Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Karolina Kośmińska"'
Autor:
Riccardo Callegari, Abigail K. Barker, Christopher J. Barnes, Katarzyna Walczak, Grzegorz Ziemniak, Iwona Klonowska, Ellen Kooijman, Sabine Rousku, Karolina Kośmińska, Jarosław Majka
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
The Central Iapetus Magmatic Province (CIMP) is a large igneous province (LIP) emplaced in the Baltican and Laurentian paleocontinents that marks the onset of the Caledonian Wilson Cycle. Paleozoic magmatism of the CIMP is preserved in both northeast
Externí odkaz:
https://doaj.org/article/895fb6dc09ae496dbde03b6fe01af999
Autor:
Michał Bukała, Christopher J. Barnes, Pauline Jeanneret, Károly Hidas, Stanisław Mazur, Bjarne S. G. Almqvist, Karolina Kośmińska, Iwona Klonowska, Juraj Šurka, Jarosław Majka
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
The Tsäkkok Lens of the Scandinavian Caledonides represents the outermost Baltican margin that was subducted in late Cambrian/Early Ordovician time during closure of the Iapetus Ocean. The lens predominantly consists of metasedimentary rocks hosting
Externí odkaz:
https://doaj.org/article/b46bf0871fec4cf5b5e277ce5871e716
Autor:
Riccardo Callegari, Karolina Kośmińska, Iwona Klonowska, Christopher J. Barnes, Jarosław Majka
The Middle Allochthon of the Scandinavian Caledonides represents the Neoproterozoic distal continental passive margin intruded by a dyke swarm with minor Mesoproterozoic and Paleoproterozoic orthogneiss. Locally, it carries early Neoproterozoic pluto
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec983db667d21c292bb6ff127b0e7298
https://doi.org/10.5194/egusphere-egu23-13021
https://doi.org/10.5194/egusphere-egu23-13021
The Pearya Terrane of northern Ellesmere Island is composed of a Tonian crystalline arc, Neoproterozoic to Paleozoic sedimentary successions, an Ordovician island arc complex and related volcaniclastics, and middle Ordovician to Silurian sedimentary
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60288035efb03ab17dd1079f937b0864
https://doi.org/10.5194/egusphere-egu23-8869
https://doi.org/10.5194/egusphere-egu23-8869
Autor:
Olga Turek, Karolina Kośmińska
The Bogegga Formation crops out on Oscar II Land in the western part of Svalbard archipelago. It is part of the Kongsvegen Group which belongs to the Southwestern Basement Province. This unit contains garnet-bearing mica schists and gneisses, pegmati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dbcbdd222ea83873c6bbda14ac0668f0
https://doi.org/10.5194/egusphere-egu23-6510
https://doi.org/10.5194/egusphere-egu23-6510
Autor:
Karolina Kośmińska, Jarosław Majka
The pressure-temperature-time (P-T-t) history of a blueschist and an eclogite from the high pressure-low temperature Vestgötabreen Complex, Svalbard, has been constrained using the conventional geothermobarometry, trace elements thermometry, and ela
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e71a1e9344021bbd21836824b8944c9
https://doi.org/10.5194/egusphere-egu23-2038
https://doi.org/10.5194/egusphere-egu23-2038
Autor:
Ludwik de Doliwa Zieliński, Michał Bukała, Jakub Bazarnik, Mateusz Mikołajczak, Karolina Kośmińska, Jarosław Majka
The crystalline basement of the Tatra Mountains belongs to the northernmost part of the Tatric unit of the Western Carpathians and is composed of pre-Mesozoic crystalline rocks, overlain by Mesozoic and Cenozoic sedimentary cover and nappes. Metamorp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3c5a5dc7cfc219ad3075501b4e78f63
https://doi.org/10.5194/egusphere-egu23-6470
https://doi.org/10.5194/egusphere-egu23-6470
Autor:
Stanislaw Mazur, Jarosław Majka, Christopher J. Barnes, William McClelland, Michał Bukała, Marian Janák, Karolina Kośmińska
Publikováno v:
Terra Nova. 34:330-339
Autor:
Jakub Bazarnik, Karolina Kośmińska, William C. McClelland, Justin V. Strauss, Karsten Piepjohn, Synnøve Elvevold, Grzegorz Zieliński, Jarosław Majka
Publikováno v:
Canadian Journal of Earth Sciences.
Tectonic models for development of the Svalbard Caledonides depend on reliable assessment of the metamorphic evolution of the various basement provinces involved. The Mosselhalvøya Group (MG) and the Atomfjella Complex (AC) have previously been assi
Autor:
Pauline Jeanneret, Iwona Klonowska, Christopher Barnes, Jarosław Majka, Johanna Holmberg, Mattia Gilio, William Nachlas, Matteo Alvaro, Karolina Kośmińska, Henning Lorenz, Thomas Zack, Anna Ladenberger, Hemin Koyi
The Seve Nappe Complex is a subduction-related high-grade metamorphic unit that was emplaced onto the margin of Baltica during Caledonian orogenesis. In this paper, the tectonometamorphic evolution of the Lower Seve Nappe in the Scandinavian Caledoni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f71ada50d09c526a62dd3cab71f9545c
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-496712
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-496712