Zobrazeno 1 - 10
of 168
pro vyhledávání: '"Meccheri, M."'
Autor:
Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2, Brogi A.[4], Liotta D. [4, Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6
Publikováno v:
Sedimentary Geology 364 (2018): 180–203. doi:10.1016/j.sedgeo.2017.12.012
info:cnr-pdr/source/autori:Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2,3], Brogi A.[4], Liotta D. [4,5], Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6,8]/titolo:Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Golemezli travertine depositional system (western Anatolia, Turkey)/doi:10.1016%2Fj.sedgeo.2017.12.012/rivista:Sedimentary Geology/anno:2018/pagina_da:180/pagina_a:203/intervallo_pagine:180–203/volume:364
Università degli studi di Firenze-IRIS
info:cnr-pdr/source/autori:Capezzuoli E.[1], Ruggieri G.[2], Rimondi V.[2,3], Brogi A.[4], Liotta D. [4,5], Alcicek M.[6], Alcicek H.[6], Bulbul A.[6], Gandin A.[7], Meccheri M.[8], Shen C.[9], Baykara M. [6,8]/titolo:Calcite veining and feeding conduits in a hydrothermal system: Insights from a natural section across the Pleistocene Golemezli travertine depositional system (western Anatolia, Turkey)/doi:10.1016%2Fj.sedgeo.2017.12.012/rivista:Sedimentary Geology/anno:2018/pagina_da:180/pagina_a:203/intervallo_pagine:180–203/volume:364
Università degli studi di Firenze-IRIS
Linking the architecture of structural conduits with the hydrothermal fluids migrating from the reservoir up to the surface is a key-factor in geothermal research. A contribution to this achievement derives from the study of spring-related travertine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::696f546238756cc039b7bdc357071368
https://hdl.handle.net/11499/10859
https://hdl.handle.net/11499/10859
Autor:
Alcicek, H, Bulbul, A, Brogi, A, Liotta, D, Ruggieri, G, Capezzuoli, E, Meccheri, M, Yavuzer, I, Alcicek, MC
The Golemezli Geothermal Field (GGF) is one of the best known geothermal fields in western Anatolia (Turkey). The exploited fluids are of meteoric origin, mixed with deep magmatic fluids, which interacted with the metamorphic rocks of the Menderes Ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3566::35bd2d4fa6889c35391c2e235dc5d17a
http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/24638
http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/24638
Publikováno v:
The Journal of Geology, 1994 May 01. 102(3), 297-305.
Externí odkaz:
https://www.jstor.org/stable/30070515
Autor:
Brogi, A, Alcicek, MC, Yalciner, CC, Capezzuoli, E, Liotta, D, Meccheri, M, Rimondi, V, Ruggieri, G, Gandin, A, Boschi, C, Buyuksarac, A, Alcicek, H, Bulbul, A, Baykara, MO, Shen, CC
Coexistence of thermal springs, travertine deposits and tectonic activity is a recurring feature for most geothermal areas. Although such a certainty, their relationships are debated mainly addressing on the role of the tectonic activity in triggerin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::2ca5367860c38b4a6deba6f90a5e9100
http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/23109
http://acikerisim.pau.edu.tr:8080/xmlui/handle/11499/23109
Autor:
Pertusati, P., Musumeci, G., Carosi, R., Meccheri, M., Baroni, C., Capponi, G., Carmignani, L., Castelli, D., Colombo, F., Crispini, L., Di Vincenzo, G., Ghezzo, C. Gosso G., Lombardo, B., Montomoli, C., Montrasio, A., Oggiano, G., Perchiazzi, N., Rocchi, S., Salvini, F., Skinner, D. N. B., Talarico, F., Tessensohn, F., Casnedi, R., Kleinschmidt, G., Ricci, C. A., Roland, N. W., Roland N. W., M. Schmidt-Thomè
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3710::d045141c9597f641bd3d6e73252d1330
https://hdl.handle.net/11567/893736
https://hdl.handle.net/11567/893736
Autor:
Alçiçek C.[1], Brogi A.[2], Capezzuoli E.[3], Gandin A.[4], Liotta D.[2], Meccheri M.[4], Ruggieri G.[5]
Publikováno v:
Acta vulcanologica (Pisa, Online) 26/27 (2016): 123–135. doi:10.19272/201500102010
info:cnr-pdr/source/autori:Alçiçek C.[1], Brogi A.[2], Capezzuoli E.[3], Gandin A.[4], Liotta D.[2], Meccheri M.[4], Ruggieri G.[5]/titolo:Extensional structures and hydrothermal fluid flow in Western Anatolia: a review from the Neogene-Quaternary Dinar and Denizli Basins/doi:10.19272%2F201500102010/rivista:Acta vulcanologica (Pisa, Online)/anno:2016/pagina_da:123/pagina_a:135/intervallo_pagine:123–135/volume:26%2F27
