新噴發巖 的英文怎麼說
中文拼音 [xīnpēnfāyán]
新噴發巖
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。Preliminary study on late pleistocene phreato - magmatic eruptions in northern hainan island
瓊北地區晚更新世射氣巖漿噴發初步研究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。If a new round of small, precursor eruptions begins in yellowstone ? and they usually do so weeks to hundreds of years before a catastrophic explosion ? testing the oxygen fingerprint of those lavas and the ages of their zircons should reveal what type of magma is abundant in the chamber below
如果黃石國家公園開始產生新一波前兆性質的小型噴發（通常是在災難性爆發的前幾周甚至數百年前） ，這時測試熔巖中含氧的特徵以及鋯石的年齡，應該就可以了解下方巖漿庫富含何種型態的巖漿。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。A look at the composition of tiny crystals trapped inside erupted lava and ash at yellowstone has suggested a partial answer, by providing new insight into how magma forms
藉由研究黃石國家公園噴發熔巖與火山灰內的微小晶體，這個疑問獲得了部份解答，也使我們對于巖漿的形成機制有了新的見解。分享友人