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  • Articles  (3)
  • Articles: DFG German National Licenses  (3)
  • Springer  (3)
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  • Articles  (3)
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  • 1
    Electronic Resource
    Electronic Resource
    A fore-arc origin for the Thrace Basin, NW Turkey (1996)
    Springer
    International journal of earth sciences 85 (1996), S. 662-668 
    Details
    ISSN: 1437-3262
    Keywords: Fore-arc ; Medial Eocene ; Strike-slip Thrace ; Basin ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Hydrocarbon-bearing Thrace Basin occupies much of the European part of Turkey. The Middle Eocene to Oligocene sequence in the centre of the basin exceeds 9 km in thickness. Based on the stratigraphy, structure and the regional context of this basin, we propose that it developed as a fore-arc basin between the medial Eocene and the Oligocene, above the northward subducting Intra-Pontide Ocean. Its post-Miocene history has been dominated mainly by wrench tectonics resulting from the activity of the now-deactivated northwestern strand. of the present-day North Anatolian fault zone.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02440103
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Geological evolution of the Gulf of Saros, NE Aegean Sea (1998)
    Springer
    Geo-marine letters 18 (1998), S. 1-9 
    Details
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic régime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s003670050045
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    Paper (German National Licenses)
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  • 3
    Electronic Resource
    Electronic Resource
    A fore-arc origin for the Thrace Basin, NW Turkey (1996)
    Springer
    Geologische Rundschau 85 (1996), S. 662-668 
    Details
    ISSN: 0016-7835
    Keywords: Key words Fore-arc ; Medial Eocene ; Strike-slip ; Thrace Basin ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Hydrocarbon-bearing Thrace Basin occupies much of the European part of Turkey. The Middle Eocene to Oligocene sequence in the centre of the basin exceeds 9 km in thickness. Based on the stratigraphy, structure and the regional context of this basin, we propose that it developed as a fore-arc basin between the medial Eocene and the Oligocene, above the northward subducting Intra-Pontide Ocean. Its post-Miocene history has been dominated mainly by wrench tectonics resulting from the activity of the now-deactivated northwestern strand of the present-day North Anatolian fault zone.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/s005310050104
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    Paper (German National Licenses)
    Fulltext
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