Mineralogical and isotopic analysis of authigenic carbonates from different gas hydrate-bearing
seepage structures in the Derugin Basin (Sea of Okhotsk) are presented. The analysis showed the
existence of four morphological types of carbonates, with all of them mainly of Mg-calcite.13C
values of carbonates generally light owing to the inheritance of carbon from microbial methane.
13C-enriched samples at the VNIIOkeangeologia structure with 13C values of up to +9.3‰
represent carbonate precipitation due to methanogenesis. The calculated equilibrium 18O values
of carbonates in general correspond to measured values.
| Identifer | oai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:BVAU.2429/1173 |
| Date | 07 1900 |
| Creators | Krylov, Alexey, Logvina, Elizaveta, Hachikubo, Akihiro, Minami, Hirotsugu, Nunokawa, Yutaka, Shoji, Hitoshi, Mazurenko, Leonid, Matveeva, Tatyana, Obzhirov, Anatoly, Jin, Young Keun |
| Source Sets | Library and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada |
| Language | English |
| Detected Language | English |
| Type | text |
| Rights | Krylov, Alexey |
Page generated in 0.0023 seconds