Zobrazeno 1 - 10
of 52
pro vyhledávání: '"A. F. Burmester"'
Autor:
Nicholas E. Bader, McKenzie Elliott, Russell F. Burmester, Sarah Strozyk, Gabriella Elizabeth McGann, Molly Coates
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::977898274e15b57e09778ce127e2b7bd
https://doi.org/10.1130/abs/2021am-370154
https://doi.org/10.1130/abs/2021am-370154
Publikováno v:
Geological Society of America Bulletin. 128:1403-1422
The Himalayan syntaxes are exceptionally dynamic landscapes characterized by high-relief topography and some of the most rapid and focused crustal exhumation on Earth. In the eastern Himalayan syntaxis, it has been hypothesized that thermo-mechanical
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81683ac791ff3d22a264ab0e07d7d4e1
https://doi.org/10.1130/b31419.1
https://doi.org/10.1130/b31419.1
Autor:
Nicholas E. Bader, Russell F. Burmester, Gabriella Elizabeth McGann, Sarah Strozyk, Molly Coates, McKenzie Elliott
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cab5d8d450389bd969096af07bc13b06
https://doi.org/10.1130/abs/2019cd-329703
https://doi.org/10.1130/abs/2019cd-329703
Autor:
Bernard A. Housen, Esther Izquierdo-Llavall, Belén Oliva-Urcia, Russell F. Burmester, Emilio L. Pueyo, Antonio María Casas Sáinz
Publikováno v:
Zaguán. Repositorio Digital de la Universidad de Zaragoza
instname
instname
The Internal Sierras (IS) in the southern margin of the Western and Central Axial Zone (Southern Pyrenees) are affected by a syn-orogenic remagnetization that provides information to reconstruct deformation geometries at the time of acquisition of ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::94db441a9ca5fda0da34baa6baf8e76a
https://doi.org/10.1093/gji/ggv042
https://doi.org/10.1093/gji/ggv042
Autor:
Elizabeth R. Schermer, Russell F. Burmester, Juliet G. Crider, Bernard A. Housen, Rachel E. Dunham
Publikováno v:
Journal of Structural Geology. 33:1627-1638
Field, thin section, and magnetic fabric analyses of monoclinal, contractional kink bands in the Darrington Phyllite of northwestern Washington, USA, provide evidence of kinematic evolution and microstructural processes during kinking. Relationships
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b7d9077c941602dabff82d0990c2641
https://doi.org/10.1016/j.jsg.2011.08.010
https://doi.org/10.1016/j.jsg.2011.08.010
Publikováno v:
Canadian Journal of Earth Sciences. 47:1383-1404
The authors analyzed detrital zircon grains from 10 metasedimentary rock samples of the Priest River complex and three other amphibolite-facies metamorphic sequences in north-central Idaho to test the previous assignment of these rocks to the Mesopro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec3edff8a6a5dcc82b530fde46d101d1
https://doi.org/10.1139/e10-049
https://doi.org/10.1139/e10-049
Publikováno v:
Canadian Journal of Earth Sciences. 40:1335-1356
Documenting the timing and kinematics of deformation in orogens is critical to unraveling their history. Anisotropy of magnetic susceptibility defines the orientation of magnetic fabrics in the Eocene Cooper Mountain pluton in the North Cascade Mount
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::abbb0e240e55e0048c3038d353d952cc
https://doi.org/10.1139/e03-055
https://doi.org/10.1139/e03-055
Autor:
R. Sargent, T. Montgomery, Bernard A. Housen, G. Petro, D. Tucker, I. Mynatt, N. Liner, Myrl E. Beck, K. Addis, K. Curtis, J. Ladd, B. Molitor, T. Fawcett, Russell F. Burmester, B. Palmer, I. White
Publikováno v:
American Journal of Science. 303:263-299
We have collected 20 new paleomagnetic sites from the Mount Stuart batholith and the adjacent Beckler Peak stock. Using thermal and low-temperature demagnetization, and rock-magnetic tests, we have found that the remanence in most of the batholith is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::813e7187080219c7d5fa1ae8b30ef567
https://doi.org/10.2475/ajs.303.4.263
https://doi.org/10.2475/ajs.303.4.263