massifs

massifs的基本解释

n.

山丘( massif的名词复数 )

与massifs相关的网络例句 [注：此内容来源于网络，仅供参考]

Based on the fractal theory and the area data of the global continental massifs,both of the characteristic yardstick of the modern global continental massifs and their frequency have been analyzed and discussed in this paper.

根据分形理论和各板块的面积以及现代大陆各地块面积资料，分别进行了全球岩石圈板块和全球大陆地块自相似性特征尺度与频度关系的研究讨论。

Some massifs were piled up by the discarded porcelain slices over many years .Can you imagine that how many years could the massifs be shaped by the kiln factory on a large production of scale in the remote Tang Dynasty ?

有些小山丘就是当年窑场废气物累年堆积而成，真不知在那遥远的唐代，长沙窑是怎样的生产规模，又是延续了多少年，才能遗留下这么大量的残存物。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

与massifs相关的网络解释 [注：此内容来源于网络，仅供参考]

diskettes with drivers for RAID- massifs：磁盘驱动突击-岩体

CD disk with documents, drivers and utilities;光盘磁盘文件,司机和公用事业; | diskettes with drivers for RAID- massifs;磁盘驱动突击-岩体; | bridge for connection two video card;大桥连接两个视频卡;