Zobrazeno 1 - 5
of 5
pro vyhledávání: '"M. S. Zechmeister"'
Publikováno v:
Geosphere. 8:1146-1169
Tectonic models for Borneo’s Cenozoic evolution differ in several aspects, particularly in the extent to which they include paleomagnetic data suggestive of strong counterclockwise rotation between 30 and 10 Ma. Key areas are undersampled. We prese
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9039ffc8af69fc7e49adc5b09f0d7532
https://doi.org/10.1130/ges00750.1
https://doi.org/10.1130/ges00750.1
Publikováno v:
Geological Society, London, Special Publications. 371:123-144
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::72ed52db32b921048a0881e3782f1af6
https://doi.org/10.1144/sp371.11
https://doi.org/10.1144/sp371.11
Publikováno v:
Journal of Structural Geology. 29:1114-1130
The Dora Maira Massif (DM), Western Alps is a type example of an ultra-high pressure (UHP) metamorphic terrain. The occurrence of pseudotachylytes within the Val Gilba area of DM led to speculation regarding the role of seismic slip in the exhumation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bc0b2b067ddc9c1bb3ca355e2faada6
https://doi.org/10.1016/j.jsg.2007.03.009
https://doi.org/10.1016/j.jsg.2007.03.009
Autor:
Eric C. Ferré, John W. Geissman, Mimi J. Hill, François Demory, M. S. Zechmeister, J. Gattacceca
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, 2014, 119 (8), pp.6113-6135. ⟨10.1002/2014JB011168⟩
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2014, 119 (8), pp.6113-6135. ⟨10.1002/2014JB011168⟩
Journal of Geophysical Research : Solid Earth, 2014, 119 (8), pp.6113-6135. ⟨10.1002/2014JB011168⟩
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2014, 119 (8), pp.6113-6135. ⟨10.1002/2014JB011168⟩
Fault pseudotachylytes form by quenching of silicate liquids produced through coseismic frictional melting. Here we show that in natural pseudotachylytes the main carrier of magnetic remanence blocked in during cooling of the frictional melt is fine-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3a960eca4b47eaed5c2b821fb128e16f
https://hal.science/hal-01735723
https://hal.science/hal-01735723
Publikováno v:
Journal of Geophysical Research: Solid Earth. 117
[1] We investigate the petrographic, geochemical and magnetic properties of fault pseudotachylytes formed by frictional melting in granitic rocks from Southern California, the Italian Alps and Kyushyu, Japan. The main magnetic remanence carriers are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e850e2faa46bd9fe16ac1139453ef384
https://doi.org/10.1029/2011jb008762
https://doi.org/10.1029/2011jb008762