Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Ingo Heyde"'
Autor:
Małgorzata Ponikowska, Stanislaw Mazur, Tomasz Janik, Dariusz Wójcik, Michał Malinowski, Christian Hübscher, Ingo Heyde
Defining a transition zone between the Precambrian East European Craton (EEC) and the Palaeozoic West European Platform (WEP) is still a matter of discussion despite a large body of geophysical and geological data. The main tectonic feature of the tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d4e3bbfc51fb57332afba105abe69aa7
https://doi.org/10.5194/egusphere-egu22-7769
https://doi.org/10.5194/egusphere-egu22-7769
Autor:
Andreas Brotzer, Thomas Funck, Wolfram H. Geissler, Karsten Piepjohn, Ingo Heyde, Kai Berglar
Publikováno v:
Tectonophysics. 843:229588
Autor:
Ingo Heyde, Anouk Beniest, Udo Barckhausen, Mark D. Hannington, Michael Schnabel, Anna Jegen, Florian Schmid, Heidrun Kopp, Anke Dannowski
The Lau Basin is a young back-arc basin steadily forming at the Indo-Australian-Pacific plate boundary, where the Pacific plate is subducting underneath the Australian plate along the Tonga-Kermadec island arc. Roughly 25 Ma ago, roll-back of the Ker
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::afac44f257739d641f496f13f855f72a
https://doi.org/10.5194/egusphere-egu21-7605
https://doi.org/10.5194/egusphere-egu21-7605
Autor:
Christian Hübscher, Stanisław Mazur, Małgorzata Ponikowska, Michal Malinowski, Dariusz Wójcik, Ingo Heyde, Tomasz Janik
The southern Baltic Sea area is in the transition zone between the Fennoscandian Shield as part of the East European Craton (EEC) and the West European Platform. This area is characterised by a mosaic of various geological blocks separated by several
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cef8c440dee16db5fbcccbd8f0ea26ce
https://doi.org/10.5194/egusphere-egu2020-16237
https://doi.org/10.5194/egusphere-egu2020-16237
Autor:
Philipp A. Brandl, Ingo Heyde, Mark D. Hannington, Nico Augustin, Michael Riedel, Colin W. Devey, Florian Schmid, M. Engels, Anouk Beniest, Ingo Klaucke, Anke Dannowski, Michael Schnabel, Heidrun Kopp
Publikováno v:
[Poster] In: EGU General Assembly 2020, 03.05.-08.05.2020, Vienna, Austria .
The northeastern Lau Basin is one of the fastest opening and magmatically most active back-arc regions on Earth. Although the current pattern of plate boundaries and motions in this complex mosaic of microplates is fairly well understood, the structu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::37f3b0e493be5a0abbb745ba66d4ee73
https://doi.org/10.5194/egusphere-egu2020-1404
https://doi.org/10.5194/egusphere-egu2020-1404
Autor:
Kai Berglar, Rüdiger Lutz, Ingo Heyde, Wolfram Geissler, Peter Klitzke, Dieter Franke, Bernd Schreckenberger
Publikováno v:
Journal of Geodynamics. 118:154-165
We study the basement configuration in the slow-spreading Eurasia Basin, Arctic Ocean. Two multichannel seismic (MCS) profiles, which we acquired during ice-free conditions with a 3600 m long streamer, image the transition from the North Barents Sea
Autor:
Chiara Girolami, Massimiliano Rinaldo Barchi, Andrea Cannata, Ingo Heyde, Cristina Pauselli, Francesco Vetere
Publikováno v:
Geophysical Journal International. 211:865-882
Publikováno v:
International Journal of Earth Sciences. 107:177-190
In this study, we focus on structural configuration of the Entenschnabel area, a part of the German exclusive economic zone within the North Sea, by means of gravity and magnetic modelling. The starting point of the 3D modelling approach is published
Autor:
Peter Klitzke, Axel Ehrhardt, Rüdiger Lutz, Dieter Franke, Jan Inge Faleide, Ingo Heyde, Lutz Reinhardt
The evolution of the Olga Basin region in the northern Norwegian Barents Sea and its relation to the Caledonian and Timanian orogenies is poorly understood due to sparse geophysical data and the lack of well control. In 2015, the German Federal Insti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::129ed3b0a3a78d7d4839ebab691dff19
https://hdl.handle.net/10037/16794
https://hdl.handle.net/10037/16794
Publikováno v:
Tectonophysics. 691:31-47
The crustal structure and continental margin between southern Nares Strait and northern Baffin Bay were studied based on seismic refraction and gravity data acquired in 2010. We present the resulting P wave velocity, density and geological models of