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首页> 外文期刊>Swiss journal of geosciences >A new magnetostratigraphic framework for the Lower Miocene (Burdigalian/Ottnangian, Karpatian) in the North Alpine Foreland Basin
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A new magnetostratigraphic framework for the Lower Miocene (Burdigalian/Ottnangian, Karpatian) in the North Alpine Foreland Basin

机译:北高山前陆盆地下中新世(布尔迪加利/奥特南纪,卡尔帕提亚)的新地层学框架

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摘要

Oligocene-Miocene chronostratigraphic correlations within the Paratethys domain are still highly controversial. This study focuses on the late Early Miocene of the Swiss and S-German Molasse Basin (Late Burdi-galian, Ottnangian-Karpatian). Previous studies have published different chronologies for this time interval that is represented by the biostratigraphically well constrained Upper Marine Molasse (OMM, lower and middle Ottnan-gian), Upper Brackish Molasse (OBM, Grimmelfingen and Kirchberg Formations, middle and upper Ottnangian to lower Karpatian, MN 4a-MN 4b) and Upper Freshwater Molasse (OSM, Karpatian-Badenian, MN 5). Here, we suggest a new chronostratigraphic framework, based on integrated magneto-litho-biostratigraphic studies on four sections and three boreholes. Our data indicate that the OBM comprises chrons 5D.lr and 5Dn (Grimmelfingen Fm), chron 5Cr (lower Kirchberg Fm) and the oldest part of chron 5Cn.3n (upper Kirchberg Fm). The OSM begins during chron 5Cn.3n, continues through 5Cn, and includes a long reversed segment that can be correlated to chron 5Br. The OMM-OSM transition was completed at 16.0 Ma in the Swiss Molasse Basin, while the OBM-OSM changeover ended at 16.6 Ma in the S-German Molasse Basin. As the lower Kirchberg Fm represents a facies of the Ottnangian, our data suggest that the Ottnangian-Karpatian boundary in the Molasse Basin is approximately at 16.8 Ma, close to the 5Cr-5Cn.3n magnetic reversal, andthus 0.4 Myr younger than the inferred age of 17.2 Ma used in recent Paratethys time scales. Notably, this would not be problematic for the Paratethys stratigraphy, because chron 5Cr is mainly represented by a sedimentation gap in the Central Paratethys. We also realise, however, that additional data is still required to definitely solve the age debate concerning this intriguing time interval in the North Alpine Foreland Basin. We dedicate this work to our dear friend and colleague Jean-Pierre Berger (8 July 1956-18 January 2012).
机译:Paratethys域内的渐新世-中新世年代地层相关性仍然存在很大争议。这项研究的重点是瑞士和S-German Molasse盆地(晚Burdi-galian,Ottnangian-Karpatian)的中新世晚期。先前的研究已经发表了该时间间隔的不同年代,以生物地层学上受约束的上海洋Molasse(OMM,下奥特南-吉安中下部),上咸淡淡的Molasse(OBM,Grimmelfingen和Kirchberg地层,中上奥特南期至上Karpatian代表)为代表。 ,MN 4a-MN 4b)和上部淡水Molasse(OSM,Karpatian-Badenian,MN 5)。在此,我们基于对四个断面和三个井眼的磁-岩-生物地层学综合研究,提出了一个新的年代地层学框架。我们的数据表明,OBM包括年代5D.lr和5Dn(Grimmelfingen Fm),年代5Cr(下基希贝格Fm)和年代5Cn.3n的最老部分(上基希贝格Fm)。 OSM在时钟5Cn.3n期间开始,一直持续到5Cn,并包括一个长的反向段,该段可以与时钟5Br相关。瑞士Molasse盆地的OMM-OSM转换完成于16.0 Ma,而S-德国Molasse盆地的OBM-OSM转换终止于16.6 Ma。由于较低的Kirchberg Fm代表了Ottnangian的相,我们的数据表明,Molasse盆地的Ottnangian-Karpatian边界约为16.8 Ma,接近5Cr-5Cn.3n磁逆,因此比推断年龄年轻0.4 Myr最近的Paratethys时标中使用的17.2 Ma值得注意的是,这对于Paratethys地层来说是没有问题的,因为chron 5Cr主要由中Paratethys的沉积间隙代表。但是,我们也意识到,仍然需要额外的数据来明确解决有关北阿尔卑斯前陆盆地这一有趣的时间间隔的年龄争论。我们将这项工作献给我们亲爱的朋友和同事让·皮埃尔·伯杰(Jean-Pierre Berger)(1956年7月8日至2012年1月18日)。

