. "\u041B\u0438\u0442\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435, \u0442\u0430\u043A\u0436\u0435 \u0433\u0435\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435 (\u0430\u043D\u0433\u043B. lithostatic pressure, overburden pressure) \u2014 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435 \u0432\u0441\u0435\u0441\u0442\u043E\u0440\u043E\u043D\u043D\u0435\u0435, \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u0435\u043C\u043E\u0435 \u0432\u0435\u0441\u043E\u043C \u0441\u0442\u043E\u043B\u0431\u0430 \u0432\u044B\u0448\u0435\u043B\u0435\u0436\u0430\u0449\u0438\u0445 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434, \u043E\u0431\u0443\u0441\u043B\u043E\u0432\u043B\u0435\u043D\u043D\u043E\u0435 \u0433\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u043D\u043D\u044B\u043C \u043F\u043E\u043B\u0435\u043C \u0417\u0435\u043C\u043B\u0438 \u0438 \u0447\u0438\u0441\u043B\u0435\u043D\u043D\u043E \u0440\u0430\u0432\u043D\u043E\u0435 \u0432\u0435\u0441\u0443 \u0432\u044B\u0448\u0435\u043B\u0435\u0436\u0430\u0449\u0438\u0445 \u043C\u0430\u0441\u0441 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434. \u041E\u0434\u0438\u043D \u0438\u0437 \u043A\u043B\u044E\u0447\u0435\u0432\u044B\u0445 \u0444\u0430\u043A\u0442\u043E\u0440\u043E\u0432 \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0438\u0437\u043C\u0430 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434 \u043D\u0430\u0440\u044F\u0434\u0443 \u0441 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043E\u0439 \u0438 \u0444\u043B\u044E\u0438\u0434\u0430\u043C\u0438. \u0412\u0441\u0435\u0441\u0442\u043E\u0440\u043E\u043D\u043D\u0435\u0435 \u043B\u0438\u0442\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435 \u043D\u0430 \u0433\u043B\u0443\u0431\u0438\u043D\u0435 10 \u043A\u043C \u043C\u043E\u0436\u0435\u0442 \u043F\u0440\u0435\u0432\u044B\u0448\u0430\u0442\u044C 200 \u041C\u041F\u0430, \u0430 \u043D\u0430 \u0433\u043B\u0443\u0431\u0438\u043D\u0435 30 \u043A\u043C \u2014 600\u2014700 \u041C\u041F\u0430. \u0415\u0441\u043B\u0438 \u0433\u0435\u043E\u0442\u0435\u0440\u043C\u0438\u0447\u0435\u0441\u043A\u0438\u0439 \u0433\u0440\u0430\u0434\u0438\u0435\u043D\u0442 \u0434\u043E\u0441\u0442\u0438\u0433\u0430\u0435\u0442 25 \u0433\u0440\u0430\u0434/\u043A\u043C, \u0433\u043E\u0440\u043D\u044B\u0435 \u043F\u043E\u0440\u043E\u0434\u044B \u043C\u043E\u0433\u0443\u0442 \u043D\u0430\u0447\u0430\u0442\u044C \u043F\u043B\u0430\u0432\u043B\u0435\u043D\u0438\u0435 \u043D\u0430 \u0433\u043B\u0443\u0431\u0438\u043D\u0435 \u043E\u043A\u043E\u043B\u043E 20 \u043A\u043C. \u041F\u0440\u0438 \u0432\u044B\u0441\u043E\u043A\u0438\u0445 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F\u0445 \u043F\u043E\u0440\u043E\u0434\u044B \u0441\u0442\u0430\u043D\u043E\u0432\u044F\u0442\u0441\u044F \u043F\u043B\u0430\u0441\u0442\u0438\u0447\u043D\u044B\u043C\u0438. \u041F\u043E\u043C\u0438\u043C\u043E \u043B\u0438\u0442\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0433\u043E, \u0441\u0443\u0449\u0435\u0441\u0442\u0432\u0443\u0435\u0442 \u043E\u0434\u043D\u043E\u0441\u0442\u043E\u0440\u043E\u043D\u043D\u0435\u0435 \u0441\u0442\u0440\u0435\u0441\u0441\u043E\u0432\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435, \u043F\u0440\u043E\u044F\u0432\u043B\u044F\u044E\u0449\u0435\u0435\u0441\u044F \u0432 \u0432\u0435\u0440\u0445\u043D\u0435\u0439 \u0447\u0430\u0441\u0442\u0438 \u0437\u0435\u043C\u043D\u043E\u0439 \u043A\u043E\u0440\u044B \u0441\u043A\u043B\u0430\u0434\u0447\u0430\u0442\u044B\u0445 \u0437\u043E\u043D. \u041E\u043D\u043E \u0432\u044B\u0437\u044B\u0432\u0430\u0435\u0442 \u043C\u0435\u0445\u0430\u043D\u0438\u0447\u0435\u0441\u043A\u0438\u0435 \u0434\u0435\u0444\u043E\u0440\u043C\u0430\u0446\u0438\u0438 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434, \u0438\u0445 \u0434\u0440\u043E\u0431\u043B\u0435\u043D\u0438\u0435, \u0440\u0430\u0441\u0441\u043B\u0430\u043D\u0446\u0435\u0432\u0430\u043D\u0438\u0435, \u0443\u0432\u0435\u043B\u0438\u0447\u0435\u043D\u0438\u0435 \u0440\u0430\u0441\u0442\u0432\u043E\u0440\u0438\u043C\u043E\u0441\u0442\u0438 \u043C\u0438\u043D\u0435\u0440\u0430\u043B\u043E\u0432 \u0432 \u043D\u0430\u043F\u0440\u0430\u0432\u043B\u0435\u043D\u0438\u0438 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u044F. \u0412 \u0432\u043E\u0437\u043D\u0438\u043A\u0430\u044E\u0449\u0438\u0435 \u043F\u0440\u0438 \u044D\u0442\u043E\u043C \u0442\u0440\u0435\u0449\u0438\u043D\u044B \u043F\u0440\u043E\u043D\u0438\u043A\u0430\u044E\u0442 \u0444\u043B\u044E\u0438\u0434\u044B, \u0432\u044B\u0437\u044B\u0432\u0430\u044E\u0449\u0438\u0435 \u043F\u0435\u0440\u0435\u043A\u0440\u0438\u0441\u0442\u0430\u043B\u043B\u0438\u0437\u0430\u0446\u0438\u044E \u043F\u043E\u0440\u043E\u0434."@ru . . . "Press\u00E3o litost\u00E1tica (em grego: \u03BB\u03AF\u03B8\u03BF\u03C2 lithos [m.]; \"rocha\", \"rochoso\"), por vezes designada por press\u00E3o de confinamento, \u00E9 a press\u00E3o exercida pelo peso da coluna de rocha sobre os materiais geol\u00F3gicos subjacentes. Este conceito apresenta paralelismo com o o conceito equivalente de press\u00E3o hidrost\u00E1tica em hidrodin\u00E2mica."@pt . . . "Pressure is force magnitude applied over an area. Overburden pressure is a geology term that denotes the pressure caused by the weight of the overlying layers of material at a specific depth under the earth's surface. Overburden pressure is also called lithostatic pressure, or vertical stress. In a stratigraphic layer that is in hydrostatic equilibrium; the overburden pressure at a depth z, assuming the magnitude of the gravity acceleration is approximately constant, is given by: Where: \n* is the depth in meters. \n* is the overburden pressure at depth . \n* is the pressure at the surface. \n* is the density of the material above the depth . \n* is the gravity acceleration in . In deep-earth geophysics/geodynamics, gravitational acceleration varies significantly over depth and should not be assumed to be constant, and should be inside the integral. Some sections of stratigraphic layers can be sealed or isolated. These changes create areas where there is not static equilibrium. A location in the layer is said to be in under pressure when the local pressure is less than the hydrostatic pressure, and in overpressure when the local pressure is greater than the hydrostatic pressure."@en . . . . "Als lithostatischer Druck rsp. (von alt-/neugriechisch: \u03BB\u03AF\u03B8\u03BF\u03C2 lithos [m.] \u2013 \u201AStein\u2018, \u201AGestein\u2018) wird in Geophysik, Geologie und Geotechnik jener Druck in der Lithosph\u00E4re (Erdkruste und Teil des Erdmantels) bezeichnet, den die dar\u00FCber liegenden Gesteinsschichten durch ihr Gewicht aus\u00FCben. Dieser spezifische Druck bildet ein isotropes Spannungsfeld."