Last edited by Dular
Saturday, July 18, 2020 | History

3 edition of Tectonics of the North Sudetic Synclinorium found in the catalog.

Tectonics of the North Sudetic Synclinorium

Andrzej Solecki

Tectonics of the North Sudetic Synclinorium

by Andrzej Solecki

  • 246 Want to read
  • 20 Currently reading

Published by Wydawnictwo Uniwersytetu Wrocławskiego in Wrocław .
Written in English

    Places:
  • Poland,
  • Kaczawa Mountains.
    • Subjects:
    • Geology, Structural -- Poland -- Kaczawa Mountains.

    • Edition Notes

      StatementAndrzej Solecki.
      SeriesActa Universitatis Wratislaviensis,, no 1618, Prace geologiczno-mineralogiczne,, 45, Prace geologiczno-mineralogiczne (Warsaw, Poland : 1990) ;, 45.
      Classifications
      LC ClassificationsQE1 .B64 no. 45
      The Physical Object
      Pagination59 p. :
      Number of Pages59
      ID Numbers
      Open LibraryOL531519M
      ISBN 108322911408
      LC Control Number96108150
      OCLC/WorldCa33199210

      Coniacian sandstones from the North Sudetic Synclinorium revisited: palaeoenvironmental and palaeogeographical reconstructions based on trace fossil analysis and associated body fossils By: Alina Chrząstek and Monika Wypych. The tectonic history of the North Sea area can be subdivided into five stages: Caledonian geosynclinal stage (Cambrian-Devonian). Metamorphic and intrusive rocks of Caledonian age form the basement complex for much of the North Sea area.

        The Sudetic region in SW Poland includes the Sudetes Mts and the Fore-Sudetic block. Both form the marginal NE part of the Bohemian Massif. The Fore-Sudetic block, ultimately formed in the Neogene, is a tectonic step between the uplifted Sudetes Mts and the lowered Fore-Sudetic Monocline. The Trans-North China Orogen (TNCO) is a tectonic zone that records significant magmatic, metamorphic, and tectonic events during the Paleoproterozoic. The central part of the TNCO comprises several Precambrian blocks (the Hengshan Block, the Wutai Block, the Fuping Block, and the Fanshi Block) that are separated by three Paleoproterozoic.

      north sudetic basin This depression was opened within the Kaczawa Com-plex during the Late Palaeozoic times. Its SW margin is limited by the Main Lusatian Fault and the NE border is defined by the Marginal Sudetic Fault (Fig. 2). Up-per Carboniferous sediments followed by sequences of Permian age overlie unconformably the Kaczawa meta-. Only that part of (2) beyond the areal confines of (1) is both of known age and known configuration; these rocks are in sedimentary contact above the older rocks of the synclinorium sequence and are autochthonous. At the north end of the Taconic sequence in western Vermont, rocks of group (1) are beyond reasonable doubt allochthonous.


Share this book
You might also like
Guidebook for field trips in the Rangeley Lakes - Dead River Basin region, western Maine.

Guidebook for field trips in the Rangeley Lakes - Dead River Basin region, western Maine.

The legend of Korra

The legend of Korra

Continuing professional development portfolio, a route to enhanced competence in caring for patients with epilepsy.

Continuing professional development portfolio, a route to enhanced competence in caring for patients with epilepsy.

Word Perfect 6

Word Perfect 6

Savings through energy conservation.

Savings through energy conservation.

Rebels

Rebels

Arrangement of the performances, at Mr. St. Aivres second exhibition, on Monday evening, March 14th, half past seven oclock, at Corres Hotel.

Arrangement of the performances, at Mr. St. Aivres second exhibition, on Monday evening, March 14th, half past seven oclock, at Corres Hotel.

Seasonal adjustment of unemployment series

Seasonal adjustment of unemployment series

The life of Edward FitzGerald

The life of Edward FitzGerald

composers eleven

composers eleven

Treasure Island!!!

Treasure Island!!!

Canada in space

Canada in space

The New York pulpit in the revival of 1858

The New York pulpit in the revival of 1858

Tectonics of the North Sudetic Synclinorium by Andrzej Solecki Download PDF EPUB FB2

Tectonics of the North Sudetic Synclinorium (Acta Universitatis Wratislaviensis) [Solecki, Andrzej] on *FREE* shipping on qualifying offers. Tectonics of the North Sudetic Synclinorium (Acta Universitatis Wratislaviensis)Author: Andrzej Solecki.

A few reports deal with trace fossils from the Lower Muschelkalk of the North Sudetic Synclinorium, SW Poland (Szulc a;Chrząstek Chrząstek, Chrząstek, Chrząstek, b.

This paper presents the results of sedimentological studies of Zechstein marine deposits occurring in the Wleń Graben, a tectonic unit located in the southeastern part of the North Sudetic Synclinorium (NSS; Western Sudetes, SW Poland).Author: Aleksander Kowalski, Karol Durkowski, Paweł Raczyński.

FSB Fore-Sudetic Block, K-P Synclinorium Kościerzyna-Puławy Synclinorium, MPA Mid-Polish Anticlinorium, NSS North-Sudetic Synclinorium, Sz-M Synclinorium Szczecin-Miechów Synclinorium, WEP West. The North Sudetic Basin formed as a synclinal trough within the Late Cretaceous Central European seaway linking the Boreal and Tethyan marine provinces Cited by: 1.

