扬子板块,Yangtze Plate
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
英文短句/例句
1.Lithofacies Paleogeographic Constraints of Southwestern Boundary between Yangtze and Cathaysian Plates in Caledonian加里东期扬子板块与华夏板块西南段分界线的岩相古地理制约
2.The North Lancangjiang suture: the boundary between Gondwana and Yangtze?北澜沧江带的性质——是冈瓦纳板块与扬子板块的界线吗?
3.THE CRUST-MANTLE LITHOSPHERE STRUCTURE ANDTHE PALEOZOIC BASINS ON THE NORTHERNMARGIN OF YANGTZE PLATE扬子板块北缘壳(慢)岩石圈结构与古生代盆地
4.Qinling fold belt is located at the junction of the North China plate and the Yangtze plate, and its portion in Henan Province is a part of the East Qinling Mountains (EQM).秦岭褶皱带位于华北板块和扬子板块结合部位，其在河南省内的部分多划为东秦岭。
5.The tectonics of Jiangnan recombination melange belt is very complex resulted from long actuation of Yangtse plate and Cathaysian plate.江南复合混杂岩带是扬子板块与华夏板块长期活动所致,构造极为复杂。
6.The deformational dynamics is controlled by the compressional settings which are caused by the minor-angle oblique subduction of the Izanagi Plate and the continent-to-continent collision betneen the Yangtze Plate and the North China Plate.变形动力学受控于伊泽奈崎板块的小角度斜向俯冲和扬子板块与华北板块陆陆碰撞造成的挤压背景。
7.The Yangtze plate drifted toward the north during Palaeozoic and the studied area reached 9° south latitude or so at the end of Cambrian and the beginning of Ordovician.古生代扬子板块由南向北漂移,寒武纪末—奥陶纪初本区到达南纬9°左右。
8.Yangtze and Huaxia continental blocks together formed uniform South China plate after many times tension and compression during the Caledonian Cycle.加里东旋回经多次拉张、挤压后,扬子陆块与华夏陆块拼合形成统一的华南板块;
9.A Few Thoughts on the Construction of “Nanjing-Zhenjiang-Yangzhou Economic Zone”;构建“宁镇扬经济板块”的几点思考
10.Research on Cooperation Development of Industrial Clusters in Nanjing-Zhenjiang-Yangzhou Economic Zone宁镇扬经济板块产业集群的联动发展研究
11.Middle Proterozoic Geotectonics in Northeast Sector of the Yangtze Massif扬子地块东北缘中元古代的大地构造
12.Characteristics of Upwelling Sedimentation in Cambrian in Southeast Margin of Yangtze Plate扬子地块东南陆缘寒武系上升流沉积特征
13.PLATFORM COPPER METALLOGENESIS OF WESTERN MARGIN OF YANGTZE CRUSTOBODY--CITE THE EXAMPLE OF YUNNAN SEGMENT扬子壳块西缘地台型铜成矿作用——以云南段为例
14.A Giant Palaeoslope Zone of Early Paleozoic Era in Southeastern Yangtze Landmass扬子陆块东南缘早古生代的巨型斜坡带
15.The identification of the Grenvillian granite on the western margin of the Yangtze Block and its geological implications扬子地块西缘Grenville期花岗岩的厘定及其地质意义
16.Strategy of Modern Logistics Service Industry Integrated Development in Nanjing,Zhenjiang and Yangzhou Economic Block;宁镇扬经济板块现代物流服务业一体化发展战略
17.The Cathaysian block is more mobile in comparison with the Yangtze block.华夏地块相对于扬子地块是比较活动的构造单元。
18.It was furnished with some old tables, a blackboard and an old stove.有几张旧桌子，一块黑板和一个旧炉子。
相关短句/例句
Yangtze paleo-plate扬子古板块
1.The correlation of evolutions betweenYangtze 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 theYangtze 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。
3)northern margin of Yangtze plate扬子板块北缘
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 thenorthern 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 ofYangtze 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
延伸阅读
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
