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onsets相关的网络例句

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与 onsets 相关的网络例句 [注:此内容来源于网络,仅供参考]

The interpretation of the results from these two experiments may be that the subjects were aware of the existence of the onsets in the surface form in the initial positions of the suffixes –a and –e; however, they didn't consider this kind of onsets as underlying.

对於这两个实验的结果我们的解释为:受试者应该意识到在表层结构中,是有子音存在在词缀&仔&及&个&之前的,但是他们并不认为这样的声母子音是存在於深层结构中。

Before the occurrence of ENSO, due to the anticyclonic anomaly in midlatitude of the South Indian Ocean, the anticyclonic anomaly over Australia tends to be enhanced through the dispersion of Rossby wave; In the meantime, the equatorial convergence of the southerly anomaly off the east of Australia and the northerly anomaly in the Philippine excite the onsets of the westerly anomaly in the equatorial western Pacific and the occurrence of ENSO.

在ENSO发生前,南印度洋中纬度为反气旋异常,并通过Rossby波的频散作用加强了澳大利亚附近的反气旋异常;同时,澳大利亚东部沿海的南风异常与菲律宾附近的北风异常在赤道辐合,促进了赤道西太平洋西风异常的爆发和其后ENSO的发生。

The nasalization distinguishes itself in four aspects, including the nasal spreading can be bi-directional, the nasal spreading exhibits different situations between open and close syllables, vowels preceding nasal codas can not be nasalized, and postvocalic glottal stops and glides must agree with nasal onsets. The literature background is based on seven proposals, including Lin's (1992) proposal, Li's (1992) right-spreading theory, Wang's (1995) bi-directional spreading theory, Ang's (1996) downward-spreading theory, Chung's (1996) domain percolation, Ang's (2001) and Chou's (2002) OT analysis.

闽南语鼻音主要有四个特徵:闽南语鼻音扩散可以是双向的;闽南语鼻音在开音节与闭音节里呈现不同的扩散现象;鼻音化子音前的母音无法受到鼻音化;元音后喉音及滑音必须与韵首子音行形成鼻音上的和谐。

At pentad 31 or 32 and after monsoon onsets, precipitation, convection, low-level west wind and SST extend northeastward, and at nearly pentad 41 they arrive at the most northeast zone quickly, and then their intensities decrease, but they still have a trend of extending eastward.

在31或32候(6月初)季风爆发后降水、对流、西风和海温开始向东向北扩展,在41候(7月下旬)左右时都迅速达到最北地区,之后强度减弱,但仍有向东扩展的趋势。

But due to Pucheng's devoicing of ancient obstruent onsets, the [32] tone contour lacks obvious characteristics of either IVA or IVB, so it is difficult to reach a conclusion as to whether it is voiceless IV merged with IVB or voiced IV merged with IVA.

但由于浦城古全浊声母已经清化[32]的调值也缺乏明显的阴调或阳调的特征,所以难以断定究竟是清入归阳入,还是浊入归阴入。

Pucheng dialect's IVA syllables and IVB syllables can merge, just because its obstruent onsets had already devoiced, not preserving the cause of the natural division between voiceless A and voiced B.

浦城方言的阴入字和阳入字之所以可以合并,正是因为它的全浊声母已经清化,不存在清阴浊阳的天然界线的缘故。

For example, the merger of ancient voiced obstruent onset tone IV syllables into IB covers the whole Mandarin area except for Jiangsu and Anhui which preserve tone IV, and the merger of sonorant onset tone IV syllables into III covers the Mandarin areas of Hebei-Shandong, Lanyin, Beijing, the Northeast, Liaoning, etc., and the merger of voiceless onsets into IA covers the Mandarin areas of the central plains and Hebei-Shandong.

例如,古全浊声母入声字归阳平的读法涵盖了除保留入声的江淮官话以外的所有官话区,古次浊声母入声字归去声的读法涵盖了冀鲁、兰银、北京、东北、胶辽等五个官话区,古清声母归阴平的读法也涵盖了中原官话和冀鲁官话。

The major conclusions of this paper are as follows:(1) WNPSM onsets at pentad 31 or so, ends at pentad 60, lasts a period of five months.

本文的主要结论如下:(1)西北太平洋夏季风在31候(6月初)前后爆发,60候(10月末)结束,历时5个月。

According to the theory of wavelet transformation, the singularities of the ECG signal are corresponding to the series of maximum-minimum pairs. The algorithm detects the onsets of Q wave at the scale 3 detail and offsets of T wave at the scale 4 detail. So the duration of QT is calculated by onset of Q wave and offset of T wave.

根据小波变换的原理,心电中的奇异点在变换后将产生一个模极大值和模极小值对,在小波变换3尺度上检测出QRS波群的起点,在小波变换4尺度上检测出T波终点,从而确定QT间期。

Results show that the Spiti shale in Zanskar terminated 15Ma later than that in southern Tibet, while the lowermost Cretaceous quartz sandstone in Zanskar appeared 18Ma later than that in southern Tibet. The age of volcanic sandstone in southern Tibet is very poorly time constraint and their deposition occurred somewhere within Berriasian~early Albian. In Thakkhola, the Chukh Group volcanic sandstone are of late Hauterivian-early Albian age (duration about 20Ma), while in Zanskar, the volcanic sandstones facies only appeared in Albian (duration of less than 10Ma). Therefore, it can be concluded that the onsets of both quartz sandstone and volcanic sandstone occurred earlier in eastern Tethys Himalayas than in western Tethys Himalayas .

侏罗纪末~白垩纪初印度大陆的北缘同时期存在大陆向上挠曲,导致陆源碎屑输入量的快速增加,石英砂岩广泛存在;早白垩世火山岩屑砂岩对应着的印度大陆北缘地层侵蚀加深,使得较深部的深成火山岩暴露并遭受侵蚀;石英砂岩和早白垩世岩屑砂岩所代表的印度大陆剥露时间在空间上的&东早西晚&,说明构造运动首先是从特提斯喜马拉雅的东部开始(大印度与澳大利亚的彻底分离),然后逐渐波及西部的,东西时间差为15~20Ma;由于地壳均衡作用,大陆分离后原先地壳挠曲转变为地壳下沉,发生强烈的构造沉降,故Albian之后沉积一套深水环境下的海绿石、磷酸盐和黑色页岩沉积。

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