查询词典 end of line
- 与 end of line 相关的网络例句 [注:此内容来源于网络,仅供参考]
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Once published, his work became famous for the absence of rhyme at the end of each line.
出版后,他的作品因行末不压韵而闻名。
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Once published,his work became famous for the absence of rhyme at the end of each line.
发行后,他的诗作因为行尾不押韵而大获其名。
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Once published, his work became famous for the absence of rhyme at the end of each line.
下一代英国大诗人有约翰多恩的名字中国读者欣赏他的作品,是因为他使用令人惊奇的意象,会使人联想起苏东波等人的作品。
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Once published, his work became famous for the absence of rhyme at the end of each line.
他的诗作发表后,因为行尾不压韵而大获其名。
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Once publish ,his work became famous for the absence of rhyme at the end of each line .
他的诗作发表后,以行尾不押韵而大获其名。
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Once published, his work became famous for the absence of rhyme at the end of each line.
付印后,他的诗作因为行尾不押韵而大获其名。
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Once published,his work became famous for the absence of rhyme at the end of each line.
他的诗作发表后,因为行尾不押韵而大获其名。
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Once published his work became famous for the absence of rhyme at the end of each line.
Book2Unit4p28 他的作品一出版就出名了,因为诗的每一行末尾都不押韵。
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Once published , his works became famous for the absence of rhyme at the end of each line .
他的诗作一出版就因为行尾不压韵而大获其名。
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Once published, his work became famous for the absence of rhyme at the end of each line.
一旦付印,他的诗作因为行尾不压韵而大获其名。
- 相关中文对照歌词
- The End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- End Of The Line
- Standing At The End Of The Line
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。