- Geolines Volume 17
The last, 8th meeting of the Czech Tectonic Studies Group (CTS) was held in Hrubá Skála chateau in Czech Republic and was successfully introduced also as the 1st meeting of the newly established Central European Tectonics Group (CETeG). However, it was organized still in a “traditional” fashion, i.e. Czech, Polish and Slovak speakers presented their contributions in their native languages, though the conference materials have always been published in English. The main objective of the CETeG meetings should be presentation of new research results and exchange of scientific ideas between colleagues in different stages of their scientific careers and from different branches of geosciences, as well as providing an introducing international scientific forum for young scientists and students. Therefore a different policy was adopted for the second and next CETeG meetings. To allow a really international attendance of our meetings and because of Central Europe speaks not only by Slavic languages, it was decided to accept English as the official CETeG conferences language. The positive reaction to this decision is a quite large amount of Hungarian colleagues present at the 2nd CETeG meeting. This will surely enrich our discussions in new results, methods and ideas. Inspired by the proportional attendance of researchers and students from all four Visegrad countries, the organizing committee applied also for a grant from the International Visegrad Fund, which would be utilized mostly for publishing conference materials. CETeG gratefully acknowledges the potential support from the Visegrad Fund.
The topics of the conference traditionally include the following items:
- Structural, petrological and geochemical clues to orogenic belt histories
- Tectonic and climatic signals in sedimentary successions
- Basin formation and inversion · Magmatism as a tracer of tectonic events
- Geophysical research of crustal and upper mantle structures
G17-01 | Jurassic-Cretaceous Evolution of the Czorsztyn Unit (Pieniny Klippen Belt, Western Carpathians: New Aspects |
G17-02 | Regional Trends in Thermal Maturity of Paleozoic Rocks of the Moravo-Silesian Basin: a Combined Study of Conodont Alteration Index (CAI), Vitrinite Reflectance and Rock Eval Pyrolysis |
G17-03 | The Sudetic Marginal Fault, SW Poland: a Reactivated Sinistral-Normal Fault |
G17-04 | The Quantitative Link between Fold Geometry, Mineral Fabric and Mechanical Anisotropy: as Exemplified by the Deformation of Amphibolites Across a Regional Metamorphic Gradient |
G17-05 | Petrology of Lamprophyres Occuring in the Northern Part of the Ditrău (Ditró) Alkaline Massif (Jolotca Creek Basin), Romania |
G17-06 | Petrography and Geochemistry of Granitoids from South Part of Strzelin Crystalline Massif (SW Poland) |
G17-07 | Geochemistry and Geochronology of the Javornik Granodiorite and its Geodynamic Significance in the Eastern Variscan Belt |
G17-08 | Some Remarks on the Geophysical Research of the Lithosphere |
G17-09 | Seismic Activity after 2000 Swarm and New Results In The Western Bohemia/Vogtland Area |
G17-10 | Amphibolites in the Vicinity of the Nové Město na Moravě (NE Part of the Moldanubian Zone, Bohemian Massif – the Evidence of Older Granulite Facies Metamorphism |
G17-11 | Denudation Surfaces, Development of Pannonian Formations and Facies Distribution Indicate Late Miocene to Quaternary Deformation of the Transdanubian |
G17-12 | Apatite Fission Track Constraints on Exhumation History of Basement Highs along the Northern Margin of the Danube Basin |
G17-13 | The Outline of the Tectonics of the Hranice Palaeozoic Carbonates (Moravosilesian Palaeozoic) |
G17-14 | Origin and Metamorphic Evolution of Blueschists and Very Low-Grade Rocks of the Meliata Unit, Western Carpathians |
G17-15 | Application of Multicomponent Diffusion Modeling to Garnets in Polymetamorphic Rocks From the Eastern Alps |
G17-16 | Deformation and Exhumation of Magmatic and Metamorphic Rocks of the Pohorje-Kozjak Mts. (Slovenia): Constraints from Structural Geology, Geochronology |
