Assessing provenance of Upper Cretaceous siliciclastics using spectral γ-ray record
Geologica Carpathica, 2015 The relationship between contents of clay minerals/grain size and spectral γ-ray record (concentrations of K, U and Th) in sediments is used for interpretation of sedimentary facies in wire-line logs.
Šimíček Daniel, Bábek Ondřej
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Field trip - Outer Flysch Carpathians, Pieniny Klippen Belt (PKB), and Tatra Mountains
Geotourism/GeoturystykaThe 36th HKT Workshop (Himalaya-Karakorum- Tibet) is organised by the AGH University of Krakow, Poland. Kraków is situated at the front of the Carpathian orogenic system of the ancient Tethys Ocean and is perfect place for meeting between European-Asian Alpine-Himalayan orogenic belt with long history of the Western and Eastern Tethyan Ocean Realms ...
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Hydrogeological Relationships of the Golubinka Karst Spring in Ljubač Bay, Dalmatia, Croatia
Geologia Croatica, 2006 The Golubinka spring is a typical karst spring situated in northernDalmatia, Croatia. The catchment area is mostly composed of limestonesof the Cretaceous and Palaeogene, with some dolomitic parts.Hydrogeological barriers are composed of flysch or ...
Ante Pavičić +2 more
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Evaluation of existing knowledge of the tectonic history and lithospheric structure of South America [PDF]
While data is available on the lithospheric and crustal structure of the Andes region of South America, there is limited knowledge of these aspects of the eastern portion of the continent.
Keller, G. R., Lidiak, E. G.
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Sedimentary Geology, 1993 Abstract Various techniques of geometric and kinematic analyses, including cross-section balancing and forward modeling, have been applied successfully to the outer Carpathian flysch units along regional geologic profiles crossing the belt from its undeformed foreland to the Pieniny klippen belt (western Carpathians, Poland) or to the central east ...
F. Roure, E. Roca, W. Sassi
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Devonian and Carboniferous palynostratigraphy of the South Portuguese Zone, Portugal : an overview [PDF]
, 2007 A Zona Sul Portuguesa (ZSP) representa o ramo sul do Orógeno Varisco Ibérico e compreende os seguintes domínios, de norte para sul: o Antiforma do Pulo do Lobo, a Faixa Piritosa Ibérica, o Grupo do Flysch do Baixo Alentejo e o Sector Sudoeste ...
Fernandes, Paulo +3 more
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Comment on "Evidence of extensional metamorphism associated to Cretaceous rifting of the North-Maghrebian passive margin : The Tanger-Ketama Unit (external Rif, northern Morocco)" by Vázquez et al., Geologica Acta 11 (2013), 277-293 [PDF]
, 2015 No ...
Chaloouan, A. +3 more
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JURASSIC PALEOGEOGRAPHY OF THE PIENINY AND OUTER CARPATHIAN BASINS
Rivista Italiana di Paleontologia e Stratigrafia, 2004 The Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the
JAN GOLONKA, MICHAL KROBICKI
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Devonian and carboniferous palynostratigraphy of the South Portuguese zone, Portugal - an overview [PDF]
, 2014 The South Portuguese Zone (SPZ) represents the southern branch of the Iberian Variscides and comprehends the following geologic domains: the Pulo do Lobo Antiform, the Iberian Pyrite Belt, the Baixo Alentejo Flysch Group and the Southwest Portugal ...
Fernandes, Paulo +3 more
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MineralogiaVolcanic rocks in the Pieniny Klippen Belt (PKB) of the Western Carpathians have been the focus of geologists for over a century (e.g. Uhlig, 1890; Małkowski, 1921). Miocene volcanism is most common in the PKB.
Bazarnik Jakub +5 more
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