pulsative中文是什么意思

發(fā)音:

中文翻譯
造句

adj.
＝pulsatile.

pulsative echoencephalography 腦回聲搏動圖
pulsative oscillation 脈沖式振蕩; 脈動振蕩
pulsative zoning 脈動分帶
pulsationwelding 脈沖焊接
pulsationsphygmus 脈博
pulsationcycle 脈動循環(huán) 脈動周期
pulsatoary oscillations 脈震動
pulsation-free output 無脈動輸出
pulsator n. 〔拉丁語〕脈動器。
pulsation welding timer 脈沖焊接計時器

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Clinical application ofaccelerating peripheral nerve regeneration by pulsative electrical stimulation
脈沖電刺激促進周圍神經(jīng)再生的應用
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。