[HTML][HTML] Authigenic greigite as an indicator of methane diffusion in gas hydrate-bearing sediments of the Hikurangi Margin, New Zealand
M Kars, A Greve, L Zerbst - Frontiers in Earth Science, 2021 - frontiersin.org
Authigenic ferrimagnetic iron sulfides, essentially greigite (Fe3S4), are commonly found in
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a by …
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a by …
Authigenic greigite as an indicator of methane diffusion in gas hydrate-bearing sediments of the Hikurangi Margin, New Zealand
M Kars, A Greve, L Zerbst - Frontiers in Earth Science, 2021 - ui.adsabs.harvard.edu
Authigenic ferrimagnetic iron sulfides, essentially greigite (Fe3S4), are commonly found in
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a by …
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a by …
Authigenic Greigite as an Indicator of Methane Diffusion in Gas Hydrate-Bearing Sediments of the Hikurangi Margin, New Zealand
M Kars, A Greve, L Zerbst - Frontiers in Earth …, 2021 - publikationen.bibliothek.kit.edu
Authigenic ferrimagnetic iron sulfides, essentially greigite (Fe $ _ {3} $ S $ _ {4} $), are
commonly found in gas hydrate-bearing marine sediments of active accretionary prisms …
commonly found in gas hydrate-bearing marine sediments of active accretionary prisms …
Authigenic Greigite as an Indicator of Methane Diffusion in Gas Hydrate-Bearing Sediments of the Hikurangi Margin, New Zealand
M Kars, A Greve, L Zerbst - Advances in Magnetism of Soils and …, 2021 - books.google.com
Authigenic ferrimagnetic iron sulfides, essentially greigite (Fe3S4), are commonly found in
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a byproduct …
gas hydrate-bearing marine sediments of active accretionary prisms. Greigite is a byproduct …