Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Vladimír Cajz"'
Autor:
Stanislav Šlechta, Vladimír Cajz, Zuzana Skácelová, Kristýna Čížková, Petr Schnabl, Daniela Venhodová, Zoltán Pécskay
Publikováno v:
Geologica Carpathica. 63:423-435
This paper presents the results of a paleomagnetic study carried out on Plio-Pleistocene Cenozoic basalts from the NE part of the Bohemian Massif. Paleomagnetic data were supplemented by 27 newly obtained K/Ar age determinations. Lavas and volcanicla
Autor:
Jaroslav Valecka, Vladimír Cajz
Publikováno v:
Journal of GEOsciences. :201-215
*Corresponding author The paper presents the results of a new detailed survey in the SW part of the Ceske středohoři Mts. (a section of the Ohře/Eger Graben/Rift), focused on its tectonic setting. Courses of the SE marginal graben faults are trace
Autor:
Pavel Raška, Tomáš Řídkošil, Zoltán Pécskay, Vladimír Cajz, Vladislav Rapprich, Martin Košťák, Miroslav Radoň
Publikováno v:
Journal of GEOsciences. :169-180
*� Correspondingauthors Relics of solitary volcanic edifices in NE Bohemia were newly interpreted as remnants of scoria cones and their con - duits. Volcanic activity in this area occurred in a form of scattered Strombolian eruptions of basanitic m
Autor:
Milos Lang, Stanislav Šlechta, Petr Pruner, Vladimír Cajz, Petr Schnabl, Martin Chadima, Tomas Kohout, Zoltán Pécskay, Kadosa Balogh, Jaromír Ulrych, Jiří Novák
Publikováno v:
Studia Geophysica et Geodaetica. 54:77-94
This study provides new thermomagnetic and petrographic data on specific basaltic rock association from the broader vicinity of the Loucna-Oberwiesenthal volcanic centre, western Bohemia/Saxony. Two types of volcanic rocks were recognized there: (i)
Publikováno v:
Geologica Carpathica. 60:519-533
Late Miocene volcanic activity in the České středohoří Mountains (Ohře/Eger Graben, northern Bohemia)First occurrences of superficial bodies of Late Miocene volcanic activity were found in the western part of the České středohoří Volcanic
Publikováno v:
Tectonophysics. 466:47-63
Recent studies of igneous rocks indicate that the predominant occurrence of normal/inverse fabric in dikes may either reflect the presence of multi-domain (MD)/single-domain (SD) grains or it may result from different orientation mechanisms of magnet
Publikováno v:
Studia Geophysica et Geodaetica. 44:346-351
Three independent volcanic suites have been recognised in W Bohemia: (i) the old unimodal alkaline ol. nephelinite-tephrite (29-19 Ma) in the Ohře Rift, (ii) two contemporaneous weakly (trachybasalt/trachyandesite-trachyte/rhyolite; 13-11 Ma) and st
Publikováno v:
Geological Quarterly. 58
The Certovka landslide at Vaňov south of Usti nad Labem, Czech Republic, is developed in a steep slope of the Labe River Valley (LRV). A major episode of landsliding occurred in the first months of 1995, and the slope at Vaňov has been subjected to