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COSC-1 – drilling of a subduction-related allochthon in the Palaeozoic Caledonide orogen of Scandinavia

机译:COSC-1 –在斯堪的纳维亚半岛的古生代喀里多尼造山带中钻探与俯冲有关的异源

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The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientificdrilling project focuses on mountain building processes in a majormid-Palaeozoic orogen in western Scandinavia and its comparison with modernanalogues. The project investigates the subduction-generated Seve NapeComplex. These in part under ultra-high-pressure conditions metamorphosedouter continental margin and continent–ocean transition zone assemblageswere emplaced onto the Baltoscandian platform and there influenced theunderlying allochthons and the basement. COSC-1 is the firstof two ca. 2.5 km deep, fully cored drill holes located in the vicinity of theabandoned Fr?? mine, close to the town of ?re in J?mtland,central Sweden. It sampled a thick section of the lower part of the SeveComplex and was planned to penetrate its basal thrust zone into theunderlying lower-grade metamorphosed allochthon. The drill hole reached adepth of 2495.8 m and nearly 100 % core recovery was achieved. Althoughplanning was based on existing geological mapping and new high-resolutionseismic surveys, the drilling resulted in some surprises: the Lower SeveNappe proved to be composed of rather homogenous gneisses, with onlysubordinate mafic bodies, and its basal thrust zone was unexpectedly thick(> 800 m). The drill hole did not penetrate the bottom of thethrust zone. However, lower-grade metasedimentary rocks were encountered inthe lowermost part of the drill hole together with garnetiferous mylonitestens of metres thick. The tectonostratigraphic position is still unclear, andgeological and geophysical interpretations are under revision. The compactgneisses host only eight fluid conducting zones of limited transmissivitybetween 300 m and total depth. Downhole measurements suggest an uncorrectedaverage geothermal gradient of ~ 20 °C km?1. Thispaper summarizes the operations and preliminary results from COSC-1 (ICDP5054-1-A), drilled from early May to late August 2014, and is complemented bya detailed operational report and the data repository.
机译:斯堪的纳维亚Caledonides(COSC)科学钻探项目的大山造山运动重点研究了斯堪的纳维亚西部主要中古生代造山带的造山过程及其与现代类似物的比较。该项目研究了俯冲生成的Seve NapeComplex。这些部分是在超高压条件下将变质双重大陆边缘和大陆-海洋过渡带组合置于巴尔托斯坎台地上的,并影响了其下面的异源地层和基底。 COSC-1是两个ca中的第一个。位于废弃Fr?附近的2.5公里深的全芯钻孔。矿山,靠近瑞典中部J?mtland的弗雷镇。它对SeveComplex下部的厚部分进行了采样,并计划将其基础推力区穿透到下面的低等级变质异形体中。钻孔深度达到2495.8 m,岩心采收率接近100%。尽管计划是基于现有的地质图和新的高分辨率地震勘测进行的,但钻探却带来了一些惊喜:下塞维纳皮被证实是由均质的片麻岩组成,只有下伏的镁铁质岩体,其基底冲断层异常厚(> 800 m )。钻孔未穿透推力区的底部。然而,在钻探的最下部遇到了低品位的沉积沉积岩,同时还有几米厚的石榴石化镍铁矿。构造地层的位置仍不清楚,地质和地球物理解释正在修订中。紧密片麻岩仅容纳八个在300 m和总深度之间具有有限透射率的流体传导区域。井下测量表明,未校正的平均地热梯度约为20°C km ?1 。本文总结了2014年5月上旬至8月下旬钻探的COSC-1(ICDP5054-1-A)的操作和初步结果,并辅以详细的操作报告和数据存储库。

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