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pro vyhledávání: '"Hawemann, Friedrich"'
Autor:
Hawemann, Friedrich1 (AUTHOR) friedrich.hawemann@erdw.ethz.ch, Mancktelow, Neil1 (AUTHOR), Wex, Sebastian1 (AUTHOR), Pennacchioni, Giorgio2 (AUTHOR), Camacho, Alfredo3 (AUTHOR)
Publikováno v:
Solid Earth. 2019, Vol. 10 Issue 5, p1635-1649. 15p.
Autor:
Hawemann, Friedrich1 (AUTHOR) friedrich.hawemann@erdw.ethz.ch, Mancktelow, Neil S.1 (AUTHOR), Wex, Sebastian1 (AUTHOR), Camacho, Alfredo2 (AUTHOR), Pennacchioni, Giorgio3 (AUTHOR)
Publikováno v:
Solid Earth. 2018, Vol. 9 Issue 3, p629-648. 20p.
Autor:
Hawemann, Friedrich
The localization of deformation in dry lower continental crust and the implied rheology have been investigated on the basis of field and laboratory observations from a well exposed and preserved section in Central Australia. The strength of the lower
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32e949b8bc084d2230476d017aea296b
Autor:
Auderset, Alexandra, Cafagna, Fabio, Echeverria Pazos, Leonardo, Elison, Patrick, Erlanger, Erica, Fomin, Ilya, Guitián, José, Hawemann, Friedrich, Kueter, Nico, Mandl, Maximilian, Mejía, Luz María, Moretti, Simone, Oestreicher, Nicolas Kyochi, Ott, Richard, Paneva, Nadezhda, Petschnig, Paul, Preuss, Simon, Reitano, Riccardo, Renz, Tobias, Revels, Brandi N., Wang, Yanyan, Winterberg, Sascha, Zhang, Hongrui
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::707072da3dff03d93dd7e89ec0a65c65
Autor:
Hawemann, Friedrich, Mancktelow, Neil, Wex, Sebastian, Camacho, Alfredo, Pennacchioni, Giorgio
Geophysical evidence for lower continental crustal earthquakes in almost all collisional orogens is in conflict with the widely accepted notion that rocks, under high grade conditions, should flow rather than fracture. Pseudotachylytes are remnants o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8e4d05fd9b403dbfe1ae4c8e1428a2ac
https://eartharxiv.org/c3s5g
https://eartharxiv.org/c3s5g
Autor:
Wex, Sebastian, Mancktelow, Neil, Hawemann, Friedrich, Camacho, Alfredo, Pennacchioni, Giorgio
The Musgrave Block in central Australia exposes numerous large-scale mylonitic shear zones developed during the intracontinental Petermann Orogeny around 560-520 Ma. The most prominent structure is the crustal-scale, over 600 km long, E-W-trending Wo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2d5fa9d4d019e404fecced327555ccc3
Autor:
Wex, Sebastian, Mancktelow, Neil S., Hawemann, Friedrich, Camacho, Alfredo, Pennacchioni, Giorgio
Publikováno v:
Tectonics, 36 (11)
ISSN:1944-9194
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2c2d735c9a8a308444484a8c8a876af8
http://hdl.handle.net/11577/3253538
http://hdl.handle.net/11577/3253538
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