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The correlativity in synesthesia also provides us with clues to examine the process of music expression from both direction-music creation and appreciation.

本文以联觉对应关系为基础,还从创作与欣赏双向对音乐表现对象的发生过程作了进一步的考察,回答了表现对象怎样进入到音乐中去?

The very reason why music can express non-audio concerns is the correspondance principle in synesthesia.

联觉对应关系规律是音乐之所以能够表现听觉之外对象的根本原因与最重要的基础。

This article is for the joint synesthesia through the analysis, to more systematically applied to vocal teaching, interest in learning, accelerated learning process; In its modest way as vocal psychology at the same time, another way Vocal enabled synesthesia to improve the learning process as an effective way to enrich vocal teaching

更多将其更系统地应用于声乐教学,提高学习兴趣,加速学习进程;在为声乐心理学略尽绵薄之力的同时,另辟蹊径,使联觉成为提高声乐学习进程行之有效的方法,更好地丰富声乐教学手段。

Nowadays, though, we have a new tool for resolving those tip-of-the-tongue nuisances: look it up on the internet.

Simner和Ward同时指出,这种经验是和我们大多数人所不同的,他们认为我们所有人都拥有词汇和味觉的联觉能力,但是它还处在潜意识水平之中。

How have artists used scientific concepts of synaesthesia in the past?

以前艺术家是如何理解联觉的科学概念的?

Why is there so little exchange of knowledge on synaesthesia between artists and scientists?

为什么艺术家和科学家之间对于联觉的交流如此匮乏?

Do artists and scientists speak different languages when it comes to synaesthesia?

艺术家和科学家对于联觉的看法是否大相径庭?

How synaesthesia starts (in other words, how the connections become so strong) is also unclear.

感观联觉是如何形成的(或者说,人脑内部的连通是如何变得这么紧密的)仍然是个迷。

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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。

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。

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。