Zobrazeno 1 - 10
of 16
pro vyhledávání: '"I. M. Villa"'
Publikováno v:
Solid Earth, Vol 14, Pp 551-570 (2023)
The Vinschgau Shear Zone (VSZ) is one of the largest and most significant shear zones developed under plastic conditions within the Austroalpine domain, juxtaposing the Ötztal and the Texel units to the Campo, Scharl and Sesvenna units during the bu
Externí odkaz:
https://doaj.org/article/5431a25f9e184b3ca3215f1553f50efb
Publikováno v:
Solid Earth, Vol 13, Pp 1803-1821 (2022)
Deformation of polymineralic aggregates can be accommodated by viscous granular flow, a process mediated by the interplay among intracrystalline plasticity and dissolution–precipitation, each active in specific minerals under given P–T conditions
Externí odkaz:
https://doaj.org/article/1be6e8f1859043a88d0a73e1c8b76106
Autor:
V. Peverelli, T. Ewing, D. Rubatto, M. Wille, A. Berger, I. M. Villa, P. Lanari, T. Pettke, M. Herwegh
Publikováno v:
Geochronology, Vol 3, Pp 123-147 (2021)
Epidote – here defined as minerals belonging to the epidote–clinozoisite solid solution – is a low-μ (μ=238U/204Pb) mineral occurring in a variety of geological environments and participating in many metamorphic reactions that is stable throu
Externí odkaz:
https://doaj.org/article/e3d35e708a484a0f828cf8259ebc79e5
Autor:
S. Mittempergher, S. Zanchetta, F. Caldiroli, A. Zanchi, A. Bistacchi, J. M. Hanchar, I. M. Villa
The Cenozoic Adamello batholith in the Southern Alps records solid-state deformation structures including, in order of decreasing relative age, cooling joints, shear zones and faults. In the present study we constrained age and duration of each phase
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2d9e5ed70ff3dc2a947a8f6d592bcd0
Autor:
null C. Fornacelli, null A. Briano, null L. Chiarantini, null G. Bianchi, null M. Benvenuti, null M. Giamello, null J. S. Kang, null I. M. Villa, null F. M. Talarico, null R. Hodges
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13f8e2ee1708f5554b5764e06c1431aa
https://doi.org/10.1111/arcm.12633/v3/response1
https://doi.org/10.1111/arcm.12633/v3/response1
Autor:
ROSSETTI, FEDERICO, F. BALSAMO, I. M. VILLA, M. BOUYBAOUENNE, FACCENNA, CLAUDIO, R. FUNICIELLO
This work presents the results from a multidisciplinary study carried out in the southern branch of the Larderello geothermal field (Travale-Montieri area) that is based on the integration of field data with information of the deeper structures as de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3668::f0e37eda6c4f656ca5be00f821043da2
https://hdl.handle.net/11590/117544
https://hdl.handle.net/11590/117544
Autor:
ROSSETTI, FEDERICO, F. BALSAMO, I. M. VILLA, M. BOUYBAOUENNE, FACCENNA, CLAUDIO, R. FUNICIELLO
This work presents the results of a multidiscipinary study carried out in the southern branch of the Larderello geothermal field (Travale – Montieri area), which was based on the integration of field data with information on the deeper structures
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3668::1e59ca0af81c09e1dcaa1110e7fd5bce
https://hdl.handle.net/11590/144307
https://hdl.handle.net/11590/144307
Autor:
I. M. Villa, J. L. Everard
Publikováno v:
Australian Journal of Earth Sciences. 41:265-272
The Crown Hill Andesite is one of several shallow subvolcanic hornblende‐phyric andesite/dacite intrusions, associated with similar lavas, which intrude both the Yolande River Sequence and Central Volcanic Complex units of the Mt Read Volcanics in
Autor:
Nicholas Christie-Blick, I. M. Villa
Publikováno v:
Episodes. 34:268-268