oast中文是什么意思

發(fā)音:

中文翻譯
造句

n.
(烘麥芽等的)烘爐，烤房，干燥室。

oven; oast; oasthouse; dryoff oven 烘爐
oastar 奧士達
oasmaa 瓦斯馬
oastes land 奧茨地
oasisfarming 綠洲農(nóng)業(yè)；沃洲農(nóng)業(yè)
oastler 奧斯特勒
oasis vegetation 綠洲植被
oat n. 1.〔常 pl.〕【植物；植物學】燕麥，雀麥。 ★ oats 是馬的飼料，人吃的叫 oatmeal. 2.〔常作 pl., 用作單或復(fù)〕燕麥田；燕麥種子。 3.〔常作 pl., 用作單〕＝oatmeal. 4.〔詩〕麥笛，牧笛；牧歌。 adj. 燕麥做的；(燕麥)麥稈做的。 be off one's oats 沒有胃口。 feel one's [its] oats (吃了燕麥的馬)活潑地跳來跳去；〔美俚〕(人)自負，得意起來；〔美俚〕精神飽滿，熱情洋溢。 smell one's oats (馬)快起來；(人)振奮起來。 sow one's wild oats 干年輕人的荒唐事；(年輕時)放蕩；浪費青春。
oasis state 綠洲國
oat bird cherry aphid 黍縊蚜
oasis spa 水之屋

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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
根據(jù)肥城煤田石炭系太原組的巖性、粒度分布、沉積構(gòu)造、地球化學及古生物等沉積特征，將該區(qū)晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環(huán)境，認為太原組形成于潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環(huán)境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環(huán)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:根據(jù)肥城煤田石炭系太原組的巖性、粒度分布、沉積構(gòu)造、地球化學及古生物等沉積特征，將該區(qū)晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環(huán)境，認為太原組形成于潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環(huán)境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環(huán)境演化和聚煤作用的主要因素。