1) Yangtze Plate
扬子板块
1.
Paleomagnetic feafures of middlepaleozoic rocks from western Zhejiang and southern Anhui, Yangtze Plate;
扬子板块浙西皖南中古生代古地磁特征
2.
Middle Proterozoic geotectonics in the northeast margin of the Yangtze plate;
扬子板块东北缘中元古代的大地构造划分
3.
Progressive deformation of Middle Paleozoic marine basins in the Yangtze plate, China;
扬子板块海相中古生界盆地的递进变形改造
2) Yangtze paleo-plate
扬子古板块
1.
The correlation of evolutions between Yangtze paleo-plate and Tarim paleo-plate was analyzed using the petrology of orogenic belt in the edge of plate.
研究结果表明,从新元古代至二叠纪,扬子古板块与塔里木古板块靠近,成为一个大陆,称为"塔里木—扬子古大陆"。
2.
Whether the Tarim plate or the North China plate were close to the Yangtze paleo-plate during its geodynamic evolution, and issues relating to the reconstruction of the Chinese continent have been debated for a long time.
扬子古板块在地史演化中,是与塔里木板块靠近还是与华北古板块相近,这是中国大陆再造中长期争论的问题。
4) NW margin of Yangtze Platform
扬子板块西北缘
5) northern part of the western margin of the Yangtze block
扬子板块西缘北段
1.
Neoproterozoic granitoids are widespread in the northern part of the western margin of the Yangtze block.
扬子板块西缘北段新元古代花岗岩类分布较广。
6) Yangtze plate
扬子地块
1.
Based on the survey , analysis and contrast of 19 Cambrian sections in southeast margin of Yangtze plate, it is considered that the black carbonaceous shale, silicic shale, silicic belt and conglomeration and phosphorus bed & conglomeration are formed by the upwelling in Palaeotethys in passive continental margin.
通过下扬子地块东南陆缘区 1 9条寒武系剖面的实测、分析和对比 ,认为该区寒武系中的黑色炭质页岩、硅质页岩、硅质条带和结核以及磷矿层和磷结核等是古特提斯海中上升流作用在这被动大陆边缘区形成的 ,上升流引发缺氧事件 ,造成有机质丰富的沉积 ,形成烃源岩、石煤和磷矿等 ,分析了该区上升流沉积的特征、形成演化、分布规律及其与油气的关
补充资料：扬子途中
【诗文】：
楚塞望苍然，寒林古戍边。秋风人渡水，落日雁飞天。
第二百五十八卷
【注释】：
【出处】：
全唐诗：卷257_19
楚塞望苍然，寒林古戍边。秋风人渡水，落日雁飞天。
第二百五十八卷
【注释】：
【出处】：
全唐诗：卷257_19
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