G17-17 | What Are the Tectonic Units in the Pannonian–Carpathian–Eastern Alpine Domain: Terminological Question or Key to Understand Structural Evolution? |
G17-18 | Faults, Block Rotations and the Origin of the Orava Basin in the Western Part of the Polish Outer Carpathians |
G17-19 | The Magnetic Fabric of the Velká Fatra Mts. Part two: Emplacement Mode of the Hercynian Granitic Pluton and its Relation to the Alpine Sedimentary Rocks, Based on AMS |
G17-20 | Easternmost Thrust Tectonics of Czech Part of Upper Silesian Coal Basin (Variscan Accretion Wedge, Bohemian Massif, Czech Republic |
G17-21 | Recent Tectonic Activity and Orientations of the Principal Stresses in the Jeseníky Region |
G17-22 | Nappe Contact as a Tool of Paleotectonic Reconstruction (Inner Western Carpathians a Case of Study) |
G17-23 | Petrogenetic Diversity and Petrographic Convergence of Some Spheroidal Structures in Mafic Intrusive Rocks |
G17-24 | Ground Penetrating Radar Profile Measurements above the Seismoactive Area at the Eastern Margin of the Cheb Basin, Western Bohemia |
G17-25 | Metjane Degassing and Exhumation of the Tertiary Accretionary Complex and Fore-arc Basin of the Western Carpathians |
G17-26 | Lithostratigraphy and Tectonics of the Krynica Unit, Magura Nappe in the Vicinity of Krościenko on Dunajec River, Poland |
G17-27 | A Metamorphic History from Electron Microprobe Dating of Monazite: Variscan Evolution of The Tatra Mountains |
G17-28 | Felsic Granulites from the Gföhl Unit (Austria and Czech Republic): Metamorphosed pre-Variscan Metagranites or Visean High-Pressure Melts? |
G17-29 | Significance and Consequences of Cretaceous Convergent Tectonics in the Vepor Unit, West Carpathians |
G17-30 | Polydeformational-Polymetamorphic Evolution of the Vepor Unit, West Carpathians: Petrological and Microstructural Study |
G17-31 | The Palaeogene Forearc Basin of the Eastern Alps and Western Carpathians: Subduction Erosion and Basin Evolution |
G17-32 | New Zircon FT Ages from Gemeric Granites and Pebbles from Conglomerates of the Klippen Belt |
G17-33 | Re-Os Dating of Molybdenite from the Hnilec Permian Granite-Related Mineralisation – its Tectonic Significance (Gemeric Unit, Slovakia) |
G17-34 | Pan-African Modification of the Contact between Middle and Upper Crust in the Western Zone of the Kaoko Belt (NW Namibia) |
G17-35 | Metamorphic Zonation and Anomalously Hot Geothermal Gradient of the Silesian domain: an Interplay between Devonian Rifting and Carboniferous Collision |
G17-36 | Late Miocene to Pliocene Sedimentary Environments of the Western Carpathians: Response to Tectonic and Climatic Changes |
G17-37 | Contrastive Strain Record within the Magmatic Fabric in the Land’s End Granite (SW England: a Comparative Study of the Orientation Tensor Determined |
G17-38 | Flow and Fabric Development during the Diapiric Rise of Magma: AMS Study on Plaster Models |
G17-39 | Volcanism of the Jurassic-Cretaceous Triple-Junction Zone in the Eastern Carpathians |
G17-40 | Collomorph Calcite in Hydrothermal Veinlets from Culmian Greywackes: Possible Relationships to Genesis, Fluid Flow and their Bacterial Content |
G17-41 | Syngenetic Deformation Structures in Carboniferous Turbidites in the Basement of the Fore-Sudetic Homocline – an Example from Well Marcinki IG- 1 |
G17-42 | Syn-exhumation of the Devonian Basin System in the Bohemian Massif: Geochronological and Geochemical Evidence of the Eo-Variscan Orogen |
G17-43 | PolyLX – the MATLAB™ Toolbox for Quantitative Analysis of Microstructures |
G17-44 | Sm-Nd isotopic chronometry of garnets from the Veporic Unit, Western Carpathians: Some Preliminary Age Results and P-T Constraints |
G17-45 | Petrophysical Properties and Origin of Oriented Porosity in Eclogites with Different Microstructure |
G17-46 | Fault controlled evolution of the ALCAPA region |
G17-47 | Tectonic evolution of the Mórágy Granite Complex (SW Hungary): a puzzle of the Variscan Orogeny in Central Europe |
G17-48 | Paleomagnetically Constrained Geodynamic Events and the Formation of the Ipolytarnóc – Lipovany Ignimbrites |
