magma chamber
岩漿房；岩漿庫；岩漿儲源
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
成礦物質源於鹼性玄武岩漿，基性次火山岩漿多次脈動式入侵是礦牀形成的必要條件。
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
中期似斑狀鉀長花崗岩-二長花崗岩系列岩漿來源於下地殼，是碰撞造山作用的產物；
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了結晶分異模式外,富氟花崗岩漿液態不混溶作用也是偉晶岩成巖成礦的重要機制。
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，當某些巖體的被測礦物有捕虜體成因、岩漿成因、地幔成因等各種來源時，可分別求出某單一事件的年齡。
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
礦牀類型以岩漿晚期分異交代型、氣成熱液型、偉晶岩型、風化殼型和砂礦型爲主。
The volcano erupted, spewing hot magma everywhere.
火山爆發，噴射熱熔岩到處都是。
Geologists study the composition and behavior of magma.
地質學家研究岩漿的成分和行爲。
Magma can solidify to form igneous rocks like granite.
岩漿可以凝固形成花崗岩等火成岩。
The magma chamber beneath the volcano is expanding.
火山下面的岩漿室正在膨脹。
Magma can reach temperatures of over 1,000 degrees Celsius.
岩漿可以達到1000攝氏度以上的溫度。
The cooling of magma leads to the formation of crystals.
岩漿冷卻導致晶體的形成。
Magma is a mixture of molten rock, gases, and solids.
岩漿是熔融岩石、氣體和固體的混合物。
Magma rising to the surface can trigger volcanic eruptions.
岩漿上升到地表可能引發火山爆發。
The movement of magma beneath the Earth's crust causes earthquakes.
地殼下岩漿的運動引起地震。
Minerals dissolved in magma can crystallize as it cools.
隨着岩漿冷卻，溶解在其中的礦物質會結晶。
magma chamber
岩漿房；岩漿庫；岩漿儲源
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
成礦物質源於鹼性玄武岩漿，基性次火山岩漿多次脈動式入侵是礦牀形成的必要條件。
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
中期似斑狀鉀長花崗岩-二長花崗岩系列岩漿來源於下地殼，是碰撞造山作用的產物；
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
除了結晶分異模式外,富氟花崗岩漿液態不混溶作用也是偉晶岩成巖成礦的重要機制。
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，當某些巖體的被測礦物有捕虜體成因、岩漿成因、地幔成因等各種來源時，可分別求出某單一事件的年齡。
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
礦牀類型以岩漿晚期分異交代型、氣成熱液型、偉晶岩型、風化殼型和砂礦型爲主。
The volcano erupted, spewing hot magma everywhere.
火山爆發，噴射熱熔岩到處都是。
Geologists study the composition and behavior of magma.
地質學家研究岩漿的成分和行爲。
Magma can solidify to form igneous rocks like granite.
岩漿可以凝固形成花崗岩等火成岩。
The magma chamber beneath the volcano is expanding.
火山下面的岩漿室正在膨脹。
Magma can reach temperatures of over 1,000 degrees Celsius.
岩漿可以達到1000攝氏度以上的溫度。
The cooling of magma leads to the formation of crystals.
岩漿冷卻導致晶體的形成。
Magma is a mixture of molten rock, gases, and solids.
岩漿是熔融岩石、氣體和固體的混合物。
Magma rising to the surface can trigger volcanic eruptions.
岩漿上升到地表可能引發火山爆發。
The movement of magma beneath the Earth's crust causes earthquakes.
地殼下岩漿的運動引起地震。
Minerals dissolved in magma can crystallize as it cools.
隨着岩漿冷卻，溶解在其中的礦物質會結晶。
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