Science report
| 
25 Feb 2022
Science report |
| 25 Feb 2022
| 25 Feb 2022
COSC-2 – drilling the basal décollement and underlying margin of palaeocontinent Baltica in the Paleozoic Caledonide Orogen of Scandinavia
Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden
Jan-Erik Rosberg
Engineering Geology, Lund University, John Ericssons väg 1, 221
00 Lund, Sweden
Christopher Juhlin
Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden
Iwona Klonowska
Faculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059
Kraków, Poland
Rodolphe Lescoutre
Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden
George Westmeijer
Centre for Ecology and Evolution in Microbial Model Systems (EEMiS) Linnæus University, Stuvaregatan 4, 39231 Kalmar, Sweden
Bjarne S. G. Almqvist
Department of Earth Sciences, Uppsala University, Villavägen 16, 752 36 Uppsala, Sweden
Mark Anderson
School of Geography, Earth and Environmental Sciences, University of Plymouth, B527 Portland Square, Plymouth PL4 8AA, United Kingdom
Stefan Bertilsson
Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Lennart Hjelms väg 9, 75 651 Uppsala, Sweden
Mark Dopson
Centre for Ecology and Evolution in Microbial Model Systems (EEMiS) Linnæus University, Stuvaregatan 4, 39231 Kalmar, Sweden
Jens Kallmeyer
Section 3.7 Geomicrobiology, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Jochem Kück
Section 4.2: Geomechanics and Scientific Drilling, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
Oliver Lehnert
Geozentrum Nordbayern, Friedrich-Alexander University Erlangen–Nuremberg, Schloßgarten 5, 91054 Erlangen, Germany
Luca Menegon
Njord Centre, Department of Geosciences, University of Oslo, Sem Sælands vei 24, 0371 Oslo, Norway
Christophe Pascal
Institute of Geology, Mineralogy and Geophysics, Ruhr University Bochum, Universitätsstraße 150, 44780 Bochum, Germany
Simon Rejkjær
Engineering Geology, Lund University, John Ericssons väg 1, 221
00 Lund, Sweden
Nick N. W. Roberts
NERC Isotope Geosciences Laboratory, British Geological Survey, Nottingham NG12 5GG, United Kingdom
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Nick M. W. Roberts, Kerstin Drost, Matthew S. A. Horstwood, Daniel J. Condon, David Chew, Henrik Drake, Antoni E. Milodowski, Noah M. McLean, Andrew J. Smye, Richard J. Walker, Richard Haslam, Keith Hodson, Jonathan Imber, Nicolas Beaudoin, and Jack K. Lee
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go-toreference paper for years to come.
Francesca Prando, Luca Menegon, Mark Anderson, Barbara Marchesini, Jussi Mattila, and Giulio Viola
Solid Earth, 11, 489–511, https://doi.org/10.5194/se-11-489-2020, https://doi.org/10.5194/se-11-489-2020, 2020
Julia Mitzscherling, Fabian Horn, Maria Winterfeld, Linda Mahler, Jens Kallmeyer, Pier P. Overduin, Lutz Schirrmeister, Matthias Winkel, Mikhail N. Grigoriev, Dirk Wagner, and Susanne Liebner
Biogeosciences, 16, 3941–3958, https://doi.org/10.5194/bg-16-3941-2019, https://doi.org/10.5194/bg-16-3941-2019, 2019
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Sonja Martens, Christopher Juhlin, Viktor J. Bruckman, Gregor Giebel, Thomas Nagel, Antonio P. Rinaldi, and Michael Kühn
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Ruth A. Beckel and Christopher Juhlin
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Alberto Ceccato, Luca Menegon, Giorgio Pennacchioni, and Luiz Fernando Grafulha Morales
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Sonja Martens, Christopher Juhlin, Viktor J. Bruckman, Kristen Mitchell, Luke Griffiths, and Michael Kühn
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James Gilgannon, Florian Fusseis, Luca Menegon, Klaus Regenauer-Lieb, and Jim Buckman
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Giancarlo Molli, Luca Menegon, and Alessandro Malasoma
Solid Earth, 8, 767–788, https://doi.org/10.5194/se-8-767-2017, https://doi.org/10.5194/se-8-767-2017, 2017
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We present a new case study on the role of brittle precursors in nucleating shear zone. Our studied sample shows a high-pressure, low-temperature (HP/LT) microscale ultramylonite developed by brittle precursors induced during deformation within a host HP/LT granitic mylonite. We infer that the studied structures may be considered as a small-scale example of fault structures related to stick-slip strain accommodation during subduction of continental crust.