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  • 来源
    《Swiss journal of geosciences》 |2013年第2期|309-334|共26页
  • 作者单位

    Department of Earth- and Environmental Sciences, Palaeontology and Geobiology,Ludwig-Maximilians-University, Richard-Wagner-Strasse 10,80333 Munich, Germany;

    Paleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Utrecht University, Budapestlaan 17,3584 CD Utrecht, The Netherlands;

    Paleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Utrecht University, Budapestlaan 17,3584 CD Utrecht, The Netherlands;

    Department of Earth- and Environmental Sciences, Palaeontology and Geobiology,Ludwig-Maximilians-University, Richard-Wagner-Strasse 10,80333 Munich, Germany;

    Paleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Utrecht University, Budapestlaan 17,3584 CD Utrecht, The Netherlands;

    Paleomagnetic Laboratory 'Fort Hoofddijk', Department of Earth Sciences, Utrecht University, Budapestlaan 17,3584 CD Utrecht, The Netherlands;

    Bundesamt fuer Landestopographie swisstopo, Geologische Landesaufnahme, Seftigenstrasse 264,3084 Wabern, Germany;

    Baerenhubelstrasse 10, 4800 Zofingen,Switzerland;

    Bayerisches Landesamt fuer Umwelt, Dienststelle Augsburg,Haunstetter Strasse 112, 86161 Augsburg, Germany;

    Bayerisches Landesamt fuer Umwelt, Dienststelle Hof,Hans-Hoegn-Strasse 12, 5030 Hof/Saale, Germany;

    Department of Earth- and Environmental Sciences, Palaeontology and Geobiology,Ludwig-Maximilians-University, Richard-Wagner-Strasse 10,80333 Munich, Germany,Senckenberg Center for Human Evolution and Palaeoecology (HEP), Institute for Geoscience, Palaeontological Museum and Collection, Eberhard Karls University Tuebingen,Sigwartstr. 10, 72076 Tuebingen, Germany H. Abdul Aziz;

    ENRES International, Newtonlaan 115, 3584 BH Utrecht,The Netherlands,Department of Earth- and Environmental Sciences, Geophysics,Ludwig-Maximilians-University, Theresienstrasse 41,80333 Munich, Germany;

    Senckenberg Center for Human Evolution and Palaeoecology (HEP), Institute for Geoscience, Palaeontological Museum and Collection, Eberhard Karls University Tuebingen,Sigwartstr. 10, 72076 Tuebingen, Germany H. Abdul Aziz;

    Department of Earth- and Environmental Sciences, Palaeontology and Geobiology,Ludwig-Maximilians-University, Richard-Wagner-Strasse 10,80333 Munich, Germany;

    Department of Earth- and Environmental Sciences, Geophysics,Ludwig-Maximilians-University, Theresienstrasse 41,80333 Munich, Germany;

    Department of Earth- and Environmental Sciences, Geophysics,Ludwig-Maximilians-University, Theresienstrasse 41,80333 Munich, Germany;

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  • 正文语种 eng
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  • 关键词

    Paratethys; Molasse Basin; Upper Freshwater Molasse; Upper Brackish Molasse; Small mammal biostratigraphy; Otolith zones;

    机译:Paratethys;莫拉塞盆地;上层淡水Molasse;上微咸的摩拉斯;小型哺乳动物生物地层学;耳石区域;

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