巖成土 的英文怎麼說

中文拼音 [yánchéng]
巖成土 英文
regosol
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  1. Mountains and ridges of rough lava are furrowed with narrow valleys of alkaline soil sheltering a few grasses and shrubs

    在熔的山脈和山脊間,狹窄山谷內的鹼性壤上零星散布著草叢和灌木。
  2. In the amur region there are practically unlimited reserves of kaolin rocks and anorthosites, that also will allow to decrease the cost price of final production : aluminium and silicon

    事實上在阿穆爾河地區擁有著無限的高嶺石和粒狀火儲備,這也可以降低鋁和硅最後生產的本價。
  3. The formation of a tight syncline in the tuchengzi formation is depicted accurately. 3. there are three main clast types in the conglomerate : andesite, limestone, and dolomite

    4 、確定了城子組礫中的三種主要礫石分(安山、灰和白雲礫石)的來源。
  4. Therdly because of the influence of terrain and geological structure, arenaceous resources of different regions are different in mu us. sands are mainly from riverway in northwest ; from efflorescent cretaceous sandstone on account of higher topography in the middle part of mu us ; and sands resources are intricated in southeast, mainly including riverway sands, sands blown by the wind and embedded sands under so

    3 、毛烏素沙地因受地形和地質構造影響,不同區域的砂質來源情況不盡相同,西北部地區主要為河道沙;中部地區地勢較高,為白堊系基裸露而風化沙;東南部地區沙質來源情況復雜,主要有:現代河道砂、風積沙、也有埋藏在現代壤之下的出露古沙。
  5. The historic centre of arequipa, built in volcanic sillar rock, represents an integration of european and native building techniques and characteristics, expressed in the admirable work of colonial masters and criollo and indian masons

    秘魯阿雷基帕城歷史中心由火山石建,它代表了歐洲與本建築技術、風格的融合,這些技術和風格體現在殖民宗主、克里奧爾人和印度人的作品中。
  6. It was followed by the swift flashes of the rifles, which sent their leaden messenger across the rock in volleys, as though the assailants would pour out their impotent fury on the insensible scene of the fatal contest.

    緊接著,火光閃閃,槍彈越過雙方之間的石,排地飛射過來,彷彿他們要把自己無可奈何的憤怒,全都發泄在進行這場殊死搏鬥的這片無知無覺的地上似的。
  7. Edge of the granule image by video is the key of its image partition, the article tries to carry through a deeper research on image partition at the same time. granule is made up of savageness mater and industry material ( including of rock, sand, earth, atomy, steel, china, concrete, ink powder, magnetism powder, light fine and tiny powder used silicon, cell etc. )

    顆粒是構天然物質和工業材料(石、礦石、沙子、泥、塵埃、鋼鐵、陶瓷、水泥、墨粉、磁粉、光纖和料封裝材用高純硅微粉、細胞等)的基本單元,顆粒尺寸(粒度)是顆粒的首要特徵和粉體材料的第一指標。
  8. Tourists visiting tsochen rural township for the first time are sure to be impressed by the chalk badlands, and by the bambusa stenostachya bamboo that has grown there since japanese colonial times. the ground in tsochen is mainly made up of the mt

    第一次來到左鎮的觀光客,一定會對觸目所及由白堊的青灰惡地貌,以及至日據時期種植至今的大量刺竹林蔭景觀印象深刻。
  9. The geologic, element and experimental study suggest the mechanism of small body, giant deposit in jinchuan is succeeding segregation whole magma chamber intruding from deep to emplace. the study is proof, supplementary and progress of the deep segregation, penetrating ore formation theory, which was advanced by mr tang zhongli, the academician of china. 5

    特別是通過鉑族元素、稀元素研究、實驗地球化學研究及其與實際資料的對比,提出了金川礦床礦是從深部到侵位持續熔離的新模式,論證、補充和發展了湯中立院士提出的深部熔離礦說。
  10. Evidence of the early stage weathering pedogenesis by carbonate rock

    碳酸鹽早期風化作用的證據
  11. Effects of soil - forming rocks and sprout ages on the bark quality of pteroceltis tatarinowii

    和條齡對青檀檀皮質量的影響
  12. In this paper, the engineering properties of gypsum, especially, the engineering properties of weathered mud - stone and geo - synthetics before and after soaking by acid water are discussed in detail

    本文對鹿寨磷石膏、風化泥工合材料經酸性磷石膏渣漿水浸泡后的物理力學性質進行了較為詳細的試驗研究。
  13. During the yanshanian phrase, the area is in the condition of contractional background, with multi - staged tectonic reversion. 5. through studying the origin of volcanic rocks and the characteristics of magma evolution, it concludes that there exist 3 originated areas of magma - from mantle, crust, and mantle - crust exchange. the basic magma of nandaling volcanic rocks of early jurassic is derived from upper mantle ; the magma of tiaojishan volcanic rocks of mid jurassic is formed in the contractional tectonic setting, and derived from the transition zone of crust and mantle interaction ; the acid magma of l