The North-Sudetic Synclinorium is a structural unit of the north-western Kaczawa metamorphic massif, the generation of which is dated at the Late Carboniferous.

In the Rotliegendes times, the Synclinorium area was characterized by diastrophic sedimentation of clastic deposits with intercalations of volcanic rocks, better developed further to.

A quiet tectonic period during the middle Carboniferous‐early Permian is suggested for Indochina‐North Qiangtang‐South China; The North Qiangtang, Indochina, and South China blocks started to rapid drifting sequentially from the earliest Permian to middle Triassic.

In the Grodziec Syncline (Eastern part of the North-Sudetic Synclinorium) the uppermost Zechstein sediments are represented by mudstones and very fine grained sandstones, which smoothly continue.

Define synclinorium. synclinorium synonyms, synclinorium pronunciation, synclinorium translation, English dictionary definition of synclinorium. n, pl -ria a vast elongated syncline with its strata further folded into anticlines and synclines North-Sudetic Synclinorium). MONITORING OF ANTHROPOGENIC LANDSLIDE ACTIVITY WITH COMBINED UAV AND.

Sedimentation in a synclinal shallow‐marine embayment: Coniacian of the North Sudetic Synclinorium, SW Poland Article (PDF Available) in The Depositional Record 6(1) August with Reads.

These two parts are separated from each other by a regional tectonic dislocation-the Sudetic marginal fault. This region constitutes the north-eastern part of the crystalline Bohemian massif, one.

Milewicz, J., A proposal of formal stratigraphic subdivision of the infill of the North Sudetic Depression. Przegląd Geologiczny, [In Polish, with English summary.] Milewicz, J., Upper Cretaceous of the North Sudetic depression.

Litho-and biostratigraphy, tectonics and remarks on raw materials. Lithofacies and ichnological features of the Coniacian deposits of the upper part of Żerkowice Member and lowest part of the overlying Czerna Formation in southeastern part of the North Sudetic Synclinorium are described and their sedimentary palaeoenvironment is interpreted.

Upper Cretaceous of the North-Sudetic depression (litho- and biostratigraphy, paleogeography, tectonics and remarks on raw materials. Prace Geologiczno-Mineralogic Acta Universitatis Wratislaviensis1–58 [in Polish with English summary]. Milewicz, J., Distribution of Coniacian sandstones in the North Sudetic Basin.

Tectonic evolution of the late Cretaceous Nysa Kłodzka Graben, Sudetes, SW Poland modified the north and south ends of the graben and strongly affected the graben's western walls.

The total thickness of the Upper Cretaceous strata of the Nysa Kłodzka Graben is 3 times that of the Intra-Sudetic Synclinorium, implying that the two units. BIERNACKA J. and JÓZEFIAK M. () - The Eastern Sudetic Island in the Early-to-Middle Turonian: evidence from heavy minerals in the Jerzmanice sandstones, SW Poland.

Acta Geol. Pol., BOSSOWSKI A. and BAŁAZIŃSKA J. () - Tectonic-structural evolution of the North-Sudetic Synclinorium (in Polish with English summary). Biul. as main faulls. They all have dextral character. They mark~ut three strike-sHp blocks - the Fore-Sudetic Block, the Inter-Sudetic Block and the Outer-Sudetic Block; on the last formed -the plumose system of faults and strike-slip blocks of lower order.

The Outer-Sudetic Block forms the ma~n tectonic graben of. After H. Cloos the division of Sudetic Structure is as follow: 1. The Western Sudetes and their Foreland including all the tectonic units of a higher order up to the G6ry Sowie Block and Upper Nysa Klodzka Graben in the W; the Swiebodzice Structure distinguished by H.

Teisseyre () has been considered as a part of Intra-Sudetic Synclinorium. One of the most distinct tectonic zones in the Sudetes is the Intrasudetic Shear Zone (ISZ) (Lužice-Sudetic Fault Zone sensu Uličný et al., & ; ca˚˚. It extends between the southern termination of the Karkonosze Massif in the West, over the southern part of the Intrasudetic Synclinorium (ISS), down to Kłodzko-Złoty Stok.

With unmatched capability, capacity, and color consistency, Tectonics is the premier choice to satisfy your wide format or large-scale printing needs. Over million square feet of annual production capacity means we can handle any and every project that comes our way.

The first-order structure of the basin is a broad Cenozoic synclinorium, which has an amplitude ranging from >16 km in the west to synclinorium has expanded progressively eastward across the Qaidam region: from the western basin against the Altyn Tagh fault at .The Geological Evolution of the North Sea Area in the Tectonic Framework of North Western Europe P.

A. ZIEGLER Ziegler, P. A. The geological evolution of the North Sea area in the tectonic framework of North-Western Europe. Norges geol.

Unders.The development history of the North Sea area can be subdivided into five.Tectonics embraces as its chief working principle the concept of plate tectonics (q.v.), a theory that was formulated in the late s by American, Canadian, and British geophysicists to broaden and synthesize the notion of continental drift and the seafloor spreading hypothesis (qq.v.).