info:cnr-pdr/source/autori:Alçiçek C.[1], Brogi A.[2], Capezzuoli E.[3], Gandin A.[4], Liotta D.[2], Meccheri M.[4], Ruggieri G.[5]/titolo:Extensional structures and hydrothermal fluid flow in Western Anatolia: a review from the Neogene-Quaternary Dinar and Denizli Basins/doi:10.19272%2F201500102010/rivista:Acta vulcanologica (Pisa, Online)/anno:2016/pagina_da:123/pagina_a:135/intervallo_pagine:123–135/volume:26%2F27
This paper focuses on the state of the art of two main research themes, developed through the collaboration between Italian and Turkish geoscientists, concerning the geological setting of western Anatolia: (i) the Neogene-Quaternary fault evolution;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::ddbd533cc280a42d4d18d029277c0ba0
http://www.cnr.it/prodotto/i/368432
http://www.cnr.it/prodotto/i/368432
Autor:
Brogi A.[1], Alçiçek M.C.[2], Yalçiner C.T.[3], Capezzuoli E.[4], Liotta D. [1, Meccheri M.[5], Rimondi V.[6], Ruggieri G.[7], Gandin A.[5], Boschi C.[7], Büyüksarac A.[8], Alçiçek H.[2], Bülbül A.[2], Baykara M.O.[2, Shen C.-C. [9]
Publikováno v:
Tectonophysics (Amst. Online) 680 (2016): 211–232. doi:10.1016/j.tecto.2016.05.003
info:cnr-pdr/source/autori:Brogi A.[1], Alçiçek M.C.[2], Yalçiner C.T.[3], Capezzuoli E.[4], Liotta D. [1,6], Meccheri M.[5], Rimondi V.[6], Ruggieri G.[7], Gandin A.[5], Boschi C.[7], Büyüksarac A.[8], Alçiçek H.[2], Bülbül A.[2], Baykara M.O.[2,9], Shen C.-C. [9]/titolo:Hydrothermal fluids circulation and travertine deposition in an active tectonic setting: Insights from the Kamara geothermal area (western Anatolia, Turkey)/doi:10.1016%2Fj.tecto.2016.05.003/rivista:Tectonophysics (Amst. Online)/anno:2016/pagina_da:211/pagina_a:232/intervallo_pagine:211–232/volume:680
info:cnr-pdr/source/autori:Brogi A.[1], Alçiçek M.C.[2], Yalçiner C.T.[3], Capezzuoli E.[4], Liotta D. [1,6], Meccheri M.[5], Rimondi V.[6], Ruggieri G.[7], Gandin A.[5], Boschi C.[7], Büyüksarac A.[8], Alçiçek H.[2], Bülbül A.[2], Baykara M.O.[2,9], Shen C.-C. [9]/titolo:Hydrothermal fluids circulation and travertine deposition in an active tectonic setting: Insights from the Kamara geothermal area (western Anatolia, Turkey)/doi:10.1016%2Fj.tecto.2016.05.003/rivista:Tectonophysics (Amst. Online)/anno:2016/pagina_da:211/pagina_a:232/intervallo_pagine:211–232/volume:680
Coexistence of thermal springs, travertine deposits and tectonic activity is a recurring feature for most geothermal areas. Although such a certainty, their relationships are debated mainly addressing on the role of the tectonic activity in triggerin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d967e7e37374de4c2725f389e85d7ae
https://aperta.ulakbim.gov.tr/record/58025
https://aperta.ulakbim.gov.tr/record/58025
Autor:
Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3, Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5, Vezzoli L.[8
Publikováno v:
Journal of volcanology and geothermal research 303 (2015): 1–6. doi:10.1016/j.jvolgeores.2015.07.004
info:cnr-pdr/source/autori:Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3,2], Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5,2], Vezzoli L.[8,2]/titolo:Comment on: "Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31/doi:10.1016%2Fj.jvolgeores.2015.07.004/rivista:Journal of volcanology and geothermal research/anno:2015/pagina_da:1/pagina_a:6/intervallo_pagine:1–6/volume:303
info:cnr-pdr/source/autori:Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3,2], Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5,2], Vezzoli L.[8,2]/titolo:Comment on: "Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31/doi:10.1016%2Fj.jvolgeores.2015.07.004/rivista:Journal of volcanology and geothermal research/anno:2015/pagina_da:1/pagina_a:6/intervallo_pagine:1–6/volume:303
Borgia et al. (2014) illustrated an active volcanic spreading model for the Amiata volcanic area (southern Tuscany, Italy). Although, at first glance, the model may appear appealing, this is not fully supported by the available data and the paper doe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1bc188ba886150402e588db9e4ee9626
https://publications.cnr.it/doc/334303
https://publications.cnr.it/doc/334303