oast中文是什么意思

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中文翻译
造句

n.
(烘麦芽等的)烘炉，烤房，干燥室。

oven; oast; oasthouse; dryoff oven 烘炉
oastar 奥士达
oasmaa 瓦斯马
oastes land 奥茨地
oasisfarming 绿洲农业；沃洲农业
oastler 奥斯特勒
oasis vegetation 绿洲植被
oat n. 1.〔常 pl.〕【植物；植物学】燕麦，雀麦。 ★ oats 是马的饲料，人吃的叫 oatmeal. 2.〔常作 pl., 用作单或复〕燕麦田；燕麦种子。 3.〔常作 pl., 用作单〕＝oatmeal. 4.〔诗〕麦笛，牧笛；牧歌。 adj. 燕麦做的；(燕麦)麦秆做的。 be off one's oats 没有胃口。 feel one's [its] oats (吃了燕麦的马)活泼地跳来跳去；〔美俚〕(人)自负，得意起来；〔美俚〕精神饱满，热情洋溢。 smell one's oats (马)快起来；(人)振奋起来。 sow one's wild oats 干年轻人的荒唐事；(年轻时)放荡；浪费青春。
oasis state 绿洲国
oat bird cherry aphid 黍缢蚜
oasis spa 水之屋

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例句与用法

According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。
Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field , including lithology , size distribution , sedimenta ry structure , geochemistry and paleontology etc . , the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt . it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal . the peat flat is the important paleoenviron ment for coal accumulation . the tidal channel destroys the coal bed . the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
文摘:根据肥城煤田石炭系太原组的岩性、粒度分布、沉积构造、地球化学及古生物等沉积特征，将该区晚石炭世古地理划分为碳酸盐开阔台地和潮坪环境，认为太原组形成于潮汐作用为主的陆表海海岸，泥炭坪是成煤的重要古地理环境，潮渠对煤层有一定的破坏作用，地壳的脉动性振荡作用是控制沉积环境演化和聚煤作用的主要因素。