| Attributes | Values |
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| rdf:type
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| Description
| - Skupina bahenních sopek byla objevena v SZ části Gibijského Altaje na severním úpatí pohoří Khar Argalantyn Nuruu. Zdrojem bahenních sopek je sled jurských až kvartérních sedimentů. Jurské dedimenty transgresivně nasedají na permské vulkanity a tvoří několik napjatých kolektorů uvnitř zakleslé kry. Bahenní sopky vznikly pravděpodobně jako výsledek Gob-Altajského zemětřesení v roce 1957. Toto zemětřesení s magnitudem 8,3 vytvořilo nové pukliny a otevřelo pukliny staré. Zemětřesný impuls překročil tixotropii jemnozrnných sedimetů a inicioval vznik bahenních sopek. Současná rovnováha tlakových podmínek na lokalitě je slabá. Zemětřesení nebo zvýšení piezometrického tlaku po velkých deštích může iniciovat aktivitu bahenních sopek. Vysoký obsah smektitů v sedimentech a ztráta soudržnosti jílových částic při rozpoštění solí podporují činnost bahenních sopek. (cs)
- A group of mud volcanoes was discovered in the NW part of the Gobi Altay on a northern foothill of the Khar Argalantyn Nuruu Mts. Jurassic to Quaternary sedimentary successions provide the source for the mud volcanoes. Jurassic sediments cover transgressively Permian volcanics forming several confined aquifers within a subsided, triangle shaped block. The mud volcanoes originated probably as a result of the Gobi-Altay Earthquake in 1957. The earthquake of magnitude 8.3 generated new fractures or reactivated existing fractures. The impulse of the earthquake exceeding the thixotropy of fine-grained sediments initiated the rise of the mud volcanoes. The recent equilibrium of pressure conditions in the area is labile. Earthquakes or increase in piezometric level of groundwater caused by heavy rainfalls can trigger activity of the mud volcanoes. A high content of smectites in sediments and loss of binding of clay particles due to soluble salts support mud outflows during such starting events.
- A group of mud volcanoes was discovered in the NW part of the Gobi Altay on a northern foothill of the Khar Argalantyn Nuruu Mts. Jurassic to Quaternary sedimentary successions provide the source for the mud volcanoes. Jurassic sediments cover transgressively Permian volcanics forming several confined aquifers within a subsided, triangle shaped block. The mud volcanoes originated probably as a result of the Gobi-Altay Earthquake in 1957. The earthquake of magnitude 8.3 generated new fractures or reactivated existing fractures. The impulse of the earthquake exceeding the thixotropy of fine-grained sediments initiated the rise of the mud volcanoes. The recent equilibrium of pressure conditions in the area is labile. Earthquakes or increase in piezometric level of groundwater caused by heavy rainfalls can trigger activity of the mud volcanoes. A high content of smectites in sediments and loss of binding of clay particles due to soluble salts support mud outflows during such starting events. (en)
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| Title
| - Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity
- Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity (en)
- Bahenní sopky v pohoří Khar Argalantyn Nuruu, SZ Gobi Altaj, Mongolsko jako projev současné seismické aktivity (cs)
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| skos:prefLabel
| - Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity
- Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity (en)
- Bahenní sopky v pohoří Khar Argalantyn Nuruu, SZ Gobi Altaj, Mongolsko jako projev současné seismické aktivity (cs)
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| skos:notation
| - RIV/00025798:_____/08:00000217!RIV09-MZP-00025798
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| http://linked.open...avai/riv/aktivita
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| http://linked.open...avai/riv/aktivity
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| http://linked.open...iv/cisloPeriodika
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| http://linked.open...vai/riv/dodaniDat
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| http://linked.open...aciTvurceVysledku
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| http://linked.open.../riv/druhVysledku
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| http://linked.open...iv/duvernostUdaju
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| http://linked.open...titaPredkladatele
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| http://linked.open...dnocenehoVysledku
| |
| http://linked.open...ai/riv/idVysledku
| - RIV/00025798:_____/08:00000217
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| http://linked.open...riv/jazykVysledku
| |
| http://linked.open.../riv/klicovaSlova
| - mud volcano, liquefaction, thixotropy, earthquake, Gobi Altay, Mongolia (en)
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| http://linked.open.../riv/klicoveSlovo
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| http://linked.open...odStatuVydavatele
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| http://linked.open...ontrolniKodProRIV
| |
| http://linked.open...i/riv/nazevZdroje
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| http://linked.open...in/vavai/riv/obor
| |
| http://linked.open...ichTvurcuVysledku
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| http://linked.open...cetTvurcuVysledku
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| http://linked.open...UplatneniVysledku
| |
| http://linked.open...v/svazekPeriodika
| |
| http://linked.open...iv/tvurceVysledku
| - Rukavičková, Lenka
- Hanžl, Pavel
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| issn
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| number of pages
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| is http://linked.open...avai/riv/vysledek
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