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Now showing items 1-10 of 10
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(2006)The Guadix topographic depression is a Neogene-Quaternary basin located in the central sector of the Betic Cordillera at the boundary between the South Iberian margin and the Alboran domain. This topographic depression is ...
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(2006)The Tyrrhenian margin of the Apennine chain (TMAC) experienced widespread extensional tectonics characterized by volcanism and the formation of several marine and intermontane troughs and basins in Pleistocene times. The ...
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(2006)During the late Tortonian (upper Miocene), the Guadix Basin in S Spain formed one of the Betic corridors that connected the Mediterranean Sea with the Atlantic Ocean. The closure of this connection occurred in a series of ...
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(2006)Twenty two samples were studied to investigate the nature and evolution mechanism of mixed-layer kaolinite-smectite (K-S). We examined the <2 µm or <0.2 µm fraction of K-S formed by hydrothermal and hypergenic alteration ...
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(2006)This study aims to contribute to a better understanding of the nature and evolution mechanism of interstratified clay minerals. We examined the <2 m or <0.2 size fraction of interstratified kaolinite-smectite (k-s) formed ...
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LATE MIOCENE CLIMATE IN THE CIRCUM-ALPINE REALM-A QUANTITATIVE ANALYSIS OF TERRESTRIAL PALAEOFLORAS (2006)Selected mega- and microfloras from Central and Southern Europe have been analysed for the time interval Tortonian/Pannonian (MN 9-12) with the Coexistence Approach to obtain quantitative palaeoclimate data. The results ...
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(1988)This article sums up the second stage of work on devising a Late Cenozoic radiometric time scale for the eastern Paratethys, in which we initially dated Sarmatian deposits of Moldavia and the Kerch'-Taman' region. Radiometric ...
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(2006)This study of the Çameli Basin presents a detailed basin evolution combined with structural analysis and provides the first detailed time-stratigraphic framework for the neotectonic development of Neogene grabens along the ...
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PARATETHYAN-MEDITERRANEAN CONNECTIVITY IN THE SEA OF MARMARA REGION (NW TURKEY) DURING THE MESSINIAN (2006)The Sea of Marmara region is thought to have been a gateway between Paratethys and the Mediterranean since the Middle Miocene, and is therefore an important control on water mass exchange between the two realms. The Miocene ...
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(2006)Fingerlike bodies of evaporite rocks have been observed in many regions affected by multiple tectonic phases, such as the Atlas, the Pyrenees, or the Zagros Mountains, where they have been interpreted as fault-plane diapiric ...
Now showing items 1-10 of 10