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1)  lower crust of the Yangtze continent
扬子大陆下地壳
2)  Continental lower crust
大陆下地壳
1.
A series of astonishing discoveries including seismic reflective,low velocity layer, and low resistivity layer in continental lower crust suggest that we should recognize continental lithosphere, and approach continental lower crust.
下地壳反射层 (或反射下地壳 )、下地壳低速层和低阻层等一系列惊人发现唤醒我们必须重新认识大陆岩石圈 ,研究大陆下地壳。
2.
The major results about magnetic petrology of high-grade terrenes of Archean shield areas in the world are reviewed in this article,focusing on the relationship between rock magnetism and deformation, and metamorphism and intensity of magnetization of continental lower crust and its origin.
综述国际上有关太古宙高级地体磁性岩石学研究的主要成果,侧重高级地体岩石磁性与变形、变质等级的相互关系及大陆下地壳磁化强度及其成因机制等;提出了有关高级地体岩石磁性研究中值得注意的几个问题。
3.
Continental tectonics is akey frontier that involves following important areas such as the formation and evolution oforogenic belts and sedimentary basins, three-dimension layer-block texture of continentallithosphere,thermal and rheological state of continental lower crust,seismic genesis anddynamic sources of continental crust movement.
大陆构造是大陆动力学的核心领域,涉及到盆地和造山带的形成与演化、大陆岩石圈三维层块结构、大陆下地壳的热状态和流变状态、大陆地震成因和大陆地壳运动的动力来源等一系列重大课题。
3)  mid lower continental crust
大陆中、下地壳
4)  Yangtze Continent
扬子大陆
1.
The indosininn-Yanshanian (245-122Ma) two-mica granites are widely distributed in the Sonth China Continent and the Tianshui-Yajiang region,and the foreland fold-belts are developed on both sides of the Yangtze Continent.
华南大陆与天水-雅江地带广泛分布中生代王云母花岗岩侵作入体,已有的同位素年龄范围为245~122Ma,与此同时,它们两侧的扬子大陆发育前陆褶皱带,这种成对性及其构造配置表明,扬子大陆曾向华南大陆与松潘—甘孜褶皱带发生过陆内俯冲作用。
5)  West Yangtze continent
西扬子大陆
1.
Devonian sedimentary evolution and mineralizationon the West Yangtze continent;
西扬子大陆区泥盆纪沉积演化与成矿
6)  the Yangtze paleocontinents
扬子古大陆
补充资料:扬·比比扬历险记

《扬·比比扬历险记》是保加利亚著名作家埃林·彼林(1877~1949)保加利亚著名作家最著名的一部作品,描写一个顽劣的、不听教导的男孩,干了许多坏事,最后还在小魔鬼阿嘘的诱惑下,被换掉了脑袋,骗入魔鬼王国。在魔鬼王国中,他的智慧和善良慢慢苏醒了,终于战胜了恶魔米里莱莱,冲出了魔鬼王国并找到了自己的脑袋,成了一个好孩子。 后来作家还写过一部《月亮上的扬·比比扬》,同样受到孩子们的欢迎。

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