Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Chaplygin I.[5]"'
Autor:
Deshaee A.[1], Shakeri A.[1], Taran Y.[2, Mehrabi B.[1], Farhadian M.[1], Zelenski M.[4], Chaplygin I.[5], Tassi F.[6
Publikováno v:
Journal of volcanology and geothermal research 390 (2020). doi:10.1016/j.jvolgeores.2019.106676
info:cnr-pdr/source/autori:Deshaee A.[1], Shakeri A.[1], Taran Y.[2,3], Mehrabi B.[1], Farhadian M.[1], Zelenski M.[4], Chaplygin I.[5], Tassi F.[6,7]/titolo:Geochemistry of Bazman thermal springs, southeast Iran/doi:10.1016%2Fj.jvolgeores.2019.106676/rivista:Journal of volcanology and geothermal research/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:390
info:cnr-pdr/source/autori:Deshaee A.[1], Shakeri A.[1], Taran Y.[2,3], Mehrabi B.[1], Farhadian M.[1], Zelenski M.[4], Chaplygin I.[5], Tassi F.[6,7]/titolo:Geochemistry of Bazman thermal springs, southeast Iran/doi:10.1016%2Fj.jvolgeores.2019.106676/rivista:Journal of volcanology and geothermal research/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:390
Thermal springs of the Bazman geothermal field, 27 km south of the Holocene Bazman volcano caldera in Makran continental margin, SE Iran, were studied for the first time. New data on major components,selected trace elements (Li, Rb, Cs, Ba, Sr, Fe, A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df39076388416a0c35bbe47a80803831
http://hdl.handle.net/2158/1182871
http://hdl.handle.net/2158/1182871
Autor:
Babadi M.[1], Mehrabi B.[1], Tassi F.[2, Cabassi J.[2, Vaselli O.[2, Shakeri A.[1], Pecchioni E.[2], Venturi S.[2], Zelenski M.[4], Chaplygin I. [5]
Publikováno v:
Marine and petroleum geology 106 (2019): 190–205. doi:10.1016/j.marpetgeo.2019.05.005
info:cnr-pdr/source/autori:Babadi M.[1], Mehrabi B.[1], Tassi F.[2,3], Cabassi J.[2,3], Vaselli O.[2,3], Shakeri A.[1], Pecchioni E.[2], Venturi S.[2], Zelenski M.[4], Chaplygin I. [5]/titolo:Origin of fluids discharged from mud volcanoes in SE Iran/doi:10.1016%2Fj.marpetgeo.2019.05.005/rivista:Marine and petroleum geology/anno:2019/pagina_da:190/pagina_a:205/intervallo_pagine:190–205/volume:106
info:cnr-pdr/source/autori:Babadi M.[1], Mehrabi B.[1], Tassi F.[2,3], Cabassi J.[2,3], Vaselli O.[2,3], Shakeri A.[1], Pecchioni E.[2], Venturi S.[2], Zelenski M.[4], Chaplygin I. [5]/titolo:Origin of fluids discharged from mud volcanoes in SE Iran/doi:10.1016%2Fj.marpetgeo.2019.05.005/rivista:Marine and petroleum geology/anno:2019/pagina_da:190/pagina_a:205/intervallo_pagine:190–205/volume:106
Onshore and offshore mud volcanism in the Makran accretionary prism is related to convergence of the Arabian and Eurasian plates. This study describes the chemical and isotopic composition of hydrocarbon-rich fluids from four active on-shore mud volc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::43f5e6ce37acee0c95a9fb9880c4da92
https://publications.cnr.it/doc/405300
https://publications.cnr.it/doc/405300