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1)  Yangtze block
扬子地块
1.
Geological feature and structure environment of micro-fine disseminated gold deposit in the southwest edge of Yangtze block;
扬子地块西南缘微细浸染型金矿矿床地质特征及构造环境
2.
Some geochemi-cal characteristics of the same kind of rocks related to Cu-Au mineralizations are listed here, and these rocks are from the east Yangtze Block, the Tibet Plateau and the north Xinjiang.
文中概述了强烈亏损重稀土元素的中酸性火成岩(或埃达克质岩)的研究历史、现状和意义,列出了扬子地块东部、青藏高原以及新疆北部与铜金成矿有关的同类岩石的一些特征,重点分析了当前强烈亏损重稀土元素的中酸性火成岩(或埃达克质岩)的研究中所存在的问题,并提出了一些初步的设想。
3.
A total of 316 oriented core samples collected from the Devonian-Carboniferous carbonate strata from the southern Yangtze block in the southern Guizhou Province were subjected to stepwise demagnetization.
本文通过对扬子地块西南缘贵州独山—平塘地区泥盆—石炭纪316块定向岩心样品的系统退磁处理,揭示出晚侏罗世、新生代两期重磁化成分。
2)  Yangtze massif
扬子地块
1.
Late Paleozoic basic magmatism from SW Yangtze Massif and evolution of the Paleo- Tethyan Ocean;
扬子地块西南缘晚古生代基性岩浆岩的性质与古特提斯洋的演化
2.
Yangtze massif is known for the leading phosphogenetic area in China, especially in the times of Doushantuo and Meishucun ages when the sedimentary phosphorite account for 85% of the state's total phosphorus resources.
扬子地块是我国重要的产磷区 ,陡山沱与梅树村两大成磷期磷块岩储量占全国磷矿储量的85 %。
3.
A synthetical study of geomorphology, Quaternary, isotopic geochronology, tectonics and sedimentology shows that the orogenic belt in the western margin of Yangtze massif has been mainly risen since Cenozoic, especially the Quaternary, with a rising height of 2, 000-4, 000 m.
沉积的综合分析表明,扬子地块西缘造山带的主体隆升时期发生于新生代特别是第四纪以来,其隆升幅度可达2000~4000m,中新世以来至少有5~6km地层被剥蚀,上升速率约达0。
3)  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
4)  The Lower Yangtze Block
下扬子地块
5)  the upper Yangtze Continent
上扬子地块
6)  southeastern margin of Yangtze block
扬子地块东南缘
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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