of the Alps, we investigate the formation pressure of metamorphic rocks along a profile between the Koralpe and the well-known UHP rocks of the southern Pohorje mountains. Rocks from three different regions are considered: (i) the rocks of the southernmost Koralpe to the north, (ii) the rocks of the Plankogel Unit between the Plankogel detachment and the Drava valley and (iii) the rocks between the Possruck range and the southern Pohorje mountains. In the Koralpe, pelitic rocks record a formation pressure around 15 – 18 kbar, as reported in the literature. For the Plankogel Unit, we derive pres- sures between 7.1 ± 1.95 kbar and 11.5 ± 3.42 kbar at 650 °C and recognize only a single Eoalpine metamorphic event. -
Celotno Besedilo (Pdf)
Arheološki vestnik 70, 2019, 319–334 319 Štajersko-panonska halštatska skupina. Uvodnik in kratek oris The Styrian-Pannonian Hallstatt Group. An introduction and brief outline Biba TERŽAN Izvleček Štajersko-panonska skupina je značilna predstavnica vzhodnohalštatskega kulturnega kroga. Pod tem terminom razu- memo kompleksen, večplasten kulturni fenomen, ki je obsegal prostrano območje od Štajerske (na slovenski in avstrijski strani), na zahodu do Koralp, na vzhodu je zajemal panonske nižave vzdolž rek Rabe, Mure, Drave. Nove raziskave, predstavljene na simpoziju, so prinesle novosti glede poselitvenih območij in njihovih značilnosti, ki se kažejo v tipih naselbin (višinske oz. nižinske), stavb (novost so zemljanke) ter v oblikah grobov in njihovih oznak (npr. gomile z mo- gočno grajeno grobno kamro in dromosom na eni strani ter na drugi strani grobovi, grobne parcele in gomile, obdane z jarki ipd.). Kljub skupnim kulturnim značilnostim, ki se izražajo predvsem v religiozni sferi, pa lahko v njenem okviru ugotavljamo tudi razlike med posameznimi regionalnimi skupnostmi. Ključne besede: Štajerska, Prekmurje, starejša železna doba, tipi naselbin, tipi grobov Abstract The Styrian-Pannonian group is a characteristic representative of the eastern Hallstatt cultural circle. This term refers to the complex, multi-strata cultural phenomenon that extended across a broad region from Styria (on both the Slovenian and Austrian sides), in the west to the Kor Alps, while in the east it encompassed the Pannonian plains along the Raab/ Rába, Mur/Mura, and Drau/Drava Rivers. New research presented at the symposium offered new information in terms of the settlement regions and their characteristics, as indicated by the types of settlements (in the heights or on low lying land), buildings (pit-dwellings represent a new element), and the forms of graves and their markers (e.g. -
Tectonic Interpretation of the Metamorphic Field Gradient South of the Koralpe in the Eastern Alps
Austrian Journal of Earth Sciences Vienna 2018 Volume 111/2 155 - 170 DOI: 10.17738/ajes.2018.0010 Tectonic interpretation of the metamorphic field gradient south of the Koralpe in the Eastern Alps Alexandra HERG*) & Kurt STÜWE Institute of Earth Sciences, University of Graz, Universitätsplatz 2, A-8010, Graz, Austria; *) Corresponding author: Alexandra Herg, [email protected] KEYWORDS Pohorje; Koralpe; slab extraction; Plattengneis-Plankogel shear zone Abstract In order to constrain tectonic models for the nature of the Eoalpine high pressure belt at the eastern end of the Alps, we investigate the formation pressure of metamorphic rocks along a profile between the Koralpe and the well-known UHP rocks of the southern Pohorje mountains. Rocks from three different regions are considered: (i) the rocks of the southernmost Koralpe to the north, (ii) the rocks of the Plankogel Unit between the Plankogel detachment and the Drava valley and (iii) the rocks between the Possruck range and the southern Pohorje mountains. In the Koralpe, pelitic rocks record a formation pressure around 15 – 18 kbar, as reported in the literature. For the Plankogel Unit, we derive pres- sures between 7.1 ± 1.95 kbar and 11.5 ± 3.42 kbar at 650 °C and recognize only a single Eoalpine metamorphic event. For the high grade rocks of the Pohorje mountains, we derive peak metamorphic pressures (explored with the garnet- muscovite-kyanite-quartz assemblage) that rise from 16.2 ± 3.45 kbar (at 700°C) in the north, to 23.9 ± 2.49 kbar (at 700 °C) in the south. There, we also recognize a later lower pressure event that is derived from pressure calculations with the full equilibrium assemblage. -
Southern Line Experience More
SOUTHERN EXPERIENCE LINE MORE 80 km NEW TUNNELS AND UNDERPASSES 3,500,000 18 PEOPLE LIVING IN THE SOUTHERN NEWLY BUILT RAILWAY STATIONS, TRAIN LINE’S COMMUTER BELT STOPS, AND FREIGHT TRAFFIC FACILITIES 33 km KORALM TUNNEL, ONE OF THE LONGEST RAILWAY TUNNELS IN THE WORLD 1 h 20 min 250 km/h SHORTER TRAVEL TIME POSSIBLE MAXIMUM VIENNA – KLAGENFURT LINE SPEED WL 15,000 JOBS IN THE OPERATING STAGE AFTER 2026 50 min 2026 SHORTER TRAVEL NEW, MODERNISED TIME GRAZ - VIENNA FACILITIES PUT INTO OPERATION Experience more. > 5,000 EMPLOYED WORKERS When we say "experience more", we mean all the 200 km 14,000,000 many dimensions of human travel: arriving, living EXTENDED, MODERNISED TONS OF EXCAVATED AND RAILWAY LINE EXTRACTED MATERIAL and learning. 150 NEW BRIDGES AND In 2026, trains will speed from Vienna to Klagen- UNDERPASSES furt in just 2 hours and 40 minutes and from Graz to 170 km 210,000 NEW CONSTRUCTION ROUTE NEW SEGMENTS ARE BEING Klagenfurt in 45 minutes. Covering a total of 470 km, BUILT IN THE TUNNEL they will pass through numerous new railway stations ~90 and through the Semmering and the Koralpe moun- MODERNISED RAILWAY STATIONS AND TRAIN STOPS tains at the highest of speeds. And when it comes to more "experiences" - just wait until Austria’s new Southern Line opens! 4 The Benefits The Benefits 5 The future of traveling and transport SHORTER TRAVEL TIMES The Southern Line is one of the largest and most VIENNA – GRAZ 2017: from 2 h 35 min 2026: 1 h 50 min VIENNA – KLAGENFURT 2017: from 3 h 55 min 2026: 2 h 40 min spectacular infrastructure projects of the coming decade.