Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Claudio Robustelli Test"'
Autor:
Claudio Robustelli Test, Elena Zanella
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 12, Pp n/a-n/a (2021)
Abstract Heterogeneities in the magnetic signature along intraplate shear zones complicate their correlation with the physical processes that are involved in the geodynamic evolution of megathrusts. Isolating the preferred orientation of different ma
Externí odkaz:
https://doaj.org/article/3e452ce9a4474f968f7b74f626f4957c
Publikováno v:
Geosciences, Vol 9, Iss 9, p 381 (2019)
The strong morphological similitude of the block-in-matrix fabric of chaotic rock units (mélanges and broken formations) makes problematic the recognition of their primary forming-processes. We present results of the comparison between magnetic fabr
Externí odkaz:
https://doaj.org/article/77e242417a4846348549592f5bd94294
Autor:
Rasia Shajahan, Elena Zanella, Andrew J L Harris, Lodovico Drovanti, Claudio Robustelli Test, Sonia Calvari, Lucia Gurioli, Sara Mana, Benjamin van Wyk de Vries
Detailed rock magnetic, facies and textural analyses were carried out across the San Bartolo lava flow (Stromboli) to understand the flow dynamics of lava channel-fed 'a'a entering the water. Having been emplaced 3 ka, San Bartolo is the most recent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4376b1188b62abcc598509dbf4cafab
https://doi.org/10.5194/egusphere-egu23-1000
https://doi.org/10.5194/egusphere-egu23-1000
Autor:
Jean-Marie Prival, Andrew J.L. Harris, Elena Zanella, Claudio Robustelli Test, Lucia Gurioli, Oryaëlle Chevrel, Jonas Biren
Publikováno v:
Geological Society of America Bulletin
Geological Society of America Bulletin, 2022, ⟨10.1130/B36415.1⟩
Geological Society of America Bulletin, 2022, ⟨10.1130/B36415.1⟩
Emplacement dynamics of highly viscous, silicic lava flows remain poorly constrained due to a lack of consideration of crystal-rich cases. Emplacement models mostly apply to glassy or microlitic, vesiculated rhyolitic flows. However, crystalline, ves
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2302cdbf2ddddbf0515b81629faf764e
https://hdl.handle.net/2318/1889176
https://hdl.handle.net/2318/1889176
Deciphering the stress and strain distribution across plate boundary shear zones is critical to understanding the physical processes involved in the nucleation of megathrust faults and its behaviour. Plate boundaries at shallow depth represent comple
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e257ad6c1d1ec2251d640cb0ae3d458c
https://doi.org/10.5194/egusphere-egu21-1481
https://doi.org/10.5194/egusphere-egu21-1481
Autor:
Fernando Calamita, Evdokia Tema, Elena Zanella, Dorota Staneczek, Sara Satolli, Claudio Robustelli Test
The aim of this study is to investigate how structural deformation in shear zones is documented by the anisotropy of magnetic susceptibility (AMS). The study area is located in the Pliocene outer thrust of the Northern Apennines, which involved Creta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f93ae3aee7e14147738b07bc5cae9304
https://doi.org/10.5194/egusphere-egu21-1686
https://doi.org/10.5194/egusphere-egu21-1686
Autor:
Fernando Calamita, Dorota Staneczek, Elena Zanella, Claudio Robustelli Test, Evdokia Tema, Sara Satolli
We present the results of an integrated structural and anisotropy of magnetic susceptibility (AMS) investigation in calcareous and marly rocks from thrust shear zones. A total of 17 sites from six localities along the frontal and oblique ramp of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a7c1437fee29fc801e8e15504940e64
http://hdl.handle.net/2318/1766134
http://hdl.handle.net/2318/1766134
Publikováno v:
Geosciences, Vol 9, Iss 9, p 381 (2019)
Geosciences
Volume 9
Issue 9
Geosciences
Volume 9
Issue 9
The strong morphological similitude of the block-in-matrix fabric of chaotic rock units (mé
langes and broken formations) makes problematic the recognition of their primary forming-processes. We present results of the comparison between ma
langes and broken formations) makes problematic the recognition of their primary forming-processes. We present results of the comparison between ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c35852bff06a4c928ac73f842ea3f3e3
https://www.mdpi.com/2076-3263/9/9/381
https://www.mdpi.com/2076-3263/9/9/381