Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis
We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Fedoseev, G.S. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017transfer abstract |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis - Mendu, Damodara Rao ELSEVIER, 2015, New York, NY |
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| Übergeordnetes Werk: |
volume:58 ; year:2017 ; number:8 ; pages:922-934 ; extent:13 |
| Links: |
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| DOI / URN: |
10.1016/j.rgg.2017.07.003 |
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| 520 | |a We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). | ||
| 520 | |a We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). | ||
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10.1016/j.rgg.2017.07.003 doi GBVA2017017000027.pica (DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Fedoseev, G.S. verfasserin aut Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis 2017transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). Vorontsov, A.A. oth Orekhov, A.A. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:58 year:2017 number:8 pages:922-934 extent:13 https://doi.org/10.1016/j.rgg.2017.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 58 2017 8 922-934 13 045F 550 |
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10.1016/j.rgg.2017.07.003 doi GBVA2017017000027.pica (DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Fedoseev, G.S. verfasserin aut Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis 2017transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). Vorontsov, A.A. oth Orekhov, A.A. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:58 year:2017 number:8 pages:922-934 extent:13 https://doi.org/10.1016/j.rgg.2017.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 58 2017 8 922-934 13 045F 550 |
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10.1016/j.rgg.2017.07.003 doi GBVA2017017000027.pica (DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Fedoseev, G.S. verfasserin aut Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis 2017transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). Vorontsov, A.A. oth Orekhov, A.A. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:58 year:2017 number:8 pages:922-934 extent:13 https://doi.org/10.1016/j.rgg.2017.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 58 2017 8 922-934 13 045F 550 |
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10.1016/j.rgg.2017.07.003 doi GBVA2017017000027.pica (DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Fedoseev, G.S. verfasserin aut Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis 2017transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). Vorontsov, A.A. oth Orekhov, A.A. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:58 year:2017 number:8 pages:922-934 extent:13 https://doi.org/10.1016/j.rgg.2017.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 58 2017 8 922-934 13 045F 550 |
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10.1016/j.rgg.2017.07.003 doi GBVA2017017000027.pica (DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 610 VZ 660 VZ 660 VZ 58.10 bkl Fedoseev, G.S. verfasserin aut Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis 2017transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). Vorontsov, A.A. oth Orekhov, A.A. oth Enthalten in Elsevier Mendu, Damodara Rao ELSEVIER D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis 2015 New York, NY (DE-627)ELV018845363 volume:58 year:2017 number:8 pages:922-934 extent:13 https://doi.org/10.1016/j.rgg.2017.07.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA GBV_ILN_40 58.10 Verfahrenstechnik: Allgemeines VZ AR 58 2017 8 922-934 13 045F 550 |
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Fedoseev, G.S. |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis |
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(DE-627)ELV040557049 (ELSEVIER)S1068-7971(17)30143-8 |
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Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis |
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Fedoseev, G.S. |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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D-lactic acidosis mediated neuronal encephalopathy in acute lymphoblastic leukemia patient: An under diagnosis |
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10.1016/j.rgg.2017.07.003 |
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fossil travertines and quasi-travertine in the minusa basin (west siberia): structure, composition, and comparative analysis |
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Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis |
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We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). |
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We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). |
| abstract_unstemmed |
We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite). |
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Fossil travertines and quasi-travertine in the Minusa basin (West Siberia): structure, composition, and comparative analysis |
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https://doi.org/10.1016/j.rgg.2017.07.003 |
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Vorontsov, A.A. Orekhov, A.A. |
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