火山地貌 的英文怎麼說
中文拼音 [huǒshāndemào]
火山地貌
英文
volcanic landform-
There is a north - north - east negative anomaly belt of aerial magnetism in the middle - east part of the basin, which could be displayed by the aerial magnetism of commutative field, upwardly continuation, lvt in earthquakes, the experimentation of granite liquation ( demagnetization ), the distribution of neozoic era volcanic rock, earthquake, hot spring and ground feature. the anomaly shows the blocking in east - west direction, and it is also associated with intense activity of deep heat interaction and the development of the crust - mantle mixed layer in the north qiangtang
從區域航磁、向上延拓、地震低速層、花崗巖熔融（退磁）實驗、新生代火山巖的分佈、地震、溫泉、地貌等發現，盆地中東部存在一北北東向航磁負異常帶，既顯示出東西分塊，也與北羌塘深部熱力作用強烈活動、發育「殼幔混合層」有聯系。Thc island has so pcculiar and various gcologic landforms, cxccllcnt locality, comfortablc climale, clash air, charming sunshine and sand bank, sequestered environmenl, various modem coralline, abundant sea resources and beautiful lisland sceneries that it ' s not onlyan ideal place for sightseeing, traveling and leisure vocation, but alsoa science researching, educating and surveying base for lots of subjecls such as volcanic geology, geomorpny, marine biology and environmental eclogy
島上獨特多樣的地質、地貌景觀，優越的地理位置，宜人的氣候，清新的空氣，迷人的陽光、沙灘，幽靜的環境，種類繁多的現代珊瑚及豐富的海洋資源，美麗的海島風光，不僅是觀光、旅遊、休閑渡假的理想場所，也是火山地質學、地貌學、海洋生物學、環境生態學等多種學科的科研、教學、考察基地。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。Virunga national park ( covering an area of 790, 000 ha ) comprises an outstanding diversity of habitats, ranging from swamps and steppes to the snowfields of rwenzori at an altitude of over 5, 000 m, and from lava plains to the savannahs on the slopes of volcanoes
維龍加國家公園佔地79萬公頃，地貌多種多樣，包括從沼澤地、稀樹乾草原到海拔5000米以上的魯文佐里雪山，從融巖平原到火山山坡處的大草原，不一而足。In 1976, viking orbiter 1 photographed a region of buttes and mesas with a face - like hill,
1976年，維京一號太空船在拍攝火星地形時，攝得一個貌似人面的山，Perhaps you have seen colorful limestone cave and underground river, but the eighteen caves here are mesozoic lava land forms, which is produced by the movement, cracking and weathering of the earth ' s crust
或許你見過絢麗多彩的石灰熔洞和地下暗河，但在這里的十八個山洞卻是中生代火山巖地貌，由於地殼運動斷裂風化形成的。A special feature of the north island is the central volcanic region with three still active volcanic peeks and internal activity featuring hot springs, geysers, and boiling mud pools
北島富有特色的地形風貌莫過于有著三座活火山的中部火山區，以及以熱泉、間歇泉和沸騰的泥漿為特徵的地熱活動。Unlike the earth, the large number of volcanic features on mars is due to the
火星上仍能留下大量與火山活動有關的地貌，是由於Io is famous for its active volcanic activity, which emits sulphuric compounds, and has a geologically young surface
艾奧最著名的莫過於它的火山活動，噴出大量硫化物，並形成非常年青的地貌。分享友人