magma chamber
岩浆房；岩浆库；岩浆储源
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
成矿物质源于碱性玄武岩浆，基性次火山岩浆多次脉动式入侵是矿床形成的必要条件。
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
中期似斑状钾长花岗岩-二长花岗岩系列岩浆来源于下地壳，是碰撞造山作用的产物；
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿的重要机制。
Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.
因此，当某些岩体的被测矿物有捕虏体成因、岩浆成因、地幔成因等各种来源时，可分别求出某单一事件的年龄。
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
矿床类型以岩浆晚期分异交代型、气成热液型、伟晶岩型、风化壳型和砂矿型为主。
The volcano erupted, spewing hot magma everywhere.
火山爆发，喷射热熔岩到处都是。
Geologists study the composition and behavior of magma.
地质学家研究岩浆的成分和行为。
Magma can solidify to form igneous rocks like granite.
岩浆可以凝固形成花岗岩等火成岩。
The magma chamber beneath the volcano is expanding.
火山下面的岩浆室正在膨胀。
Magma can reach temperatures of over 1,000 degrees Celsius.
岩浆可以达到1000摄氏度以上的温度。
The cooling of magma leads to the formation of crystals.
岩浆冷却导致晶体的形成。
Magma is a mixture of molten rock, gases, and solids.
岩浆是熔融岩石、气体和固体的混合物。
Magma rising to the surface can trigger volcanic eruptions.
岩浆上升到地表可能引发火山爆发。
The movement of magma beneath the Earth's crust causes earthquakes.
地壳下岩浆的运动引起地震。
Minerals dissolved in magma can crystallize as it cools.
随着岩浆冷却，溶解在其中的矿物质会结晶。
magma chamber
岩浆房；岩浆库；岩浆储源
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
成矿物质源于碱性玄武岩浆，基性次火山岩浆多次脉动式入侵是矿床形成的必要条件。
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
中期似斑状钾长花岗岩-二长花岗岩系列岩浆来源于下地壳，是碰撞造山作用的产物；
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了结晶分异模式外,富氟花岗岩浆液态不混溶作用也是伟晶岩成岩成矿的重要机制。
Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.
因此，当某些岩体的被测矿物有捕虏体成因、岩浆成因、地幔成因等各种来源时，可分别求出某单一事件的年龄。
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
矿床类型以岩浆晚期分异交代型、气成热液型、伟晶岩型、风化壳型和砂矿型为主。
The volcano erupted, spewing hot magma everywhere.
火山爆发，喷射热熔岩到处都是。
Geologists study the composition and behavior of magma.
地质学家研究岩浆的成分和行为。
Magma can solidify to form igneous rocks like granite.
岩浆可以凝固形成花岗岩等火成岩。
The magma chamber beneath the volcano is expanding.
火山下面的岩浆室正在膨胀。
Magma can reach temperatures of over 1,000 degrees Celsius.
岩浆可以达到1000摄氏度以上的温度。
The cooling of magma leads to the formation of crystals.
岩浆冷却导致晶体的形成。
Magma is a mixture of molten rock, gases, and solids.
岩浆是熔融岩石、气体和固体的混合物。
Magma rising to the surface can trigger volcanic eruptions.
岩浆上升到地表可能引发火山爆发。
The movement of magma beneath the Earth's crust causes earthquakes.
地壳下岩浆的运动引起地震。
Minerals dissolved in magma can crystallize as it cools.
随着岩浆冷却，溶解在其中的矿物质会结晶。
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