1) the Yangtze paleocontinents
扬子古大陆
2) 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。
3) Tarim-Yangtze Paleocontinent
塔里木-扬子古大陆
4) Tarim-Yangtze paleocontinent reconstruction
塔里木-扬子古大陆再造
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) Yangtze-Cathaysia
扬子-华夏古陆
补充资料：尚古子
1.见"尚古自"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条