"V" . "Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity"@en . "1802-6222" . "2"^^ . "Rukavi\u010Dkov\u00E1, Lenka" . "RIV/00025798:_____/08:00000217!RIV09-MZP-00025798" . . . "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." . . . . "2"^^ . . "Bahenn\u00ED sopky v poho\u0159\u00ED Khar Argalantyn Nuruu, SZ Gobi Altaj, Mongolsko jako projev sou\u010Dasn\u00E9 seismick\u00E9 aktivity"@cs . . . . "Skupina bahenn\u00EDch sopek byla objevena v SZ \u010D\u00E1sti Gibijsk\u00E9ho Altaje na severn\u00EDm \u00FApat\u00ED poho\u0159\u00ED Khar Argalantyn Nuruu. Zdrojem bahenn\u00EDch sopek je sled jursk\u00FDch a\u017E kvart\u00E9rn\u00EDch sediment\u016F. Jursk\u00E9 dedimenty transgresivn\u011B nasedaj\u00ED na permsk\u00E9 vulkanity a tvo\u0159\u00ED n\u011Bkolik napjat\u00FDch kolektor\u016F uvnit\u0159 zaklesl\u00E9 kry. Bahenn\u00ED sopky vznikly pravd\u011Bpodobn\u011B jako v\u00FDsledek Gob-Altajsk\u00E9ho zem\u011Bt\u0159esen\u00ED v roce 1957. Toto zem\u011Bt\u0159esen\u00ED s magnitudem 8,3 vytvo\u0159ilo nov\u00E9 pukliny a otev\u0159elo pukliny star\u00E9. Zem\u011Bt\u0159esn\u00FD impuls p\u0159ekro\u010Dil tixotropii jemnozrnn\u00FDch sedimet\u016F a inicioval vznik bahenn\u00EDch sopek. Sou\u010Dasn\u00E1 rovnov\u00E1ha tlakov\u00FDch podm\u00EDnek na lokalit\u011B je slab\u00E1. Zem\u011Bt\u0159esen\u00ED nebo zv\u00FD\u0161en\u00ED piezometrick\u00E9ho tlaku po velk\u00FDch de\u0161t\u00EDch m\u016F\u017Ee iniciovat aktivitu bahenn\u00EDch sopek. Vysok\u00FD obsah smektit\u016F v sedimentech a ztr\u00E1ta soudr\u017Enosti j\u00EDlov\u00FDch \u010D\u00E1stic p\u0159i rozpo\u0161t\u011Bn\u00ED sol\u00ED podporuj\u00ED \u010Dinnost bahenn\u00EDch sopek."@cs . "CZ - \u010Cesk\u00E1 republika" . "381044" . "11"^^ . . . . "[2201F9D6553A]" . "Mud volcanoes in the Khar Argalantyn Nuruu, NW Gobi Altay, Mongolia as manifestation of recent seismic activity"@en . "Han\u017El, Pavel" . . "Bahenn\u00ED sopky v poho\u0159\u00ED Khar Argalantyn Nuruu, SZ Gobi Altaj, Mongolsko jako projev sou\u010Dasn\u00E9 seismick\u00E9 aktivity"@cs . . "53" . . . . "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" . "RIV/00025798:_____/08:00000217" . "2" . . "Journal of Geosciences" . "mud volcano, liquefaction, thixotropy, earthquake, Gobi Altay, Mongolia"@en . "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 .