Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc
The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, a...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Julia, Frolova [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Umfang: |
16 |
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| Übergeordnetes Werk: |
Enthalten in: A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis - Lopez-Olivo, Maria A. ELSEVIER, 2022, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:183 ; year:2014 ; day:9 ; month:12 ; pages:80-95 ; extent:16 |
| Links: |
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| DOI / URN: |
10.1016/j.enggeo.2014.10.011 |
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| 520 | |a The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. | ||
| 520 | |a The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. | ||
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10.1016/j.enggeo.2014.10.011 doi GBVA2014020000024.pica (DE-627)ELV034221514 (ELSEVIER)S0013-7952(14)00266-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.83 bkl Julia, Frolova verfasserin aut Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc 2014transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. Vladimir, Ladygin oth Sergey, Rychagov oth David, Zukhubaya oth Enthalten in Elsevier Science Lopez-Olivo, Maria A. ELSEVIER A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis 2022 Amsterdam [u.a.] (DE-627)ELV008398631 volume:183 year:2014 day:9 month:12 pages:80-95 extent:16 https://doi.org/10.1016/j.enggeo.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.83 Rheumatologie Orthopädie VZ AR 183 2014 9 1209 80-95 16 045F 550 |
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10.1016/j.enggeo.2014.10.011 doi GBVA2014020000024.pica (DE-627)ELV034221514 (ELSEVIER)S0013-7952(14)00266-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.83 bkl Julia, Frolova verfasserin aut Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc 2014transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. Vladimir, Ladygin oth Sergey, Rychagov oth David, Zukhubaya oth Enthalten in Elsevier Science Lopez-Olivo, Maria A. ELSEVIER A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis 2022 Amsterdam [u.a.] (DE-627)ELV008398631 volume:183 year:2014 day:9 month:12 pages:80-95 extent:16 https://doi.org/10.1016/j.enggeo.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.83 Rheumatologie Orthopädie VZ AR 183 2014 9 1209 80-95 16 045F 550 |
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10.1016/j.enggeo.2014.10.011 doi GBVA2014020000024.pica (DE-627)ELV034221514 (ELSEVIER)S0013-7952(14)00266-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.83 bkl Julia, Frolova verfasserin aut Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc 2014transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. Vladimir, Ladygin oth Sergey, Rychagov oth David, Zukhubaya oth Enthalten in Elsevier Science Lopez-Olivo, Maria A. ELSEVIER A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis 2022 Amsterdam [u.a.] (DE-627)ELV008398631 volume:183 year:2014 day:9 month:12 pages:80-95 extent:16 https://doi.org/10.1016/j.enggeo.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.83 Rheumatologie Orthopädie VZ AR 183 2014 9 1209 80-95 16 045F 550 |
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10.1016/j.enggeo.2014.10.011 doi GBVA2014020000024.pica (DE-627)ELV034221514 (ELSEVIER)S0013-7952(14)00266-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.83 bkl Julia, Frolova verfasserin aut Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc 2014transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. Vladimir, Ladygin oth Sergey, Rychagov oth David, Zukhubaya oth Enthalten in Elsevier Science Lopez-Olivo, Maria A. ELSEVIER A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis 2022 Amsterdam [u.a.] (DE-627)ELV008398631 volume:183 year:2014 day:9 month:12 pages:80-95 extent:16 https://doi.org/10.1016/j.enggeo.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.83 Rheumatologie Orthopädie VZ AR 183 2014 9 1209 80-95 16 045F 550 |
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10.1016/j.enggeo.2014.10.011 doi GBVA2014020000024.pica (DE-627)ELV034221514 (ELSEVIER)S0013-7952(14)00266-X DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.83 bkl Julia, Frolova verfasserin aut Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc 2014transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. Vladimir, Ladygin oth Sergey, Rychagov oth David, Zukhubaya oth Enthalten in Elsevier Science Lopez-Olivo, Maria A. ELSEVIER A randomized controlled trial evaluating the effects of social networking on chronic disease management in rheumatoid arthritis 2022 Amsterdam [u.a.] (DE-627)ELV008398631 volume:183 year:2014 day:9 month:12 pages:80-95 extent:16 https://doi.org/10.1016/j.enggeo.2014.10.011 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.83 Rheumatologie Orthopädie VZ AR 183 2014 9 1209 80-95 16 045F 550 |
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effects of hydrothermal alterations on physical and mechanical properties of rocks in the kuril–kamchatka island arc |
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Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc |
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The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. |
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The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. |
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The hydrothermal systems of the Kuril–Kamchatka island arc are hosted in volcanic formations of Neogene–Quaternary age. Thermal water alters volcanic rocks and transforms them into hydrothermal rocks such as secondary quartzites, various propylites, zeolitic rocks, argillic rocks, clays, opalites, and quartz–feldspar metasomatites. Mineralogical alteration of rocks contributes to changes of their physical and mechanical properties. The relationship between type of hydrothermal alteration and rock properties is quite variable and depends on a number of factors including parent rocks, РТ-conditions, chemical composition and type of fluid, and duration of fluid–rock interaction. The study showed that high-temperature fluids cause consolidation and strengthening of rock, decrease in their porosity and permeability, and remove hygroscopic moisture. This tendency is observed independently of fluid chemical composition. Property variations caused by low-temperature subsurface fluids are more complicated and diverse but their “deterioration” prevails i.e. a decrease in density, strength and elastic modulus, formation of secondary porosity, high hygroscopy, softening and swelling in water saturated environment. |
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Effects of hydrothermal alterations on physical and mechanical properties of rocks in the Kuril–Kamchatka island arc |
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