新噴出巖 的英文怎麼說
中文拼音 [xīnpēnchūyán]
新噴出巖
英文
kainolite-
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。The scientists who discovered the “ hot spot ” say that the crust beneath the new ice stream is very thin, and suggest that hot magma from the earth ' s mantle came close enough to the surface to cause the ice stream to form
科學家們發現"熱點" ，指出，地殼下面的新冰流非常薄，並指出，從地球的地幔噴出的熱巖漿險些夠到地表造成冰流形成。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。And these pictures, taken from a helicopter, show the latest lava flow. such sights are uncommon as many eruptions simply see ash and rock blasted into the sky
這是從直升飛機上拍到的斯特龍博利火山流出的最新熔巖照片。這種景觀對於斯特龍博利火山來說不是常見的。以前斯特龍博利火山爆發時只是出現火山灰和巖石噴上天空的景象。分享友人