TY - JOUR
T1 - COSC-2 – drilling the basal décollement and underlying margin of palaeocontinent Baltica in the Paleozoic Caledonide Orogen of Scandinavia
AU - Lorenz, Henning
AU - Rosberg, Jan Erik
AU - Juhlin, Christopher
AU - Klonowska, Iwona
AU - Lescoutre, Rodolphe
AU - Westmeijer, George
AU - Almqvist, Bjarne S.G.
AU - Anderson, Mark
AU - Bertilsson, Stefan
AU - Dopson, Mark
AU - Kallmeyer, Jens
AU - Kück, Jochem
AU - Lehnert, Oliver
AU - Menegon, Luca
AU - Pascal, Christophe
AU - Rejkjær, Simon
AU - Roberts, Nick N.W.
PY - 2022/2/25
Y1 - 2022/2/25
N2 - 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.
AB - 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.
U2 - 10.5194/sd-30-43-2022
DO - 10.5194/sd-30-43-2022
M3 - Article
SN - 0734-5615
VL - 30
SP - 43
EP - 57
JO - Scientific Drilling
JF - Scientific Drilling
IS - 0
ER -