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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >3D reflection seismic imaging at the 2.51 km deep COSC-1 scientific borehole, central Scandinavian Caledonides
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3D reflection seismic imaging at the 2.51 km deep COSC-1 scientific borehole, central Scandinavian Caledonides

机译:斯堪的纳维亚喀里多尼德中部2.51公里深的COSC-1科学钻孔的3D反射地震成像

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摘要

The 2.5 km deep scientific COSC-1 borehole (ICDP 5054-1-A) was successfully drilled with nearly complete core recovery during spring and summer of 2014. Downhole and on-core measurements through the targeted Lower Seve Nappe provide a comprehensive data set. An observed gradual increase in strain below 1700 m, with mica schists and intermittent mylonites increasing in frequency and thickness, is here interpreted as the basal thrust zone of the Lower Seve Nappe. This high strain zone was not fully penetrated at the total drilled depth and is thus greater than 800 m in thickness.
机译:2014年春季和夏季,成功钻探了2.5公里深的科学COSC-1钻孔(ICDP 5054-1-A),几乎完成了岩心的恢复。通过有针对性的下塞夫纳普井进行的井下和岩心测量提供了全面的数据集。在1700 m以下观察到的应变逐渐增加,其中云母片岩和间歇性my石在频率和厚度上的增加,在这里被解释为下塞维纳皮群岛的基底逆冲带。该高应变区在总钻孔深度未完全穿透,因此厚度大于800 m。

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