Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Oblique fault"'
Autor:
Eulogio Pardo-Igúzquiza, Juan Antonio Luque-Espinar, Carlos Sanz de Galdeano, Juan José Durán-Valsero
Publikováno v:
Discover Geoscience, Vol 2, Iss 1, Pp 1-20 (2024)
Abstract The mountainous karst massif in the Sierra de las Nieves (southern Spain) and the adjacent large outcrops of subcontinental mantle peridotites provide this area with a distinctive geodiversity that has contributed to the recent declaration o
Externí odkaz:
https://doaj.org/article/901e3bc9a8a74d6c8e60b2d505004bfd
Akademický článek
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Publikováno v:
Geodinamica Acta, Vol 29, Iss 1, Pp 1-19 (2017)
Fissure-ridge travertines (FRTs) are of great importance for the determination and comparison of tectonic deformation in a region. The coeval development of these travertines with active fault zones supplies significant information about regional dyn
Externí odkaz:
https://doaj.org/article/2ee24d051faa4b39ac406f08b035d842
Publikováno v:
Geothermics 89 (2021): 1–17. doi:10.1016/j.geothermics.2020.101941
info:cnr-pdr/source/autori:Brogi A.[1,2], Alçiçek M.C.[3], Liotta D.[1,2], Capezzuoli E.[4], Zucchi M.[1], Matera P.F.[1]/titolo:Step-over fault zones controlling geothermal fluid-flow and travertine formation (Denizli Basin, Turkey)/doi:10.1016%2Fj.geothermics.2020.101941/rivista:Geothermics/anno:2021/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:89
info:cnr-pdr/source/autori:Brogi A.[1,2], Alçiçek M.C.[3], Liotta D.[1,2], Capezzuoli E.[4], Zucchi M.[1], Matera P.F.[1]/titolo:Step-over fault zones controlling geothermal fluid-flow and travertine formation (Denizli Basin, Turkey)/doi:10.1016%2Fj.geothermics.2020.101941/rivista:Geothermics/anno:2021/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:89
In the Honalilar area (Denizli Basin, Turkey), the occurrence of banded Ca-carbonate veins and travertine deposits, represented by a dismantled fissure ridge-type depositional system, are the evidence of a middle-late Pleistocene exhumed, shallow, hy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3eb06e7bc6605e2c8ca6bd2beafff359
https://doi.org/10.1016/j.geothermics.2020.101941
https://doi.org/10.1016/j.geothermics.2020.101941
WOS: 000425202000011
The west to southwestward motion of the Anatolian block results from the relative motions between the Eurasian, Arabian and African plates along the right-lateral North Anatolian Fault Zone in the north and left lateral East
The west to southwestward motion of the Anatolian block results from the relative motions between the Eurasian, Arabian and African plates along the right-lateral North Anatolian Fault Zone in the north and left lateral East
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b5ec4fff24de0e89ca9c897626132c95
https://hdl.handle.net/20.500.12508/671
https://hdl.handle.net/20.500.12508/671
Akademický článek
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Publikováno v:
Geodinamica Acta
Geodinamica Acta, Taylor & Francis, 2017, 29 (1), pp.1-19. ⟨10.1080/09853111.2016.1228037⟩
Geodinamica Acta, Vol 29, Iss 1, Pp 1-19 (2017)
Geodinamica Acta, 2017, 29 (1), pp.1-19. ⟨10.1080/09853111.2016.1228037⟩
Geodinamica Acta, Taylor & Francis, 2017, 29 (1), pp.1-19. ⟨10.1080/09853111.2016.1228037⟩
Geodinamica Acta, Vol 29, Iss 1, Pp 1-19 (2017)
Geodinamica Acta, 2017, 29 (1), pp.1-19. ⟨10.1080/09853111.2016.1228037⟩
International audience; Fissure-ridge travertines (FRTs) are of great importance for the determination and comparison of tectonic deformation ina region. The coeval development of these travertines with active fault zones supplies significant informa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62067a82dc993d9a9248c95e72bb213a
http://hdl.handle.net/11655/18919
http://hdl.handle.net/11655/18919
Publikováno v:
Journal of Computational and Applied Mathematics. 140(1-2):559-585
The purpose of this paper is to study the problem of detection of vertical and oblique faults in explicit surfaces. First, we characterize the finite jump discontinuities of a univariate function in terms of the divergence of sequences related to the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e08e1e6b5534f2d02fe920fb4d6bdda6
Publikováno v:
Quaternary international 332 (2014): 99–114. doi:10.1016/j.quaint.2013.11.011
info:cnr-pdr/source/autori:Ferranti, Luigi; Passaro, Salvatore; de Alteriis, Giovanni/titolo:Morphotectonics of the Gorringe Bank summit, eastern Atlantic Ocean, based on high-resolution multibeam bathymetry/doi:10.1016%2Fj.quaint.2013.11.011/rivista:Quaternary international/anno:2014/pagina_da:99/pagina_a:114/intervallo_pagine:99–114/volume:332
info:cnr-pdr/source/autori:Ferranti, Luigi; Passaro, Salvatore; de Alteriis, Giovanni/titolo:Morphotectonics of the Gorringe Bank summit, eastern Atlantic Ocean, based on high-resolution multibeam bathymetry/doi:10.1016%2Fj.quaint.2013.11.011/rivista:Quaternary international/anno:2014/pagina_da:99/pagina_a:114/intervallo_pagine:99–114/volume:332
High-resolution swath bathymetry of the Gorringe Bank, located along the Europe-Africa obliquely convergent plate boundary offshore SW Portugal, allowed investigation of its shallow-depth morphotectonic structure as a contribution to understanding th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2e4d6b3f1f4ce87ff910ed0bec581136
https://publications.cnr.it/doc/295616
https://publications.cnr.it/doc/295616
Autor:
Alessandra Di Domenica, Fernando Calamita, Fabio Trippetta, Eugenio Carminati, Patrizio Petricca
Publikováno v:
Journal of Structural Geology
Within inversion tectonic contexts, the reactivation of pre-existing discontinuities depends upon many structural, stratigraphic and mechanical factors. Among these, a fundamental aspect is represented by the orientation and attitude of pre-existing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::594fb14ae85e255dcaf70643a19344bf
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:664898
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:664898