维也纳盆地北部和中部的中新世岩石地层(奥地利)

IF 1.7 4区 地球科学 Q2 Earth and Planetary Sciences
M. Harzhauser, M. Kranner, O. Mandic, P. Strauss, W. Siedl, W. Piller
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引用次数: 22

摘要

摘要首次在综合岩心资料、测井资料和OMV地震资料的基础上,提出了维也纳盆地北部和中部中新世下中期(Ottnagian–Badenian)的简明岩石地层方案。提出了所有地层和成员的类型剖面,提供了地理分布和厚度,描述了典型的沉积环境和化石,并讨论了年龄限制。这个时间框架允许更可靠地计算沉降速率。这反过来可能对重建维也纳盆地的构造史很重要,因为我们没有看到背负阶段和随后的拉裂机制之间的根本差异。以下岩石地层单位在本文中被正式化和/或新引入:Bockfließ组(Ottnagian)、Aderklaa组、Gänserendorf组和Schönkirchen组(Karpatian)、巴登群、Rothneusiedl组和Mannsdorf组(下巴登尼亚)、Auersthal组、Matzen组、巴登组,Leitha组(中巴登尼亚组)和Rabensburg组(上巴登尼亚)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Miocene lithostratigraphy of the northern and central Vienna Basin (Austria)
Abstract For the first time, a concise lithostratigraphic scheme for the lower and middle Miocene (Ottnangian – Badenian) of the northern and central Vienna Basin is proposed, which is based on the integration of core-material, well-log data and seismic information from OMV. For all formations and members type sections are proposed, geographic distribution and thickness are provided, typical depositional environments and fossils are described and age constraints are discussed. This time frame allows for a more reliable calculation of sedimentation rates. This in turn might be important for the reconstruction of the tectonic history of the Vienna Basin as we do not see fundamental differences between the piggy-back stage and the subsequent pull-apart regime. Following lithostratigraphic units are formalized herein and/or are newly introduced: Bockfließ Formation (Ottnangian), Aderklaa Formation, Gänserndorf Member and Schönkirchen Member (Karpatian), Baden Group, Rothneusiedl Formation and Mannsdorf Formation (lower Badenian), Auersthal Formation, Matzen Formation, Baden Formation, Leitha Formation (middle Badenian) and Rabensburg Formation (upper Badenian).
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来源期刊
Austrian Journal of Earth Sciences
Austrian Journal of Earth Sciences Earth and Planetary Sciences-Paleontology
CiteScore
3.10
自引率
0.00%
发文量
0
审稿时长
>12 weeks
期刊介绍: AUSTRIAN JOURNAL OF EARTH SCIENCES is the official journal of the Austrian Geological, Mineralogical and Palaeontological Societies, hosted by a country that is famous for its spectacular mountains that are the birthplace for many geological and mineralogical concepts in modern Earth science. AUSTRIAN JOURNAL OF EARTH SCIENCE focuses on all aspects relevant to the geosciences of the Alps, Bohemian Massif and surrounding areas. Contributions on other regions are welcome if they embed their findings into a conceptual framework that relates the contribution to Alpine-type orogens and Alpine regions in general, and are thus relevant to an international audience. Contributions are subject to peer review and editorial control according to SCI guidelines to ensure that the required standard of scientific excellence is maintained.
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