「magma」の共起表現一覧(1語右で並び替え)
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| g indicates that it solidified from a volcanic | magma about 4.1 billion years ago. |
| Restite acts as a form of buffer within | magma, acting as a reservoir primarily of water and |
| the facility as part of a gambit to expose the | Magma agent, avoiding the same security that had thr |
| Magma am Himmel (1975) | |
| Such heroes include Osamu Tezuka's Ambassador | Magma and Eiji Tsuburaya's Ultraman and other heroes |
| Over time, enormous upward pressures of | magma and widespread geologic upheaval, which create |
| re more likely generated by the interaction of | magma and water or phreatomagmatic eruptions. |
| deposit of volcanic material (both solidified | magma, and ejecta) which appears mostly flat from th |
| nd may be useful in studying the generation of | magma and the composition of the mantle since the si |
| During the fractional crystallization of | magma, and magma generation by the partial melting o |
| sts infer that they were being resorbed by the | magma and may imply addition of fresh, hotter magma. |
| ashik's troops were caught in a pool of molten | magma and destroyed. |
| canic regions where unusually large volumes of | magma are erupted. |
| ls, the first ones to crystallize in a mass of | magma, are most unstable at the Earth's surface and |
| Magma Arizona Railroad - dieselisation began and com | |
| ragment of country rock that fell into passing | magma as a result of stoping. |
| have been progressively concentrated into the | magma as crystallization progressed, forming a "KREE |
| buffer, providing elements to the surrounding | magma as it is melted and ground up by erosive force |
| If the restite minerals are carried with the | magma, as the minerals become thermo-barometrically |
| "channel zone" where evidences of large scale | magma ascent can be observed, and a zone of superfic |
| It is considered that source of the heat is | magma associated with the Ata Caldera. |
| The soils of the region are | magma based with high levels of acidity. |
| He pilots the | Magma Beasts against Combattler V and the Nanbara Co |
| As the main | magma body cools, water originally present in low co |
| nd (as opposed to the violent fragmentation of | magma by explosive eruptions). |
| late moved westward over a center of upwelling | magma called the New England hotspot, also referred |
| The main effect of extrusion is that the | magma can cool much more quickly in the open air or |
| Trachyandesitic | magma can produce explosive Plinian eruptions, such |
| c activity and may have formed when retreating | magma caused an unsupported area of the surface to c |
| The friction and viscosity of the | magma causes phenocrysts and xenoliths within the ma |
| ssom Toes, B. B. Blunder, Solid Gold Cadillac, | Magma, Centipede, Mike Westbrook Orchestra and Full |
| a feature may have resulted from collapse of a | magma chamber underlying the central part of the cra |
| a feature may have resulted from collapse of a | magma chamber underlying the central peak ring compl |
| ssibly formed as the result of collapse of the | magma chamber during eruptions of the volcano. |
| omplex were formed as a result of emptying the | magma chamber beneath a volcano. |
| The field's | magma chamber also powers a geothermal field called |
| sing of a caldera floor due to movement in the | magma chamber beneath it. |
| help the eruption along, water seeped into the | magma chamber and created vast amounts of super-pres |
| and the Muskox is interpreted as occupying the | magma chamber which fed the volcanism. |
| Iceland Lake Pluton might be the remnants of a | magma chamber of a volcano that erupted felsic magma |
| ds generally occur where there is a high-level | magma chamber. |
| ndeed most of the lava layer and laid bare the | magma chambers and volcanic pipes deep below, allowi |
| ogical discontinuities due to major changes in | magma chemistry, volcanotectonic events, or long ero |
| column of overlying material directly over the | magma column, and does not form a large above-ground |
| gs, that grow large enough to rise through the | magma column, bursting near the top due to the decre |
| below 100 °C (212 °F) and can be produced when | magma comes into contact with a large volume of wate |
| losions caused by rising basaltic or andesitic | magma coming into contact with abundant, shallow gro |
| By finding the primitive | magma composition of a magma series it is possible t |
| In order to produce a | magma composition suitable for forming essexite the |
| The | Magma computer algebra system is produced and distri |
| may include rocks plucked off the wall of the | magma conduit, or physically picked up by the ensuin |
| water, 5 layers of lava and ash, 6 stratum, 7 | magma conduit, 8 magma chamber, 9 dike |
| The eruptions melted the ice, so the hot | magma contacted with water and caused violent explos |
| The large impact crater filled with | magma containing nickel, copper, platinum, palladium |
| If the | magma contains abundant volatile components which ar |