James M. Russell, Satria Bijaksana, Hendrik Vogel, Martin Melles, Jens Kallmeyer, Daniel Ariztegui, Sean Crowe, Silvia Fajar, Abdul Hafidz, Doug Haffner, Ascelina Hasberg, Sarah Ivory, Christopher Kelly, John King, Kartika Kirana, Marina Morlock, Anders Noren, Ryan O'Grady, Luis Ordonez, Janelle Stevenson, Thomas von Rintelen, Aurele Vuillemin, Ian Watkinson, Nigel Wattrus, Satrio Wicaksono, Thomas Wonik, Kohen Bauer, Alan Deino, André Friese, Cynthia Henny, Imran, Ristiyanti Marwoto, La Ode Ngkoimani, Sulung Nomosatryo, La Ode Safiuddin, Rachel Simister, and Gerald Tamuntuan
Sci. Dril., 21, 29–40, https://doi.org/10.5194/sd-21-29-2016, https://doi.org/10.5194/sd-21-29-2016, 2016
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The Towuti Drilling Project seeks to understand the long-term environmental and climatic history of the tropical western Pacific and to discover the unique microbes that live in metal-rich sediments. To accomplish these goals, in 2015 we carried out a scientific drilling project on Lake Towuti, located in central Indonesia. We recovered over 1000 m of core, and our deepest core extended 175 m below the lake floor and gives us a complete record of the lake.
Christopher Juhlin, Peter Hedin, David G. Gee, Henning Lorenz, Thomas Kalscheuer, and Ping Yan
Solid Earth, 7, 769–787, https://doi.org/10.5194/se-7-769-2016, https://doi.org/10.5194/se-7-769-2016, 2016
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For this paper, ca. 55 km high-resolution reflection seismic data were interpreted using constraints from magnetotelluric, potential field, and geological data. The resulting integrated geological-geophysical section through the central Caledonides in Sweden provides new insights about the regional tectonic setting, and supplies the basis for siting the second drill hole of the Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project.
Gustavo Viegas, Luca Menegon, and Carlos Archanjo
Solid Earth, 7, 375–396, https://doi.org/10.5194/se-7-375-2016, https://doi.org/10.5194/se-7-375-2016, 2016
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This paper presents microstructural and chemical data of mylonitic granitoids deformed at the brittle-ductile transition in the continental crust. Through a combination of microstructures, chemical analyses and modelling of the strength of constituent phases, we were able to show that strain localisation in shear zones may be triggered primarily by brittle failure, without the need for reaction-softening mechanisms promoted by metamorphic fluids.
H. J. Mills, J. de Leeuw, K.-U. Hinrichs, F. Inagaki, and J. Kallmeyer
Sci. Dril., 20, 59–65, https://doi.org/10.5194/sd-20-59-2015, https://doi.org/10.5194/sd-20-59-2015, 2015
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Proceedings and results are presented from the Seoul 2014 Advancing Subsurface Biosphere and Paleoclimate Research workshop. Participants discussed past and present directions of IODP and ICDP subsurface research, including efforts with DCO and IMPRESS. Discussions led to the formation of a level-based communication system with the goal of improving communication and expectations between all drilling disciplines. The production of a biology-themed handbook to guide surface research is planned.
H. J. Kjøll, G. Viola, L. Menegon, and B. E. Sørensen
Solid Earth, 6, 681–699, https://doi.org/10.5194/se-6-681-2015, https://doi.org/10.5194/se-6-681-2015, 2015
O. Ahmadi, C. Juhlin, M. Ask, and B. Lund
Solid Earth, 6, 621–632, https://doi.org/10.5194/se-6-621-2015, https://doi.org/10.5194/se-6-621-2015, 2015
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The Pärvie fault system extends up to 155km, and its scarps have offsets of tens of meters at the surface in northern Sweden. These fault scarps are inferred to have formed during earthquakes with magnitudes up to 8 at the time of the last deglaciation. In this study, we have mapped the fault system to deeper levels, by a new 22km long 2-D seismic reflection profile. Based on the present and previous seismic data, locations for future boreholes for drilling into the fault system are proposed.
T. L. Kieft, T. C. Onstott, L. Ahonen, V. Aloisi, F. S. Colwell, B. Engelen, S. Fendrihan, E. Gaidos, U. Harms, I. Head, J. Kallmeyer, B. Kiel Reese, L.-H. Lin, P. E. Long, D. P. Moser, H. Mills, P. Sar, D. Schulze-Makuch, H. Stan-Lotter, D. Wagner, P.-L. Wang, F. Westall, and M. J. Wilkins
Sci. Dril., 19, 43–53, https://doi.org/10.5194/sd-19-43-2015, https://doi.org/10.5194/sd-19-43-2015, 2015
H. Lorenz, J.-E. Rosberg, C. Juhlin, L. Bjelm, B. S. G. Almqvist, T. Berthet, R. Conze, D. G. Gee, I. Klonowska, C. Pascal, K. Pedersen, N. M. W. Roberts, and C.-F. Tsang
Sci. Dril., 19, 1–11, https://doi.org/10.5194/sd-19-1-2015, https://doi.org/10.5194/sd-19-1-2015, 2015
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The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project successfully drilled a 2.5km fully cored borehole (COSC-1) through allochthonous subduction-related high-grade metamorphic gneisses and into the underlying thrust zone. This paper summarizes the scientific rationale of the project and presents first preliminary results.