@de . . . . . . "Lithostatischer Druck"@de . . . . "I corpi rocciosi all'interno della Terra sono sottoposti ad una pressione, chiamata pressione litostatica o pressione di carico, dovuta al peso delle rocce sovrastanti. Abitualmente questa pressione \u00E8 indicata come o o nella terna degli assi dell'ellissoide delle tensioni. Ad ogni profondit\u00E0, nel sottosuolo si pu\u00F2 individuare un punto sottoposto a tensioni, scomponendo queste tensioni lungo una terna di assi tra loro perpendicolari si costruisce l'ellissoide delle tensioni, i cui assi rispettivamente coincidono con le direzione di massima tensione, di minima tensione e di tensione intermedia; in aree tettonicamente stabili, o in regime di tettonica distensiva, l'asse maggiore di questo ellissoide \u00E8 orientato verticalmente e corrisponde come direzione e valore alla pressione litostatica."@it . . "De lithostatische druk is de druk die op een bepaald punt in de ondergrond heerst als gevolg van het gewicht van erboven gelegen gesteentemateriaal. De lithostatische druk zorgt voor een mechanische spanning in gesteenten. Terwijl de hydrostatische druk bij toenemende diepte elke 100 meter 1 MPa toeneemt, bedraagt de toename van de lithostatische druk grofweg het drievoudige. De precieze toename hangt af van de dichtheid van het gesteente, die in de aardkorst tussen 2,0-3,3*10\u00B3 kg/m\u00B3 ligt (sedimenten ongeveer 2,0 *10\u00B3 kg/m\u00B3, graniet en kalksteen 2,7*10\u00B3 kg/m\u00B3 en gabbro 3,3*10\u00B3 kg/m\u00B3)."@nl . . . "\u76D6\u5C42\u538B\u529B"@zh . "Pressione litostatica"@it . . "Press\u00E3o litost\u00E1tica (em grego: \u03BB\u03AF\u03B8\u03BF\u03C2 lithos [m.]; \"rocha\", \"rochoso\"), por vezes designada por press\u00E3o de confinamento, \u00E9 a press\u00E3o exercida pelo peso da coluna de rocha sobre os materiais geol\u00F3gicos subjacentes. Este conceito apresenta paralelismo com o o conceito equivalente de press\u00E3o hidrost\u00E1tica em hidrodin\u00E2mica."@pt . . . . "De lithostatische druk is de druk die op een bepaald punt in de ondergrond heerst als gevolg van het gewicht van erboven gelegen gesteentemateriaal. De lithostatische druk zorgt voor een mechanische spanning in gesteenten. Terwijl de hydrostatische druk bij toenemende diepte elke 100 meter 1 MPa toeneemt, bedraagt de toename van de lithostatische druk grofweg het drievoudige. De precieze toename hangt af van de dichtheid van het gesteente, die in de aardkorst tussen 2,0-3,3*10\u00B3 kg/m\u00B3 ligt (sedimenten ongeveer 2,0 *10\u00B3 kg/m\u00B3, graniet en kalksteen 2,7*10\u00B3 kg/m\u00B3 en gabbro 3,3*10\u00B3 kg/m\u00B3). In de bovenmantel zijn gesteenten echter veel compacter (duniet is bijvoorbeeld 3,3 tot 4,0*10\u00B3 kg/m\u00B3, onder zeer hoge druk kan dat oplopen tot 5,0*10\u00B3 kg/m\u00B3). De berekening van de lithostatische druk is vanwege de variatie in dichtheid soms erg complex. Men kan als vuistregel echter stellen dat in de aardkorst de druk elke kilometer met 30 MPa toeneemt. In de aardmantel neemt de lithostatische druk ongeveer 35 MPa per kilometer diepte toe."