    5 、通過石化學、微量元素、稀元素的研究,探討了不同級別節律的火山因、漿演化等特徵,認為本區燕山期火山有三個漿源區,即地幔源、地殼源和殼幔混源,早侏羅世的南大嶺旋迴的基性漿,起源於上地幔;中侏羅世髫髻山旋迴火山是在相對擠壓環境中,漿起源於殼幔過渡帶;晚侏羅世無負eu異常的酸性漿來源於下地殼的古老結晶基底的局部熔融,有負eu異常的酸性漿來源於上地殼的局部熔融;早白堊世火山基性漿起源於上地幔,中性漿起源於下地殼底部的殼幔過渡帶。
  14. There is a close relation between mesozoic tectonic evolution, fluid evolution, petrogenesis and mineralization in the manzhouli - e ' erguna region in the northeast of the northern orogenic belt, china, and three evolution stages of the mesozoic tectonic - fluid - petrogenetic and metallogenetic system are proposed out : 1 ) acompanied by ree and cu mineralization, the calc - alkaline volcanic rocks and mantle - crust mixed type granite occurred under the regional tension tectonic background caused by the mongolia - okhotsk residual ocean that was closing in scissors form in the early - middle jurassic. 2 ) acompanied by pb, zn and ag mineralization, the calc - alkaline and alkaline volcanic rocks occurred under the regional shear - compression tectonic background in the late jurassic. 3 ) acompanied by u, f, pb, zn and ag mineralization, the caic - alkaline and alkaline volcanic rocks occurred under the regional tension tectonic background in the early cretaceous

    摘要本文討論了北方造山帶東北段滿洲里額爾古納地區及其毗鄰區中生代構造流體礦系統及其演化的三個不同階段: 1 )早中侏羅世張性「似裂谷環境」下所形的中基性堿性火山、同熔性花崗及深源流體活動形的稀礦床和斑性銅鋁礦床; 2 )晚侏羅世擠壓剪切環境下所形的酸性火山、斑類及深源流體活動所形的鉛鋅銀礦床; 3 )早白堊世張性環境下所形的基性堿性火山及深源流體活動所形的鈾礦床、金銀礦床及螢石礦床。
  15. And we have got the following result : 1. the technique of storing water in soil in gneiss area of tai - hang mountain : the more water in soil before rain is, the less water capability of soil is, the time shorter of water flowing from soil is, the easier the water flows on the ground ; the soil capability of reserving water of different soil thickness is terrace > acacia land > pine land > grass land, so the soil is more thick, the soil capacity which contains water is more large ; the accumulated water that flows on the ground is remarkable related with the logarithms of rain time

    太行山片麻壤蓄水規律:雨前壤含水量越高,壤可蓄水量越小,出流所需時間越短,容易形地表徑流;不同層厚度的壤蓄水量為:梯田刺槐林地油松林地草地;累積地表徑流量與降雨時間的對數呈顯著正相關,擬合方程為w = a + blnt ,相關系數均大於0 . 92 ,即在降雨強度一定的前提下,降雨時間越長,累計地表徑流量越多。
  16. Several lines of evidence, including studies on geochemistry of trace elements and rare earth elements, isotopes ( s, c, o, d, and pb ), and fluid inclusions, suggest that the main ore - forming materials were scavenged from the contemporaneous sediments and that the fluids were predominantly derived from deep circulated basin brines, recharged by meteoric water, and ancient seawater

    微量元素、稀元素、同位素( s 、 c 、 o 、 d 、 pb )和流體包裹體特徵表明礦物質來源於同沉積的賦礦圍礦流體系大氣降水為主要補給源的深循環盆地鹵水和與沉積物發生了同位素交換的埋藏古海水。
  17. The world of nocturne was a harsh, volcanic place, a land of rocky crags and soaring, basalt mountains with little to offer its early colonists save the riches of its vast mineral deposits

    那克恩是荒涼的,裹挾著巨石和懸崖,以及大片的火山地帶,遠古時期形的玄武為了殖民地的主要開采源。
  18. Based on the study on ree distribution characteristics of sinian low grade metamorphic rocks of the basement and cover volcanics, the author makes a discussion on the material source and the genesis of xiangshan volcanics, and suggests that xiangshan volcanics came mostly from the remelting of the upper crust, and the genesis should be attributed to the category of remelted granites

    摘要本文通過對相山火山盆地基底震旦系淺變質、蓋層火山元素分佈特徵的研究,探討相山火山的物質來源及因,認為相山火山主要是上部地殼重熔的產物,其因應屬于重熔型花崗的?疇。
  19. The results demonstrate that the pingba red residua is a typical in situ chemical weathering crust, and the material sources of the profile are derived from underlying triassic dolomites, the chemical weathering of dolomite can be divided into two stages : " leaching - accumulating trend " and weathering trend ", the stable teconic and whole weathering of dolomite should be the main reason for the development of thick and consecutive red weathering crust overlying dolomite rock in central guizhou

    結果顯示該剖面是下伏基白雲風化並累積的結果,無其他外來物源,是原位風化殼;過程具有兩階段模式特徵,即白雲石、方解石的溶蝕酸不溶物累積和酸不溶物進一步風化兩個階段;長時期的構造穩定和白雲整體溶蝕作用是黔中地區白雲風化殼層厚度大、分佈連續的主要制約因素。
  20. The data indicated that chemical and physical characters of soil in different vegetation types which in same climate type have some difference. that reflected chemical and physical characters of soil not only have relation with soil parent material, climate, physical chemical characters of chemical elements itself, but also with vegetation types

    數據表明,在同一氣候條件下,所覆蓋植被類型不同,壤理化性質也有差異,反映了壤理化性質除了與其、氣候和化學元素自身物理化學性質有密切關系外,植被類型的作用不可忽視。
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