A. S. L. Sjöqvist, M. Arthursson, A. Lundström, E. Calderón Estrada, A. Inerfeldt, and H. Lorenz
Sci. Dril., 19, 13–16, https://doi.org/10.5194/sd-19-13-2015, https://doi.org/10.5194/sd-19-13-2015, 2015
J. Alcalde, D. Martí, C. Juhlin, A. Malehmir, D. Sopher, E. Saura, I. Marzán, P. Ayarza, A. Calahorrano, A. Pérez-Estaún, and R. Carbonell
Solid Earth, 4, 481–496, https://doi.org/10.5194/se-4-481-2013, https://doi.org/10.5194/se-4-481-2013, 2013
P. Skyttä, T. Bauer, T. Hermansson, M. Dehghannejad, C. Juhlin, M. García Juanatey, J. Hübert, and P. Weihed
Solid Earth, 4, 387–404, https://doi.org/10.5194/se-4-387-2013, https://doi.org/10.5194/se-4-387-2013, 2013
Related subject area
Location/Setting: Continental | Subject: Geology | Geoprocesses: Tectonic processes
CALDERA: a scientific drilling concept to unravel Connections Among Life, geo-Dynamics and Eruptions in a Rifting Arc caldera, Okataina Volcanic Centre, Aotearoa New Zealand
Fifteen years of the Chinese Continental Scientific Drilling Program
COSC-1 – drilling of a subduction-related allochthon in the Palaeozoic Caledonide orogen of Scandinavia
Drilling to investigate processes in active tectonics and magmatism
Cécile Massiot, Ludmila Adam, Eric S. Boyd, S. Craig Cary, Daniel R. Colman, Alysia Cox, Ery Hughes, Geoff Kilgour, Matteo Lelli, Domenico Liotta, Karen G. Lloyd, Tiipene Marr, David D. McNamara, Sarah D. Milicich, Craig A. Miller, Santanu Misra, Alexander R. L. Nichols, Simona Pierdominici, Shane M. Rooyakkers, Douglas R. Schmitt, Andri Stefansson, John Stix, Matthew B. Stott, Camille Thomas, Pilar Villamor, Pujun Wang, Sadiq J. Zarrouk, and the CALDERA workshop participants
Sci. Dril., 33, 67–88, https://doi.org/10.5194/sd-33-67-2024, https://doi.org/10.5194/sd-33-67-2024, 2024
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Volcanoes where tectonic plates drift apart pose eruption and earthquake hazards. Underground waters are difficult to track. Underground microbial life is probably plentiful but unexplored. Scientists discussed the idea of drilling two boreholes in the Okataina Volcanic Centre, New Zealand, to unravel the connections between volcano, faults, geotherms, and the biosphere, also integrating mātauranga Māori (Indigenous knowledge) to assess hazards and manage resources and microbial ecosystems.
Zhiqin Xu, Jingsui Yang, Chengshan Wang, Zhisheng An, Haibing Li, Qin Wang, and Dechen Su
Sci. Dril., 22, 1–18, https://doi.org/10.5194/sd-22-1-2017, https://doi.org/10.5194/sd-22-1-2017, 2017
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The 5158 m deep borehole of the Chinese Continental Scientific Drilling (CCSD) Project in the Sulu ultrahigh-pressure metamorphic terrain marked the starting point of the CCSD Program. Since then, several continental scientific drilling projects were conducted with funding of the Chinese government and partially with support of ICDP, resulting in a total drilling depth of more than 35 000 m. This paper reviews the history and major progress of the CCSD Program in the past 15 years.
H. Lorenz, J.-E. Rosberg, C. Juhlin, L. Bjelm, B. S. G. Almqvist, T. Berthet, R. Conze, D. G. Gee, I. Klonowska, C. Pascal, K. Pedersen, N. M. W. Roberts, and C.-F. Tsang
Sci. Dril., 19, 1–11, https://doi.org/10.5194/sd-19-1-2015, https://doi.org/10.5194/sd-19-1-2015, 2015
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The Collisional Orogeny in the Scandinavian Caledonides (COSC) scientific drilling project successfully drilled a 2.5km fully cored borehole (COSC-1) through allochthonous subduction-related high-grade metamorphic gneisses and into the underlying thrust zone. This paper summarizes the scientific rationale of the project and presents first preliminary results.
J. Shervais, J. Evans, V. Toy, J. Kirkpatrick, A. Clarke, and J. Eichelberger
Sci. Dril., 18, 19–33, https://doi.org/10.5194/sd-18-19-2014, https://doi.org/10.5194/sd-18-19-2014, 2014
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Short summary
The Collisional Orogeny in the Scandinavian Caledonides project provides insights into the deep structure and bedrock of a ca. 400 Ma old major orogen to study deformation processes that are hidden at depth from direct access in modern mountain belts. This paper describes the successful operations at the second site. It provides an overview of the retrieved geological section that differs from the expected and summarises the scientific potential of the accomplished data sets and drill core.
The Collisional Orogeny in the Scandinavian Caledonides project provides insights into the deep...
