火山噴發巖 的英文怎麼說

中文拼音 [huǒshānpēnfāyán]
火山噴發巖 英文
volcanic
  • 火 : fire
  • 山 : 名詞1 （地面形成的高聳的部分） hill; mountain 2 （形狀像山的東西） anything resembling a mountain...
  • 噴 : 噴動詞1. （液體等受壓力而射出） spurt; spout; gush; jet 2. （噴灑） spray; sprinkle
  • 發 : 名詞（頭發） hair
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 火山 : [地質學] volcano; burning mountain
  1. The eruptions were associated with the development of several giant craters ( calderas )

    大量熔巖和火山灰噴出，火山爆發形成多個破火山口。
  2. The team collected 65 - million - year - old droppings from the volcanic deccan traps of central india in order to study the diet of titanosaurs, the group of super - size dinosaurs that includes diplodocus

    他們這支隊伍從印度中部火山噴發形成的德干巖群中收集了長達6500萬年的糞便，用以研究雷龍? ?與梁龍同屬超級大恐龍? ?的飲食結構。
  3. In this time the strike - slipping mylonite, ultramylonite as well as associated igneous and magmatic intrusion and eruptive activity of volcano were formed along the fault

    該時期斷裂帶內以走滑糜棱巖、超糜棱巖為主要形式；沿斷裂出現串珠狀巖漿巖體和火山噴發。
  4. 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。
  5. Based on the petrological, petrochemical and geochemical analyses about these rocks, it is concluded in this paper that the xenoliths were originated from the upper mantle, and comprised of both primitive pyrolite and the infusible solid residual of the upper pyrolite while the basaltic magma was melted out of it, which were brought up to the earth ' s surface via o1carnc eruption

    根據其巖石學、巖石化學及地球化學特徵分析，包體來源於上地幔，其成因既有原始地幔巖，亦有上地幔巖經部分熔融出玄武巖漿后的難熔固相殘留物，被火山噴發攜帶至地表。
  6. " our neighbourhood was destroyed by the lava, " said mungo, 37. " my house was burnt, i do n ' t know where we ' re going to go.

    蒙戈說： "我們家附近都已經被火山噴發的熔巖夷為平地了，我們家的房子也被燒毀了，我現在不知道該往哪裡去。
  7. A great number of lherzolite xenoliths occurs within the volcanic clastics characterized by terrigenous central type eruption at tianyang, jiudouyang and yingfenglin of qingtongyang, of southern leizhou peninsula

    摘要雷州半島南部田洋、九斗洋及青桐洋的英峰嶺等陸相中心式噴發的火山碎屑巖中，分佈有大量的二輝橄欖巖包體。
  8. Multi - stage regional faulting activities and volcanic eruption with multi - times of forcing generate favorable conditions for the fracture development of the volcanic rock in the eastern depression

    多期區域性斷裂活動及火山噴發，多期施力，是東部凹陷火山巖中裂縫發育的有利條件。
  9. According to the study of the mineral evolving, origin analysis etc., it is considered that the source of minerals etc mainly comes from the pyritization sources of the submarine volcano eruption

    認為含礦巖系的物源主要來自海底火山噴發作用形成的黃鐵礦化礦源層。
  10. I ' ve seen the stream of lava from a volcano

    我見過火山噴發出的熔巖流。
  11. The comparison study of the three belts indicates although they are distinct from each other all the three belts show many common features in the aspect of the metallogeny of large - rich vein uranium deposits, i. e : the important metallogenic areas are located above the old crystalline basement ; the paleo - rifting ( taphrogeny ) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment ; the occurrence of uranium deposit does not depend on the lithology of volcanic rocks ; uranium metallogeny is obviously constrained by deep geologic processes and the connected fault - structural net is the necessary condition for the formation of large - rich uranium deposits

    對比研究表明，雖然它們各具特色，就脈型富大鈾礦床成礦作用而言，它們又具有較多的共性：重要成礦區的火山噴發皆奠基在古老的結晶基底上；古裂谷（或裂陷）既控制了火山巖帶的發育，又是有利的成礦構造背景；鈾礦賦存對火山巖的巖性沒有明顯的選擇性；鈾成礦的深部控製作用明顯；聯通的構造網路系統是形成富大鈾礦的必要條件。
  12. Because the volcanics and sedimentary rocks alternated with one and another, the volcanic activity of these two periods had the characteristics of many a time, multipoint of erupting

