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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 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。
3.
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;
4.
South China (studying area) is composed of the Cathaysian block and the southeastern part of Yangtze block.
华南(研究区)由杨子地块东南部和华夏地块组成。
5.
The intension of the term Cathaysian block (continent block) in the recent magazines is not that of the original Cathaysian old land.
近期一些文献中的华夏地块(陆块)的内涵已经不是原来的华夏古陆。
6.
Property: South China Plate, who is the biggest winner?
楼市:华南板块,谁是最大的赢家?
7.
PROTEROZOIC TECTONIC SLICES ALONG THE NORTHERN MARGIN OF NORTH CHINA PLATE
华北板块北缘活动带元古宙构造岩片
8.
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。
9.
Predevonian Tectonic Evolution of South China: from Cathaysian Block to Caledonian Period Folded Orogenic Belt
华南前泥盆纪构造演化:从华夏地块到加里东期造山带
10.
Accordingly, the South China was an Early Paleozoic orogenic belt instead of the Cathaysian Block (Paleocontinent).
因此,华南是早古生代形成的造山带,而不是华夏地块(古陆)。
11.
PALAEOGEOGRAPHIC POSITION OF THE SOUTH CHINA PLATE DURING THE LOWER-MIDDLE DEVONIAN
早—中泥盆世之交华南板块的古地理位置
12.
Paleomagnetism and Paleotectonics of North China Plate in Jurassic and Cretaceous
华北板块东部侏罗纪、白垩纪古地磁与古构造
13.
The Study of Countermeasure about the Gread Residential District in Guangzhou "Huanan Project";
广州“华南板块”大型居住区建设对策研究
14.
Mycorrhizal Synthesis of Tuber Indicum with Pinus Armandii, Castanea Mollissima and Quercus Franchetii
印度块菌与华山松、板栗和锥连栎的菌根合成
15.
Evolution and hydrocarbon potential of the marine strata on the southeastern margin of the North China plate
华北板块东南缘海相层系演化特征及油气远景
16.
Timing of the Transformation from Seafloor Spreading on the South Margin of the North China Block to Subduction within the North Qinling Orogenic Belt
从华北陆块南缘大洋扩张到北秦岭造山带板块俯冲的转换时限
17.
Qinghai is geographically located in northeastern Qinghai-Tibet Plateau and tectonically in the mid-western part of the Pan-Cathysian Block Group and the north part of eastern Tethys.
青海位于青藏高原东北部、泛华夏陆块群的中西部,东特提斯的北部。
18.
The data offered here favor that the collision between the Yangtze and Cathysia blocks happened in the late Proterozoic era.
现有资料支持华夏和扬子两地块在晚元古代碰撞拼合的解释。