Volume 20 is traditional proceedings of the Meeting of the Central European Tectonic Studies Group/Meeting of the Czech Tectonic Studies Group/Carpathian Tectonic Workshop that was held in Zakopane, Poland, in April 19-22, 2006. Integral part of this volume is the excursion guide.
Two field excursions are mainly concerned on the medial portion of the Outer West Carpathians. One of these trips, “Structural development of the Magura Nappe (Outer Carpathians): From Palaeogene-Neogene subduction to Neogene-present-day collapse”, is devoted to the structural evolution of the Outer Carpathian accretionary wedge, including such topics as: early, soft-sediment deformation, succession of thrusting, large-scale Neogene rotations reconstructed from palaeomagnetic data, progressive vein mineralization, subduction-related(?) andesite intrusions and late Neogene to present-day deformation based on the analysis of fractured pebbles.
The second trip, “Late Cretaceous–Neogene evolution of the Polish Carpathians”, is focused on the Late Cretaceous – Neogene tectonosedimentary evolution of the Pieniny Klippen Belt and Outer (Flysch) Carpathian accretionary wedge, addressing: syntectonic evolution of the sedimentary basins, olistoliths, source areas, main tectonic units along the Zakopane-Kraków geotraverse, as well as timing and periodicity of thrusting.
G20-01 | Trace Element and Nd-Sr Isotopic Composition of Lamprophyres from the Ditrău Alkaline Massif, Romania |
G20-02 | Microstructural Analyse of Orthogneisses from the North-Eastern Part of the Bystrzyca Mts., West Sudetes |
G20-03 | Composition of Biotites from Čierna Hora Granitoids (Western Carpathians) as an Indicator of the Granite Tectonic Setting |
G20-04 | Granitic Rocks from Branisko Mts. (Western Carpathians): Geochemistry, Mineralogy and Tectonic Implications |
G20-05 | Attempt to Dating of Accretion in the West Carpathian Flysch Belt: Apatite Fission Track Thermochronology of Tuff Layers |
G20-06 | REE Accessory Minerals in the Gneiss and Granulite Clasts from the Silesian Unit (Western Outer Carpathians, SE Poland) as Indicators of Metamorphic Processes |
G20-07 | Geology and Tectonics of the Vršatec Klippen Area (Pieniny klipsen Belt, Western Slovakia) |
G20-08 | Tectonic Deformations in the Orava Basin Margins in the Western Carpathians, Based on the DEM Analysis and Geological Research |
G20-09 | Olistostroms as Indicator of the Geodynamic Process (Northern Carpathians) |
G20-10 | The Fault Tectonics of the Middle Skawa River Valley (Polish Flysch Carpathians) |
G20-11 | Are There Olistoliths on the Eperkés Hill? The Paleomagnetic Answer |
G20-12 | Upper Mantle Mylonites: Evidence for Hydrated Mantle Wedge Beneath the Eastern Transylvanian Basin |
G20-13 | Multicomponent Diffusion Modeling of Garnet: a Tool To Estimate Burial and Exhumation Rate of Metamorphic Complexes |
G20-14 | Tertiary Tectonic Evolution of the Pannonian–Carpathian–Eastern Alpine Domain: a Personal View of from Pannonia in the Light of the Terminological Question of Tectonic Units |
G20-15 | Kinematic and Rheological Model of Exhumation of High Pressure Granulites in the Variscan Orogenic Root: Example of the Blanský Les Granulite, Bohemian Massif, Czech Republic |
G20-16 | Structure and Petrology of the Western Part of the Meliata Unit, West Carpathians |
G20-17 | The Zázrivá Fault – Paleostress History and Kinematics (Pieniny Klippen Belt, North Slovakia) |
G20-18 | Geodynamic Evolution of the Subsilesian Realm |
G20-19 | Phanerozoic Palaeogeography of Southeast Asia |
G20-20 | Lithospheric Structure of the Carpathian Mountains, Pannonian basin and Eastern Alps Based on Seismic Data Marek GRAD and working group |
G20-21 | Tectonic Setting of Sokolov Basin in Relation to Prediction of Thermal Water Discharge Zones |
G20-22 | Two Types of “Augen Gneisses” in the Śnieżnik Metamorphic Unit, West Sudetes, Poland |
G20-23 | Variscan Hydrothermal Veins in the Prague Synform (Barrandien Area) |
G20-24 | Origin of Felsic Migmatites by Ductile Shearing and Melt Infiltration |
G20-25 | The Role of Melt Infiltration in the Formation of Migmatitic Orthogneiss |
G20-26 | New Seismo-Tectonic Activity near Zakopane (Poland) – Events Recorded by Broad-Band Stations Operated by IPE |
G20-27 | Seismo-Tectonic Activity in the NE Part of the Bohemian Massif – New Records in the Period 2004–2005 |
