火山形成 的英文怎麼說

中文拼音 [huǒshānxíngchéng]
火山形成 英文
construction of volcano
  • : fire
  • : 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...
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • 火山 : [地質學] volcano; burning mountain
  1. The study shows that cretaceous volcanics mainly consist of medium acidic volcanic lava and volcanoclastic rocks, with locally developed basic lava ; medium acidic volcanics mainly consists of calc - alkalic series, was formed in compressive orogenic environment, and has good reservoir property, while cretaceous basis lava mainly consists of alkalic series, was formed in rift environment, and has poor reservoir property

    結果認為,白堊紀巖以中酸性熔巖和碎屑巖為主,局部發育基性熔巖;中酸性巖以鈣堿性系列為主,於擠壓造環境,儲集性能較好,而白堊紀基性熔巖以堿性系列為主,於裂谷環境,儲集性能較差。
  2. The bulk of the volcano is basaltic, but the slopes are dotted with cones and lava flows consisting of glassy, silica - rich lavas called dacites

    的主體是玄武巖,但是坡卻點綴著由石英安巖(一種玻璃質、富含矽的熔巖)的熔巖錐和熔巖流。
  3. On the basis of the study on the petrology, trace element, and isotopic geochemistry, the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting. one is the basanite - alkaline basalt - olivine tholeiite magma series, which are generated by partial melting from spinel iherzolite ; the other is nephelinite magma - alkaline picritic basalt magma, which are generated by partial melting of the garnet iherzolite

    巖石化學、微量元素、同位素地球化學證據都表明,華北、華南地區的巖根據源巖和局部熔融程度的不同,可以分為兩個原生巖漿系列:一個是源巖為尖晶石二輝橄欖巖,隨著局部熔融程度的增加,的碧玄巖巖漿-堿性玄武巖巖漿-橄欖拉斑玄武巖巖漿;另一個是源巖為石榴石二輝橄欖巖,隨著局部熔融程度的增加的霞石巖巖漿-堿性苦橄玄武巖系列。
  4. Channels and vents form and disappear below the caldera

    口下面的管道及噴口不斷及消失。
  5. The eruptions were associated with the development of several giant craters ( calderas )

    大量熔巖和灰噴出,爆發多個破口。
  6. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造帶長期處于擠壓環境,伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失,導致造帶巖石圈迅速強烈拆沉伸展和減壓增溫熔融,從而大規模早白堊世花崗巖類和中酸性巖。
  7. Not far from leng shui keng is chutzuhu " bamboo lake ", where a lake was created in prehistoric times when a volcanic eruption sent debris rumbling into a valley, where it dammed up a stream. chutzuhu in recent years has become noted for its many flowers, especially the calla lilies that bloom every year from december

    冷水坑附近的竹子湖是堰塞湖,近來為花卉栽種區,每年的十二月起是海芋盛開的季節,朵朵素白色的花朵在錯落的梯田上一片花海,一陣淡淡的霧氣飄過,疑似人間仙境。
  8. Chaparral - covered slopes, caves. . a good place for weekend family picnic, hiking and climbing

    熾熱火山形成的絕頂奇石,猶如千面女郎,變化萬千,極適合野餐露營探險爬
  9. Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元,其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位的陸緣或島弧褶皺帶,具有古生代造帶的性質。研究區及鄰區印支期侵入巖於造帶強烈擠壓陸內俯沖的構造環境;燕早期侵入巖於由擠壓轉向拉伸、造帶的增厚陸殼開始發生伸展垮塌的構造環境;早白堊世於造期后進一步發生伸展垮塌的區域構造環境。
  10. In this case during paleozoic, nearly east west trending arc structures resulted from the interaction between china plate and siberian plate. in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault, diaoyudao fault, okinawa fault, uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate

    本文所涉及近東西向展布的弧構造於古生代時期中國板塊與西伯利亞板塊的碰撞帶,而在中生代,中國板塊下的kula - pacific板塊向西俯沖導致了北北東向和北東向構造(如duimadao斷層、 diaoyudao斷層、 okinawa斷層、隆起帶和沉降帶)以及位於中國板塊東部的巖漿帶。
  11. Distinct layers of ejected material on the volcanoes' slopes are allowing geologists to construct the chronological sequence of their formation.

    噴發出來的物質層次分明地留在斜坡上,使地質學家們可以確定它們的年代順序。
  12. Volcanic activity has been responsible for large chunks of surface morphology in the western states, alaska, and hawaii.

    活動是美國西部各州,阿拉斯加州和夏威夷州大片地的主要原因。
  13. 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噴發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。
  14. The study of the regional geological setting, occurence mode of ore body, ore rocks, and orecontrolling factors of shiyintan gold deposit indicates that it is an epithermal volcanic hydrothermal gold deposit

    摘要通過對石英灘金礦床區域地質背景、礦體產出態、礦石特徵、礦控制因素的研究,認為礦床因類型應屬淺低溫熱液型金礦床。
  15. Then a lake formed, probably after an eruption blocked some rivers or streams.

    可能是一次噴發之後,一些河流或溪水被堵塞了,了湖泊。
  16. And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates

    通過對測試數據的分析與綜合研究,並同中國和世界一般花崗巖類以及中國主要金、銅礦巖體的花崗巖類進行對比,得出本區花崗巖類巖石具有以下特徵:屬磁鐵礦-型或同熔型花崗巖,其巖漿物質具殼幔混源特徵:主要由熔融態巖漿經結晶分異作用,通過多期變速上侵而;其分異演化程度較低;寄主巖基和包體具有同源性;巖石的溫度范圍約為500 - 700 ,壓力大約為2 . 50gpa - 4 . 35gpa ,氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ;該巖帶主要於板塊碰撞前消減的活動板塊邊緣期,為燕至喜馬拉雅早期的大陸邊緣弧環境的產物。
  17. 2. 6 2. 7ga, these granitoids are most likely to be derived from the partial melting of hybrids both 2. 6ga metavolcanic materials in archean wutaishan magmatic arc and older continent crustal materials under lower than 1. 2gpa. petrological and geochemical characteristics of wangjiahui granitoid intrusion suggest that is probably fored under post - collisional tectonic background

    2 . 1ga在- 3 . 82 - 2 . 80范圍,表明王家會古元古代花崗巖最有可能於大約2 . 6ga五臺大洋島弧巖物質和更老的陸殼物質在
  18. On earth, haematite usually forms in water, but not always ; one type forms at the high temperatures found in volcanoes

    地球上,赤鐵礦通常於水中,但也並非沒有例外,特別的,的高溫也能促赤鐵礦的
  19. You can usually find good clay in low areas of islands or land, especially if volcanoes helped form the land

    一般在島嶼或是陸地的低洼地能夠找到很好的黏土,特別是火山形成的陸地。
  20. A series of volcanic caverns, tunnels and chambers that span out of isle of kezan through the ocean floor, connecting to adjacent smaller islands to the west of isle of kezan

    卡贊島底部遍布無數由火山形成的大型洞窟,隧道以及較小的洞穴,它們能跨海延伸到卡贊島西面的小島。
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