| This | magma cooled into the diabase dykes seen in the clif |
| Pegmatitic texture occurs during | magma cooling when some minerals may grow so large t |
| ich then collapses in the centre as the molten | magma cools and leaks out at the sides, leaving a cr |
| When the | magma cools it crystallises and forms rocks, the typ |
| assy volcanic rock formed when viscous lava or | magma cools swiftly. |
| As a | magma cools slowly the minerals have time to grow an |
| have provided a zone of crustal weakness where | magma could rise from great depths through the crust |
| a harmonic tremor, which is steady movement of | magma, deep in the mantle. |
| nes during the early phase of an eruption as a | magma degasses, and then to have lava push through t |
| Magma Design Automation | |
| Quartz Formal by | Magma Design Automation |
| In one such EDA company, | Magma Design Automation, his stake was valued around |
| opposed to intrusive rock formation, in which | magma does not reach the surface. |
| amounts, retard the compositional changes of a | magma either via providing more reagents or physical |
| or she have actually been working for a former | Magma employee, who wanted the papers in revenge for |
| In the year 2030, the | M.A.G.M.A. Energy Corporation sends its mercenaries to |
| In 2010, | Magma Energy acquired 98.5% of shares in the Iceland |
| Magma Energy Corp. is a geothermal power company bas | |
| Dissolved gases escape easily as the | magma erupts, forming lava that flows downhill quite |
| While cooling, the | magma evolves in composition because different miner |
| It had high-sulfur anhydrite-bearing | magma, explosive eruptions, pyroclastic flows, and s |
| magmatic province (CAMP) is a large connected | magma flow formed during the breakup of Pangaea duri |
| in size or disappear by later remelting during | magma flow, depending on magma heat flux. |
| Utilizing energy produced by the | magma flowing under the volcano, this new monstrosit |
| huge arms into the ground, control underground | magma flows causing geysers of magma and huge earthq |
| The | magma forming these volcanoes was not hot enough to |
| Magma from the planet's mantle rises through the pla | |
| nt of large volumes of relatively hot basaltic | magma from a mantle source. |
| f igneous volcanic rock formation in which hot | magma from inside the Earth flows out (extrudes) ont |
| this rock, as opposed to the extraction of its | magma from the mantle, is likely closer to 3.8 billi |
| Eruption of such a large quantity of | magma from underneath the Mount Katmai area resulted |
| ng formed at the ocean ridges by extrusions of | magma from the Earth's mantle, and that convection c |
| found as a trace mineral owing to the unusual | magma genesis of these rocks. |
| r a time managing French progressive rock band | Magma, Gomelsky headed for New York City in the mid- |
| French bass player, best known for his work in | Magma, Gong and Pierre Moerlen's Gong. |
| MAGMA has been developed in Armin Madadkar Sobhani R | |
| pressure changes in the rock around where the | magma has experienced stress. |
| Besides his work with | Magma, he has also performed solo, with the Christia |
| His left hand is composed of Motorarm's | Magma Horns, which melt whatever they touch. |
| melting of limestone or marble by intrusion of | magma, however geochemical and mineralogical data di |
| Gentle Giant, Wishbone Ash, Soft Machine, and | Magma in their brief career, they have always remain |
| use the word lava in connection with extruded | magma in a short account of the eruption of Mount Ve |
| Magma includes permutation, matrix, finitely-present | |
| The hotspot is explosive because basaltic | magma interacts with groundwater in aquifers below t |
| hem as the product of the intrusion of igneous | magma into metamorphic rocks at depth. |
| alapai Hill is the product of the intrusion of | magma, into White Tank monzogranite, that cooled as |
| During the Variscan orogeny, | magma intruded along structural zones, but cooled an |
| Basaltic | magma intruding near the surface flashed ground wate |
| beneath the Earth's surface during a period of | magma intrusion about 73 to 78 million years ago (La |
| The | magma intrusions forming the White Mountains today w |
| is time, melting occurred, creating subsurface | magma intrusions. |
| Magma is produced and distributed by the Computation | |
| The | magma is likely a mix from three different sources, |
| ptions, pumice and ash are formed when silicic | magma is fragmented in the volcanic conduit, because |
| The Museum of Avant-Garde Mastery ( | MAGMA) is a continually renewed collection of hundre |
| Magma is a French progressive rock band founded in P | |
| The volatile portion of the | magma is gradually excluded from the forming crystal |
| Magma, Knaur publishing house 2007, ISBN 978-3-426-6 | |
| avier, would have settled to the bottom of the | magma lake, forming a metallic layer buried by a rel |
| The high water content of the | magma made it possible for the crystals to grow quic |