G20-28 | Geodynamic Implications of Flattened Equigranular Textured Peridotites from the Central Part of the Carpathian–Pannonian Region |
G20-29 | Magnetic Fabric and Ductile Deformation Differences between the Magura and Krosno Groups of Thrust Sheets of the Flysch Belt of the West Carpathians and their Tectonic Implications |
G20-30 | Fluid Inclusion, Stable Isotope and Geochronologic Evidence of Cretaceous Collision-Related Formation of Hydrothermal Veins in the Gemeric Basement (Western Carpathians) |
G20-31 | Metamorphism and Exhumation Processes of the Shotur Kuh Metamorphic Complex, Semnan Province (Central Iran Zone) |
G20-32 | Emplacement Mechanisms of the Thrust Sheets in the Barrandian (Bohemian Massif) |
G20-33 | Contrasting Petrogenesis of two Volcanic Suites in the Devonian Vrbno Group (Hrubý Jeseník Mts., Czech Republic) |
G20-34 | On the Genesis of Two Meridionally Trending Lineations in Rocks of the Orlica-Śnieżnik Dome: Evidence from Marbles of the Strojič Formation |
G20-35 | Application of Newly Developed ArcGIS Software Extensions for Localization of Faults and Natural Zones of Methane’s Escape by Morphotectonic Analysis (Moravosilesian Region) |
G20-36 | Deformation Pattern Related to an Orogen Parallel Extension Event Recorded in the Vepor Unit, West Carpathians |
G20-37 | Tectonic Control and Basin Evolution of the Northern Transdanubian Eocene Basins (Vértes Hills, Central Hungary) |
G20-38 | Do You Separate Sets of Reactivated Faults Manually? |
G20-39 | Do We Have a Remnant of the Hanseatic Terrane and/or Rheno-Hercynian Ocean in the Western Carpathians? – A Case Study from the Devonian of the Považský Inovec Mts. |
G20-40 | Paleogene-Early Miocene Igneous Rocks and Geodynamics of the Alpine-Carpathian-Pannonian-Dinaric Region: an IntegratedApproach |
G20-41 | Depositional Systems and Lithofacies of the Zlín Formation near the Contact between the Bystrica and Rača Units (Magura Nappe, Outer Carpathians, Eastern Slovakia) |
G20-42 | Depositional Environments and Biostratigraphy of the Lower Part of Rača Unit Paleogene (Magura Nappe, Outer Carpathians, Eastern Slovakia) |
G20-43 | Temporal Investigations and Retrograde Metamorphism of the North-Eastern Part of the Bohemian Massif |
G20-44 | Tectonic Position of the Latest Triassic–Jurassic Sequences of Rudabánya Hills, NE Hungary – The First Steps in a Puzzle |
G20-45 | Multiple Magmatic Fabrics in Episodically Emplaced Granites inTranstensional Setting: Tectonic Model Based on AMS Study and Numerical Modeling |
G20-46 | Caledonian Orogeny in Southeast Asia: Questions and Problems |
G20-47 | Komparative Velocity-Dependent Gravity Modeling of the Density Section Along Three Carpathian DSS Profiles |
G20-48 | Timing and Structural Style of Final Thrusting Movements of the Carpathian Orogenic Wedge, S Poland |
G20-49 | Salt Tectonics in Compressional Settings: Comparison of the S Pyrenees and the N Carpathians |
G20-50 | Role of Basement Tectonics in Evolution of Salt Diapirs: the Mid-Polish trough Versus the Dead Sea Basin |
G20-51 | Internal Flow Fabric Study of Viscous Lava Domes in Central Slovakia by Means of AMS and Quantitative Microstructural Study |
G20-52 | Vertically Decoupled Thickening and Exhumation Processes in Orogenic Supra- and Infra-Structure During Building of Gemer- -Vepor Continental Wedge |
G20-53 | Young Tectonics of the Orava Basin and Southern Magura Nappe, Polish Western Carpathians, in the Light of Gravity Studies: A New Research Proposal |
G20-54 | Structural Position and Metamorphism of Peridotite and Eclogite Bodies Within Granulite in the Bestvina Unit, Bohemian Massif |
G20-55 | Neotectonic Investigations of the Érmellék Region (NE Pannonian Basin, NW Transylvania) |
G20-56 | REE Accessory Minerals as Regional Metamorphic Processes Indicators: An Example from Wedel Jarlsberg Land, Svalbard |
G20-57 | The Tectonic History of the Mýto – Tisovec Fault (Western Carpathians) |
G20-58 | A New Method in the Geologic-Tectonic-Hydrogeologic Documentation of Shafts and Tunnels Page 91 |
G20-59 | Reconstructing Post-Carboni ferous History of the Krkonoše Piedmont Basin Using Detrital Apatite Fission-Track Data |
G20-60 | The Contact Zone between the ALCAPA and Tisza-Dacia Mega-Tectonic Units of Northern Romania in the Light of New Paleomagnetic Data |
G20-61 | First Paleomagnetic Results from the Oligocene Sediments of the Silesian Nappe, Western Outer Carpathians |
