Details for: Vincenzo Stagno
-
Vincenzo Stagno (Sapienza University of Rome)
Goldschmidt Conference Archive Goldschmidt2017 Goldschmidt2019
No bio for this user.
Note: abstracts are only listed if one of the following email addresses was provided when the abstract was submitted: vincenzo.stagno@uniroma1.it. Otherwise, try an advanced search.
(2023) Redox Heterogeneities in the Archean Mantle Inferred from Mineral Inclusions in Siberian E-Type Diamonds: Implications for Volatile Speciation and Diamond Formation
Marras G, Mikhailenko D, McCammon C, Aulbach S, Logvinova A, Dominijanni S & Stagno V(2022) Co-evolution of Continental Mantle and Magmas, and Some Implications for Carbon Cycling
Aulbach S & Stagno V(2022) Viscosity Measurements of Magmas in the Earth’s Upper Mantle: Constraints on Rates and Ascent Timescales of a Primitive Alkaline Basalt
Bonechi B, Stagno V, Kono Y, Hrubiak R, Ziberna L, Andreozzi GB, Perinelli C & Gaeta M(2021) Chemical Geodynamics with Eclogite – P. Gast Medal Lecture
Aulbach S, Arndt NT, Gerdes A, Heaman LM, Höfer HE, Stagno V, Stern RA, Viljoen F & Woodland AB(2019) The Redox State of the Graphite- and Diamond-Bearing Eclogite Xenoliths from Udachnaya Kimberlite Pipe (Siberian Craton): Implication for the Origin of Diamonds
Mikhailenko D, Stagno V, Korsakov A, Andreozzi G, Cerantola V, Marras G, Golovin A & Malygina E(2019) Viscosity and Atomic Structure of CO2-bearing Magmas in the Earth’s Interior
Stagno V, Stopponi V, Kono Y, Romano C, Poe BT, Lupi S, D'Arco A, Hrubiak R, Scarlato P, Bonechi B, Perinelli C, Gaeta M & Manning CE(2017) Do Fe-Bearing Minerals Control the Deep Carbon Cycle in the Interior of the Earth?
Stagno V, McCammon CA, Cerantola V, Andreozzi GB, Caruso M, Arimoto T & Irifune T(2017) From Carbon in Meteorites to Carbonatite Rocks on Earth
Stagno V, Kono Y, Greaux S, Kebukawa Y, Stopponi V, Scarlato P, Lustrino M & Irifune T(2017) Melting Temperature of Tagish Lake (CI2) Meteorite from 5 to 30 GPa
Greaux S, Stagno V & Irifune T(2017) The Transition from Carbonatitic to Carbonate-Silicate Magmas in Carbonated Eclogite Rocks as Function of Pressure, Temperature and Oxygen Fugacity
Caruso M & Stagno V(2016) Melting of Tagish Lake Meteorite at High Pressure: Implications for the Fate of the Carbonaceous Matter during Planetary Accretion
Stagno V, Du W, Kebukawa Y & Irifune T(2023) Redox Heterogeneities in the Archean Mantle Inferred from Mineral Inclusions in Siberian E-Type Diamonds: Implications for Volatile Speciation and Diamond Formation
Marras G, Mikhailenko D, McCammon C, Aulbach S, Logvinova A, Dominijanni S & Stagno V(2022) Viscosity Measurements of Magmas in the Earth’s Upper Mantle: Constraints on Rates and Ascent Timescales of a Primitive Alkaline Basalt
Bonechi B, Stagno V, Kono Y, Hrubiak R, Ziberna L, Andreozzi GB, Perinelli C & Gaeta M(2022) Co-evolution of Continental Mantle and Magmas, and Some Implications for Carbon Cycling
Aulbach S & Stagno V(2021) Chemical Geodynamics with Eclogite – P. Gast Medal Lecture
Aulbach S, Arndt NT, Gerdes A, Heaman LM, Höfer HE, Stagno V, Stern RA, Viljoen F & Woodland AB(2019) Viscosity and Atomic Structure of CO2-bearing Magmas in the Earth’s Interior
Stagno V, Stopponi V, Kono Y, Romano C, Poe BT, Lupi S, D'Arco A, Hrubiak R, Scarlato P, Bonechi B, Perinelli C, Gaeta M & Manning CE(2019) The Redox State of the Graphite- and Diamond-Bearing Eclogite Xenoliths from Udachnaya Kimberlite Pipe (Siberian Craton): Implication for the Origin of Diamonds
Mikhailenko D, Stagno V, Korsakov A, Andreozzi G, Cerantola V, Marras G, Golovin A & Malygina E(2017) Do Fe-Bearing Minerals Control the Deep Carbon Cycle in the Interior of the Earth?
Stagno V, McCammon CA, Cerantola V, Andreozzi GB, Caruso M, Arimoto T & Irifune T(2017) From Carbon in Meteorites to Carbonatite Rocks on Earth
Stagno V, Kono Y, Greaux S, Kebukawa Y, Stopponi V, Scarlato P, Lustrino M & Irifune T(2017) The Transition from Carbonatitic to Carbonate-Silicate Magmas in Carbonated Eclogite Rocks as Function of Pressure, Temperature and Oxygen Fugacity
Caruso M & Stagno V(2017) Melting Temperature of Tagish Lake (CI2) Meteorite from 5 to 30 GPa
Greaux S, Stagno V & Irifune T(2016) Melting of Tagish Lake Meteorite at High Pressure: Implications for the Fate of the Carbonaceous Matter during Planetary Accretion
Stagno V, Du W, Kebukawa Y & Irifune TMentorship
Goldschmidt2019: Mentor (Mentoring Ke Zhu)
Goldschmidt2017: Mentor (Mentoring Levente Patkó)