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Integrating magnetostratigraphy,biostratigraphy, cyclostratigraphy and seismic data to obtain a high resolution stratigraphic record: a case study from the Vienna Basin

机译:整合磁地层学,生物地层学,旋回地层学和地震数据以获得高分辨率地层记录:以维也纳盆地为例

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摘要

We have developed an integrated methodology to obtain a high resolution stratigraphic record that assists in evaluatingthe relative contributions of tectonics, eustacy, and other factors to sedimentary basin infills. The approach combinesmagnetostratigraphic and biostratigraphic analyses of well data to form a basic chronostratigraphic framework. Seismicdata are included to refine the time lines by taking into account unconformities and faults that cause time gaps. These aresubsequently corroborated by detailed analysis of electrical borehole images. The latter, having a vertical resolution of about1 cm, are used to perform a spectral frequency analysis in order to identify cyclicities in the sedimentary record. Using thechronostratigraphic framework, the cyclostratigraphic analysis is well constrained and can provide a temporal resolutionthat lies significantly higher than the Milankovitch cycles. This methodology is demonstrated with a dataset from a boreholein the Central Paratethyan Vienna Basin. Focusing on the Upper Sarmatian, the approach described above resulted in accu-rate chronostratigraphic age dating, the identification and location of time gaps caused by unconformities and faults, andan accurate sedimentation rate for this stage. The cyclostratigraphic results indicate that a strong allocyclic orbital forcingwas superposed on the overall tectonic evolution of the basin.
机译:我们已经开发出一种综合的方法来获得高分辨率的地层记录,以帮助评估构造,储量和其他因素对沉积盆地填充物的相对贡献。该方法结合了井数据的磁性地层学和生物地层学分析,形成了基本的年代地层学框架。通过考虑不整合和导致时间间隔的故障,地震数据包括在内以完善时间线。随后,通过对电井眼图像的详细分析可以证实这些情况。后者具有大约1 cm的垂直分辨率,用于执行频谱频率分析,以识别沉积记录中的周期性。使用年代地层学框架,对地层地层分析进行了很好的约束,可以提供比米兰科维奇旋回明显更高的时间分辨率。维也纳中Paratethyan盆地的一个钻孔数据集证明了这种方法。着眼于上萨尔马蒂安,上述方法导致了准确的年代地层年代测年,对不整合面和断层造成的时间间隙的识别和定位,以及该阶段的准确沉积速率。旋回地层学结果表明,该盆地的整体构造演化过程中叠加了强烈的别针轨道强迫。

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