G20-62 | Dating of the Gneiss Clasts from Gródek at the Jezioro Rożnowskie Lake (the Silesian Unit, SE Poland) Based on U-Pb Method |
G20-63 | Traces of the Pre-Variscan Tectono-Thermal Event in Rocks of the Orlica-Śnieżnik Dome |
G20-64 | Thrusts and Folds in the Neyriz Ophiolite and Associated Rocks, Iran |
G20-65 | Contrasting Metamorphic Evolution of HP Rocks in the Gföhl Unit of the Kutná Hora Crystalline Complex and the Moldanubian Zone in Austria. |
G20-66 | Geodynamic Signifi cance of Late Cretaceous Lamprophyres from the Carpathian-Pannonian Region |
G20-67 | Tertiary Stress Field Evolution in the Eastern Part of the Bükk Mountains, NE Hungary |
G20-68 | Geochemistry of Metabasites in the Stronie Group and Nové Město Group, the Orlica-Śnieżnik Dome, West Sudetes |
G20-69 | Granitoids from the Ditrău Alkaline Massif, Transylvania, Romania |
G20-70 | Tertiary Tectonics and Paleostress Reconstruction in the Central Carpathian Paleogene Basin (Orava Region) |
G20-71 | Tectonic Evolution of the Pie niny Klippen Belt and its Structural Relationships to the External and Central Western Carpathians |
G20-72 | Late Jurassic to Early Miocene Tectonic Evolution and Palaeo geography of the Western Outer Carpathians 1 |
G20-73 | Geochronology of the Crystalline Basement of the Western Outer Carpathians’ Source Areas – Constraints from K/Ar Dating of Mica and Th-U-Pb Chemical Dating of Monazite from the Crystalline ‘Exotic’ Pebbles |
G20-74 | A Ramp-and-Flat Geometry of Thrust Faults in the Pavlov Hills, Western Carpathians, Czech Republic |
G20-75 | Late Neogene Tectonic Activity of the Central Part of the Carpathian Foredeep, South Poland Pages 113-114 |
G20-76 | Pattern of the Mesoscopic Thrust Faults in the Eastern Part of the Silesian Nappe (Polish Western Outer Carpathians) |
G20-77 | The Black Box of the Stress Analysis Based on Calcite Twinning |
G20-78 | Neotectonic and Landscape Evolution of the Gödöllő Hills, Central Pannonian Basin, Hungary Pages 116-118 |
G20-79 | Lower Crustal Channel Flow in Hot Orogens in Space and Time Exemplifi ed by the Variscan Eastern Margin |
G20-80 | Extraction of Morphotectonic Features from High-Resolution Photogrammetric DEM (Mecsek Mts., Hungary) |
G20-81 | Gravity Modelling of the Krkonoše-Jizera Pluton |
G20-82 | The Problem of Garnet Composition in Eclogite-Bearing Gneisses from the Śnieżnik Metamorphic Complex (Western Sudetes) |
G20-83 | The Basement of Eastern Part of the Polish Carpathians in the Light of Geophysical Data Interpretation |
G20-84 | Application of Paleomagnetic Methods for the Tectonic Study of Northern Variscan Thrust Front Pages 124-125 |
G20-85 | Mechanics of Large-Scale Sand Injection – Understanding the Hamsun Giant Sand Injectite Complex |
G20-86 | Record of Motion Along the Red River Fault Zone in Provenence Studies, Northern Vietnam |
G20-87 | Structural Analysis and Paleostress Reconstruction of the Spišská Magura and Podhale Region Pages 127-128 |
G20-88 | Garnet Pyroxenites from Eastern Transylvanian Basin: An Integrated Textural and Geochemical Study |
G20-89 | Neotectonic Character of the Horná Nitra Depression |
G20-90 | Tectonics of Variscan Foreland Coalbearing Basin on Example of Karvina Subbasin – Upper Silesian Coal Basin |
G20-91 | Tectonic Features Within the Cap Rock of the Mogilno Salt Structure, Central Poland |
G20-92 | Quaternary Tectonic Activity of the Central Part of the Polish Carpathian Foredeep, Evidences from Archaeological Open Site at Brzezie near Kraków |
G20-93 | Kinematic Indicators of Slip Sense Along Faults in Loess Deposits: A Case Study from Fossil Graben at Brzezie, Polish Carpathian Foredeep |
G20-94 | Analogue Modeling of AMS Development During Emplacement of Shallow Level Volcanic Bodies (Extrusive Domes and Laccoliths) |
G20-95 | The Mode of Flow and Emplacement of a Trachyte Body of the České Středohoří Mts. Studied by Means of AMS and EBSD Techniques |
G20-96 | Tectonometamorphic Evolution of the Svratka Crystalline Complex(NE Bohemian Massif): Evidence for Wrench-Dominated Tranpression along the NE Margin of the Variscan Orogenic Root |
G20-97 | Textural Relations and Mineral Compositions of Retrogressed Low-Grade, High-Pressure Metabasites and Phyllites around Krkonoše –Jizera Complex and near Kraslice in Krušné Hory Mts. |
G20-98 | Cadomian Versus Variscan Fabrics in the Desná Dome Basement Rocks, East Sudetes |