@nl . . "Pressure is force magnitude applied over an area. Overburden pressure is a geology term that denotes the pressure caused by the weight of the overlying layers of material at a specific depth under the earth's surface. Overburden pressure is also called lithostatic pressure, or vertical stress. In a stratigraphic layer that is in hydrostatic equilibrium; the overburden pressure at a depth z, assuming the magnitude of the gravity acceleration is approximately constant, is given by: Where:"@en . . "\u041B\u0438\u0442\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435"@ru . . . "Als lithostatischer Druck rsp. (von alt-/neugriechisch: \u03BB\u03AF\u03B8\u03BF\u03C2 lithos [m.] \u2013 \u201AStein\u2018, \u201AGestein\u2018) wird in Geophysik, Geologie und Geotechnik jener Druck in der Lithosph\u00E4re (Erdkruste und Teil des Erdmantels) bezeichnet, den die dar\u00FCber liegenden Gesteinsschichten durch ihr Gewicht aus\u00FCben. Dieser spezifische Druck bildet ein isotropes Spannungsfeld."@de . "Press\u00E3o litost\u00E1tica"@pt . . "Lithostatische druk"@nl . "146153"^^ . "Overburden pressure"@en . "2418"^^ . . "1120056454"^^ . . . "\u041B\u0438\u0442\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435, \u0442\u0430\u043A\u0436\u0435 \u0433\u0435\u043E\u0441\u0442\u0430\u0442\u0438\u0447\u0435\u0441\u043A\u043E\u0435 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435 (\u0430\u043D\u0433\u043B. lithostatic pressure, overburden pressure) \u2014 \u0434\u0430\u0432\u043B\u0435\u043D\u0438\u0435 \u0432\u0441\u0435\u0441\u0442\u043E\u0440\u043E\u043D\u043D\u0435\u0435, \u043E\u043F\u0440\u0435\u0434\u0435\u043B\u044F\u0435\u043C\u043E\u0435 \u0432\u0435\u0441\u043E\u043C \u0441\u0442\u043E\u043B\u0431\u0430 \u0432\u044B\u0448\u0435\u043B\u0435\u0436\u0430\u0449\u0438\u0445 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434, \u043E\u0431\u0443\u0441\u043B\u043E\u0432\u043B\u0435\u043D\u043D\u043E\u0435 \u0433\u0440\u0430\u0432\u0438\u0442\u0430\u0446\u0438\u043E\u043D\u043D\u044B\u043C \u043F\u043E\u043B\u0435\u043C \u0417\u0435\u043C\u043B\u0438 \u0438 \u0447\u0438\u0441\u043B\u0435\u043D\u043D\u043E \u0440\u0430\u0432\u043D\u043E\u0435 \u0432\u0435\u0441\u0443 \u0432\u044B\u0448\u0435\u043B\u0435\u0436\u0430\u0449\u0438\u0445 \u043C\u0430\u0441\u0441 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434. \u041E\u0434\u0438\u043D \u0438\u0437 \u043A\u043B\u044E\u0447\u0435\u0432\u044B\u0445 \u0444\u0430\u043A\u0442\u043E\u0440\u043E\u0432 \u043C\u0435\u0442\u0430\u043C\u043E\u0440\u0444\u0438\u0437\u043C\u0430 \u0433\u043E\u0440\u043D\u044B\u0445 \u043F\u043E\u0440\u043E\u0434 \u043D\u0430\u0440\u044F\u0434\u0443 \u0441 \u0442\u0435\u043C\u043F\u0435\u0440\u0430\u0442\u0443\u0440\u043E\u0439 \u0438 \u0444\u043B\u044E\u0438\u0434\u0430\u043C\u0438."@ru . . "I corpi rocciosi all'interno della Terra sono sottoposti ad una pressione, chiamata pressione litostatica o pressione di carico, dovuta al peso delle rocce sovrastanti. Abitualmente questa pressione \u00E8 indicata come o o nella terna degli assi dell'ellissoide delle tensioni. Ad ogni profondit\u00E0, nel sottosuolo si pu\u00F2 individuare un punto sottoposto a tensioni, scomponendo queste tensioni lungo una terna di assi tra loro perpendicolari si costruisce l'ellissoide delle tensioni, i cui assi rispettivamente coincidono con le direzione di massima tensione, di minima tensione e di tensione intermedia; in aree tettonicamente stabili, o in regime di tettonica distensiva, l'asse maggiore di questo ellissoide \u00E8 orientato verticalmente e corrisponde come direzione e valore alla pressione litostatica."@it .