液態巖漿 的英文怎麼說

中文拼音 [yètàiyánjiāng]
液態巖漿 英文
magma liquid
  • 液 : 名詞（液體） liquid; fluid; juice
  • 態 : 名詞1. （形狀; 狀態） form; condition; appearance 2. [物理學] （物質結構的狀態或階段） state 3. [語言學] （一種語法范疇） voice
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 漿 : 漿同「糨」
  • 液態 : [物理學] liquid state液態空氣 liquid air; 液態氣體 liquid gas
  1. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類：正向穹窿型、負向塌陷型、邊隆核陷型：依據巖漿-熱力作用影響的深淺程度或深度分為五類： （古）地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜（熱穹窿） 、中深層侵入型、深部地幔（地殼）熱柱型；提出了熱力構造作用空間分佈的理想模式，將洋陸系統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用（拆沉）等納入一個整體統一的熱力作用系統中，為盆地動力學研究打開了一個新窗口；研討了熱力構造研究方法。
  2. If the next eruption is depleted in oxygen 18, then it is most likely still being fed by stagnant remnants of the original magma, which by now is probably more of a thick crystal mush than an explosive liquid

    如果下一次的噴發較缺乏氧18 ，那麼它最有可能的來源是先前巖漿庫中滯留的殘餘物，此時可能是充滿結晶的糊狀物，而不是噴發的液態。
  3. These fiery conditions had to subside before molten rock could harden into a crust, before continents could form, before the dense, steamy atmosphere could pool as liquid water, and before the earth ' s first primitive life could evolve and survive

    要使熔融的巖漿能夠凝固成地殼、陸地能夠形成、濃密大氣中的蒸氣能夠凝結成液態水、最原始的生命能夠演化與存活，在這之前，都得先讓地球那熾熱如火球般的狀態平息下來才行。
  4. For decades, geologists assumed that magma sits as a pool of liquefied rock for millions of years at a time and that each time some of it pours out onto the earth ' s surface, new liquid rises up from below to refill the chamber immediately

    幾十年來，地質學家都假設，巖漿是一池數百萬年前同時液化的熔巖，每次噴發時湧出一部份到地表上，新的液態物質會隨即從下方上升來補充巖漿庫。
  5. They accumulated so quickly that the heat generated by the process melted the outer portion of the nascent moon and formed a global ocean of liquid rock, or magma

    它們聚積的速度之快，使得過程中產生的熱熔化了初生月球的外部，並產生了全球性的液態巖海，或稱為巖漿。
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