    火山巖與正常沉積巖相間分佈，且火山角礫巖發育，因此這兩個時期火山活動都具有多期次、多點噴發的特點。
  13. After the volcanic eruption of multi - phrase cycle - deformation, filling of basin, crustal uplifting event being studied, this dissertation tries constructing the different degree rhythm of magma activity corresponding with crust - mantle dynamic system, studying the crust - mantle deep processes. based on the studies on the characteristics of volcanic rhythm, igneous rocks assemblages, temporal and spatial distribution of igneous rocks, tectonic deformation, the author has util ized the methods of petrology, geochemistry, isotopic geology et al. to do research on the above - mentioned geological problems

    通過多次幕式火山噴發-構造變形-盆地充填-地殼隆升事件序列的釐定，從火山活動節律特徵、火成巖構造組合類型、時空分佈及其演化和構造變形的歷史記錄，利用巖石學、地球化學、同位素地質學等方法，反演深部過程與淺部響應等來闡明造山過程，建立與不同級別巖漿活動節律對應的殼幔動力學系統，追索殼幔深部過程，已成為當今地球動力學研究的前沿課題之一。
  14. On the basis of study on petrology, volcanic geology, geochemistry, isotopic chronology, antitheses of the regional strata and 4 suits of volcanic rock stratum of the yanshan - liaoning area, the rhythm of yanshanian volcanic activity is divided into 1 gigantic - cycle, 4 cycles, 11 micro - cycles, 24 sub - cycles and many rhythms. in addition, the temporal and spatial evolution and regional contrast of every - level rhythms are discussed. 3. based on the study on classifications of rhythm of volcanic activity and regional contrast, the petrology, mineralogy, geochemistry, and isotopic characteristics of every - level rhythms are discussed

    2 、通過對燕遼地區燕山期發育的四套火山巖的巖石學、火山地質學、地球化學、同位素年代學的綜合研究，通過運用綜合方法進行區域地層對比和分析火山噴發盆地火山巖地層特徵的基礎上，將本區燕山期火山活動節律，劃分為1個二級節律（大旋迴） 、 4個三級節律（旋迴） 、 11個亞三級節律（小旋迴） 、 24個四級節律（亞旋迴）和多個五級節律（韻律）等，論述了各級火山活動節律特徵及其時空演化和區域對比。
  15. The archaea contain many organisms of extreme environments, such as hydrothermal vents, hot springs, saline sediments, volcanic craters and boiling muds. they include methane - generating organ - isms ( methanogens ), sulfate reducers, and extremophiles

    古細菌包括許多生長在極端環境中的有機體，如高熱溫泉口，高鹽沉積地區，火山噴發處，沸騰的巖漿中等的生物有機體，還包括產甲烷菌等。
  16. Driven from their homes by the great eruption of 922 that destroyed the city of ithrak, a few mining families of the stonefist clan settled in these lava - burnt caverns

    在被922年摧毀艾瑟拉克的強烈火山噴發逐出家園之後，石拳氏族的小部分礦工家庭定居在火山巖洞窟之中。
  17. The ratio of y / ho in ores approximates to the ratio of black chimney in tag seafloor. the ore - forming fluids show high temperature and redox characteristics. in conjunction with the geological setting of the deposit, the primary ore - forming fluids might certain higher ree and higher volatile elements derived from the mantle degassing or the alkaline volcanic magmas

    同時結合礦床形成的構造一地質環境及礦體產出的地質形態，認為迅納廠稀七鐵銅礦床可能是在昆陽裂谷初期，在堿性火山巖漿噴發的間歇期，來自地慢富稀土、揮發份的成礦流體山火山噴流一同生沉積方式形成的礦床。
  18. To make the yanshanian volcanic tempral and spatial distribution and evolution law clear, study the relationship of the deep crust - mantle processes and the volcanic rocks, the author selects the typical areas, xishan of beijing, duolun of inner mongolia, west liaoning, as the study areas where the volcanic rocks strata are developed. through the emphasised geological profiles of yanshanian volcanic strata being surveyed, much field work being done detailly, the small volcanic eruptive units have been defined originally, the levels of volcanic activity rhythm being constructed gradually, as a result, a integrated and systemic rhythm of yanshanian volcanic acivity has been constructed

    為了揭示該區燕山期火山巖火山活動的時空分佈與演化特徵，探討與深部殼幔過程的關系，選擇了燕山期火山巖地層發育比典型的北京西山、內蒙多倫、冀北和部分遼西等地區，系統的測制了燕山期火山巖重點地層剖面，通過野外大量的詳細觀察，從建立最小的火山噴發單元開始，逐步地建立火山活動節律的級別，結合區域地層對比，建立了一個比較完整的燕山期火山活動節律及其級序。
  19. 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。
  20. Thick grey smoke, ash and lava continue to spew from the volcano which has been rumbling for weeks, 14, 000 people live within five miles of the volcano

    轟鳴數周的默拉皮火山噴發出滾滾濃煙，火山灰以及巖漿，火山方圓5英里內居住著1 . 4萬人。
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