Results 61 to 70 of about 6,721 (174)
Paesaggi dei flysch appenninici
, 2004 I Flysch sono successioni di arenarie, calcari e peliti di origine torbiditica. I paesaggi dei Flysch, sono in funzione della litologia che li costituisce (alternanza di litotipi) e, soprattutto, dell’assetto strutturale. Nell'articolo vengono descritti,
CASTALDINI, Doriano
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What, if anything, is a Paratrochamminoides? A key to the morphology of the Cretaceous to Cenozoic species of Conglophragmium and Paratrochamminoides (Foraminifera) [PDF]
, 2004 We present a review of the current taxonomical status of the genus Paratrochamminoides Soliman, 1972. We recognise five main subgroups of this genus based upon the following modes of coiling: trochospiral, streptospiral, glomospiral, triloculine or ...
Kaminski, M.A., Kuhnt, W.
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Studia Geotechnica et Mechanica, 2015 The paper presents the results of analysis of surface roughness parameters in the Krosno Sandstones of Mucharz, southern Poland. It was aimed at determining whether these parameters are influenced by structural features (mainly the laminar distribution ...
Pieczara Łukasz
doaj +1 more source
Acta Universitatis Carolinae Geographica, 2013 The occurrence and evolution of crevice-type caves is one of the most spectacular phenomena in the progression of slope failures in distinct types of rocks.
Jan Lenart, Tomáš Pánek
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Origin of megarhythms in flysch sequences of the Quebec Appalachians
, 1979 The cyclic and positive sequences observed in the External Domain of the Quebec Appalachians between L'IsIet and Grosses Roches have been interpreted as facies of deep-sea fans that result from progradation.
Jean Lajoie
core +1 more source
Etude du Kemalpaşa Dağı (Province d'İzmir, Turquie)
Bulletin of the Mineral Research and Exploration, 1963 Le Kemalpaşa Dağı est un massif calcaire de 20 km de diametre s'elevant jusqu'a 1500 m entre İzmir et les contreforts du massif cristallin de Menderes. La structure est compliquee; une orientation SW-NE predomine cependant. Des failles WE le tronquent au
Joel VERDIER
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Detrital pyroxenes in the Eocene flysch of the Istrian Basin (Slovenia, Croatia) [PDF]
, 2008 For the first time, few detrital augite and pigeonite crystals have been found in the Eocene flysch basins of Istria (Trieste-Koper basin; Italy, Slovenia, Croatia) and Krk Island (Croatia).
Lenaz, Davide, Lenaz, D.
core +1 more source
Rockwall retreat on badlands in Slovene Istria
Geologija, 2008 Steep bare rocky slopes that are badlands at the same time, are a morphogenetic particularity of the flyschpart of the Istrian Peninsula. On them, microrelief forms are of a short life cycle, since erosion processes are fast. On the basis of measurements
Matjaž Mikoš, Matija Zorn
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The Buzet Thrust Fault in Istria and overturned carbonate megabeds in
Geologija, 2004 Detailed geological mapping undertaken in the framework of monitoring of the motorway construction works in SW Slovenia has revealed the existence of a large-scale thrust fault between Buzet and Koper (termed the Buzet Thrust Fault) and extensive thrust ...
Ladislav Placer +4 more
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The serpulid worm Rotularia spirulaea from Eocene beds near Gračišće in Istria, Croatia
Geologija, 2008 In paper several selected specimens of sedentary Polychaetes of species Rotularia spirulaea (Lamarck, 1818) are presented. They were found in Middel Eocene – Lutetian calcareous breccias and conglomerates, respectively olistostromes,below the village of ...
Vasja Mikuž
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