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dc.contributor.authorLorenz, H
dc.contributor.authorRosberg, J-E
dc.contributor.authorJuhlin, C
dc.contributor.authorKlonowska, I
dc.contributor.authorLescoutre, R
dc.contributor.authorWestmeijer, G
dc.contributor.authorAlmqvist, BSG
dc.contributor.authorAnderson, M
dc.contributor.authorBertilsson, S
dc.contributor.authorDopson, M
dc.contributor.authorKallmeyer, J
dc.contributor.authorKück, J
dc.contributor.authorLehnert, O
dc.contributor.authorMenegon, L
dc.contributor.authorPascal, C
dc.contributor.authorRejkjær, S
dc.contributor.authorRoberts, NNW

<jats:p>Abstract. The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project aims to characterise the structure and orogenic processes involved in a major collisional mountain belt by multidisciplinary geoscientific research. Located in western central Sweden, the project has drilled two fully cored deep boreholes into the bedrock of the deeply eroded Early Paleozoic Caledonide Orogen. COSC-1 (2014) drilled a subduction-related allochthon and the associated thrust zone. COSC-2 (2020, this paper) extends this section deeper through the underlying nappes (Lower Allochthon), the main Caledonian décollement, and the upper kilometre of basement rocks. COSC-2 targets include the characterisation of orogen-scale detachments, the impact of orogenesis on the basement below the detachment, and the Early Paleozoic palaeoenvironment on the outer margin of palaeocontinent Baltica. This is complemented by research on heat flow, groundwater flow, and the characterisation of the microbial community in the present hard rock environment of the relict mountain belt. COSC-2 successfully, and within budget, recovered a continuous drill core to 2276 m depth. The retrieved geological section is partially different from the expected geological section with respect to the depth to the main décollement and the expected rock types. Although the intensity of synsedimentary deformation in the rocks in the upper part of the drill core might impede the analysis of the Early Paleozoic palaeoenvironment, the superb quality of the drill core and the borehole will facilitate research on the remaining targets and beyond. Protocols for sampling in the hard rock environment and subsequent sample preservation were established for geomicrobiological research and rock mechanical testing. For the former, a sparse sample series along the entire drill core was taken, while the target of the latter was the décollement. COSC-2 was surveyed by a comprehensive post-drilling downhole logging campaign and a combined borehole/land seismic survey in autumn 2021. This paper provides an overview of the COSC-2 (International Continental Scientific Drilling Project – ICDP 5054_2_A and 5054_2_B boreholes) operations and preliminary results. It will be complemented by a detailed operational report and data publication. </jats:p>

dc.publisherCopernicus Publications
dc.subject37 Earth Sciences
dc.subject3705 Geology
dc.subject3706 Geophysics
dc.titleCOSC-2 – drilling the basal décollement and underlying margin of palaeocontinent Baltica in the Paleozoic Caledonide Orogen of Scandinavia
dc.typeJournal Article
plymouth.publication-statusPublished online
plymouth.journalScientific Drilling
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering
plymouth.organisational-group/Plymouth/Faculty of Science and Engineering/School of Geography, Earth and Environmental Sciences
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA
plymouth.organisational-group/Plymouth/REF 2021 Researchers by UoA/UoA07 Earth Systems and Environmental Sciences
plymouth.organisational-group/Plymouth/Users by role
plymouth.organisational-group/Plymouth/Users by role/Academics
dc.rights.embargoperiodNot known
rioxxterms.typeJournal Article/Review
plymouth.funderCOSC 2 – Providing first constraints on the age and setting of Proterozoic igneous and early Palaeozoic sedimentary rocks below and within the Caledonian nappe pile::German Research Foundation

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