The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter
Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this flu...
Ausführliche Beschreibung
Autor*in: |
Maksimov, S. O. [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2016 |
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Anmerkung: |
© Pleiades Publishing, Ltd. 2016 |
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Übergeordnetes Werk: |
Enthalten in: Doklady earth sciences - Pleiades Publishing, 1998, 466(2016), 2 vom: Feb., Seite 142-147 |
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Übergeordnetes Werk: |
volume:466 ; year:2016 ; number:2 ; month:02 ; pages:142-147 |
Links: |
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DOI / URN: |
10.1134/S1028334X16020070 |
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Katalog-ID: |
OLC2040791205 |
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10.1134/S1028334X16020070 doi (DE-627)OLC2040791205 (DE-He213)S1028334X16020070-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Maksimov, S. O. verfasserin aut The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2016 Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. Olivine Cerium Tephra DOKLADY Earth Science Carbonaceous Shale Safronov, P. P. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 466(2016), 2 vom: Feb., Seite 142-147 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:466 year:2016 number:2 month:02 pages:142-147 https://doi.org/10.1134/S1028334X16020070 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 466 2016 2 02 142-147 |
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10.1134/S1028334X16020070 doi (DE-627)OLC2040791205 (DE-He213)S1028334X16020070-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Maksimov, S. O. verfasserin aut The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2016 Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. Olivine Cerium Tephra DOKLADY Earth Science Carbonaceous Shale Safronov, P. P. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 466(2016), 2 vom: Feb., Seite 142-147 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:466 year:2016 number:2 month:02 pages:142-147 https://doi.org/10.1134/S1028334X16020070 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 466 2016 2 02 142-147 |
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10.1134/S1028334X16020070 doi (DE-627)OLC2040791205 (DE-He213)S1028334X16020070-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Maksimov, S. O. verfasserin aut The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2016 Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. Olivine Cerium Tephra DOKLADY Earth Science Carbonaceous Shale Safronov, P. P. aut Enthalten in Doklady earth sciences Pleiades Publishing, 1998 466(2016), 2 vom: Feb., Seite 142-147 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:466 year:2016 number:2 month:02 pages:142-147 https://doi.org/10.1134/S1028334X16020070 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 466 2016 2 02 142-147 |
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the formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter |
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The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter |
abstract |
Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. © Pleiades Publishing, Ltd. 2016 |
abstractGer |
Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. © Pleiades Publishing, Ltd. 2016 |
abstract_unstemmed |
Abstract The processes of fluid destruction of various silicate rocks under diffusion of flows of compressed gases (mainly carbonaceous) were studied. The gas condensate nature was ascertained for the forming alumoslilicate and ore (cobalt–iron–manganese hydroxide) substances produced under this fluid destruction in the forms of microcrusts and microconcretions. The ore condensates contained in high concentrations the typomorphic elements of oceanic ferromanganese formations (Mn, Co, Ni, Cu, Pb, Ce, and Pt). The elemental composition of the ore oxide substance formed under the destruction of various silicate matrices exhibits a definite degree of endemism with prevalence of the Co–Mn association. The pronounced concentration of barium is related to the substantially carbonaceous composition of the fluid systems. A cerium paradox is revealed: $ Ce^{3+} $ is oxidized into $ Ce^{4+} $ and absorbed by ferromanganese hydrogel and the minimum of cerium appears in rare-earth phosphates. © Pleiades Publishing, Ltd. 2016 |
collection_details |
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container_issue |
2 |
title_short |
The formation of cobalt-bearing ferromanganese crusts under fluid destruction of silicate matter |
url |
https://doi.org/10.1134/S1028334X16020070 |
remote_bool |
false |
author2 |
Safronov, P. P. |
author2Str |
Safronov, P. P. |
ppnlink |
242069096 |
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hochschulschrift_bool |
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doi_str |
10.1134/S1028334X16020070 |
up_date |
2024-07-04T03:08:14.055Z |
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