| Contact between the water of the aquifer and | magma may have caused the explosive phreatic eruptio |
| rock/fusion band, formed in 1976 around former | Magma members, bassist Bernhard Paganotti and keyboa |
| reduced pressure and thus potential sites for | magma migration and emplacement. |
| High-temperature | magma, most of which is basaltic in composition, beh |
| plift and deformation of the surface itself by | magma movement underground. |
| the Catoctin Formation, deposition of basaltic | magma occurred during the formation of the Iapetus O |
| As crystallization of this | magma ocean proceeded, minerals such as olivine and |
| e initially been molten, forming a near-global | magma ocean. |
| have supplied the energy needed to form such a | magma ocean. |
| iver Hot Springs Provincial Park are heated by | magma of the Northern Cordilleran Volcanic Province. |
| hat form igneous rocks (rocks that cooled from | magma or lava). |
| r fine grained zone along the margin where the | magma or lava has contacted air, water, or particula |
| Silicic is a term used to describe | magma or igneous rock rich in silica. |
| models of the GTI were distinguished by their | Magma Orange paint job, special Fahrenheit badging, |
| lso runs her own booking and management agency | Magma, organises events and on top of that she has h |
| thermal activity builds up and is released in | magma plume spewing through the Earth's crust, formi |
| Several of the old | magma plumes are now quarried, the rich black Larvik |
| MAGMA President is Viatcheslav Moshe Kantor. | |
| r Fort Rock and Hole-in-the-Ground, but rising | magma probably encountered permeable aquifers beneat |
| Viscous (thick) | magma produces volcanoes characterised by explosive |
| At the bottom of the | magma reservoir, a cumulate rock forms. |
| As the body of | magma rises toward the surface, the volatile compoun |
| ed by seismic activity is certain evidence for | magma rising beneath the surface. |
| dystone Rock was part of a volcanic vent where | magma rose repeatedly to the surface of the earth. |
| nds the temperature range downwards before the | magma sets solid completely, allowing concentration |
| mplaced during several episodes from a crustal | magma source. |
| Initial values of 87Sr, when the | magma stated fractional crystallization, might be es |
| Carbon dioxide gas from | magma still bubbles up at the southeastern shore, an |
| Intermediate composition | magma such as andesite tends to form cinder cones of |
| Monogenetic fields occur only where the | magma supply to the volcano is low or where vents ar |
| The predecessor of the | Magma system was called Cayley (1982-1993). |
| o known to occur and are probably derived from | magma that was over-saturated with silica. |
| Magma that reaches the surface to become lava cools | |
| r temperature and pressure calculations of the | magma that produced igneous rock containing this min |
| Magma that remains trapped in large quantities below | |
| eep as most other volcanoes, and the resulting | magma that is pushed toward the surface is high in m |
| onstituents, including glass (which represents | magma that has been quenched by rapid cooling), smal |
| Magma that remains trapped below ground in thin intr | |
| The remnant | magma thus becomes richer in water, and also in rare |
| st the existence of three chemically different | magma types within the Bravo Lake Formation. |
| The two | magma types then form separate magma chambers giving |
| In the root zone, mantle-derived | magma underwent fractional crystallisation which was |
| alia hotspot is a volcanic hotspot that forces | magma up at weak spots in the Indo-Australian Plate |
| This sudden expansion propels the | magma upward at rapid speeds, resulting in a shallow |
| Physical nature of | magma: viscous; basaltic. |
| Here, the large | magma volumes which are created by mid-ocean ridge s |
| te 2006, the book Discovering Mathematics with | Magma was published by Springer as volume 19 of the |
| ric suite of faults providing space into which | magma was able to intrude. |
| An estimated 6 km³ of | magma was erupted, producing around 16 km³ of tephra |
| If | magma were to rise towards the surface of Nazko, new |
| Cross of King Crimson, and Didier Lockwood of | Magma were also members at various times. |
| s crust produces relatively low-density molten | magma which can rise upwards towards the surface. |
| body represents essentially a single pulse of | magma, which crystallized from the bottom upward and |
| The mantle is not quite solid and consists of | magma which is in a state of semi-perpetual convecti |
| w banding is caused by friction of the viscous | magma which is in contact with a solid rock interfac |
| es, which are from sudden sporadic movement of | magma, which is blocked from moving due to a blockag |
| the northeast flank of the mountain, exposing | magma which hardened in the volcano's conduits to fo |
| rizontal plane of weakness which the ascending | magma will exploit, forming a sill or lopolith. |
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