G17-49 | Geodynamic Application of Paleomagnetism in the ALCAPA Region |
G17-50 | 3D Tectonics of the Prague Synform (Barrandian, Central Bohemia): New Preliminary Results |
G17-51 | P-T-d Record of Rocks of the Stronie Formation (Orlica-Śnieżnik Dome, Sudetes): Evidence of a Continental Collision |
G17-52 | Style and mechanisms of the Early Phase Deformation in the Eastern Part of the Bükk Mts. (NE Hungary) |
G17-53 | Position of the Marmarosh Flysch (Eastern Carpathians) and its Relation to Magura Nappe (Western Carpathians) |
G17-54 | Position of the Late Cretaceous – Palaeocene Source Areas of the Magura Basin – Evidence from Heavy Mineral Study |
G17-55 | Evolution of Neogene-Quaternary Magmatism in the Carpathian Arc and Intra-Carpathian Area: Geodynamic Implications |
G17-56 | The Structural and Metamorphic Record of the Variscan Orogenesis at the Eastern Margin of the Moldanubian Zone in the Bohemian Massif Associated with the Brunovistulian Foreland Underthrusting |
G17-57 | Thrust Tectonics in the Southern Part of the Moravian Karst |
G17-58 | Evolutionary Model for Exhumation of the Meliata Blueschists, Western Carpathians (Slovakia) |
G17-59 | Biotic Responce of Mid-Cretaceous Palaeoceanographic Changes: Data Sets from Planktic Foraminiferal Analysis of Red Beds (Ukrainian Carpathians) |
G17-60 | Turbidite Bed Thickness Distributions Applied in Interpretation of Submarine-Fan Depositional Environments of the Kyčera Beds (Rača Unit, Magura Group) |
G17-61 | Pore Space Geometry of the Rock under Investigation by Ultrasonic Pulse Transmission Pages 84-85 |
G17-62 | Deep Structure, Seismicity Pattern and Subduction Generated Concentration of Metals in Continental Wedges Overlying Convergent Plate Margins |
G17-63 | Correlation of Lithologically Contrasting Rocks from the Kutná Hora-Svratka Region, Czech Republic |
G17-64 | Burial and Exhumation of Eclogites in Continental Accretionary Wedge: An Indentation Model of Eclogite Formation in Variscan Collisional Zone |
G17-65 | Structural and Metamorphic Record of Thickening and Exhumation of the Moldanubian Lower Crust (NE Moldanubian Domain, Bohemian Massif ) |
G17-66 | Controls on Delta Plain Sandstone Geometries and their Implication for Reservoir Exploration in Middle Jurassic Successions: Saltwick Formation, Yorkshire Ness Formation, North Sea |
G17-67 | Lithological Control on Tectonic Deformation of Upper Neogene, Poorly Indurated Strata at Witów, Carpathian Foredeep (Poland) |
G17-68 | Devonian Exotics in the Pieniny Klippen Belt Flysch and their Significance for the Plate Paleozoic Plate Tectonic Reconstruction of the West Carpathian |
G17-69 | Results of Paleomagnetic Study in the Vihorlatské vrchy Mts (East Slovakia) |
G17-70 | A New Natural LPO Type of Clinopyroxene: Evidence from EBSD Study of Eclogite Xenoliths from Kaapvaal Craton, South Africa |
G17-71 | Structural Evolution and Emplacement of the Durbachitic Knížecí Stolec Pluton, South Bohemian (Moldanubian Batholith) |
G17-72 | Structural and Petrological Relations among Granitoids Near Nová Pec (Moldanubian Zone, Šumava – Bohemian Forest) |
G17-73 | Tectonic Control of Glacialy Induced Deformations within Kleczew Graben Zone (Konin Elevation, Great Poland) |
G17-74 | Influence of Strain on the Chemical Composition of Low-Grade Metamorphic Sandstones: Example from Talass Alatau, Kyrgyzstan |
G17-75 | The Reduced Stress Tensor: Problems with Tilting and Block Rotation |
G17-76 | On the Mechanics of Basin Formation in the Pannonian Basin: Inferences from Analogue and Computer Modelling |
G17-77 | Geodynamic Interpretation of Anomalies in the Orientation of the Upper Segment of the Nysa Kłodzka River |
G17-78 | Are the Malé Karpaty Mts. Composed From Three Granite Massifs? |
G17-79 | Differential Exhumation in An Orogenic Root Domain: Snieznik Dome |
G17-80 | The Trans-European Suture Zone Revisited: New Geological and Geophysical Evidence from SE Poland |
G17-81 | Group Lučenec, Slovakia, April 22–25, 2004: Excursion Guide |