1.
Preliminary Discussion on Sedimentary Tectonics of the Clustered Continents of South China
浅议华南陆块群的沉积大地构造学问题
2.
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;
3.
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
4.
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)。
5.
BASIC FEATURES AND EVOLUTIONAL PROCESS OF DISPERSED BLOCK OF MESO-CENOZOIC SOUTH CHINA CONTINENTAL MARGIN
中、新生代华南陆缘离散地块的基本特征及演化过程
6.
The Mesozoic Tectonic Evolution and Pb-Zn-Ag Metallogeny in the South Margin of North China Craton;
华北陆块南缘中生代构造演化与铅锌银成矿作用
7.
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。
8.
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。
9.
And then,the discussed question falls on therelationship between the floras of the ancient lands and the Cathaysian flora.
然后分别讨论了各个古陆或陆块与华夏植物区系的关系.
10.
the land mass gradually moved to the colder areas in the South,
这个大陆块慢慢地移向南方更冷的地区，
11.
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
12.
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
13.
ARCHITECTURE AND IDENTIFICATION OF LARGE QUATERNARY MASS TRANSPORT DEPOSITIONS IN THE SLOPE OF SOUTH CHINA SEA
南海陆坡大型块体搬运体系的结构与识别特征
14.
Property: South China Plate, who is the biggest winner?
楼市：华南板块，谁是最大的赢家？
15.
We suggested that all the Early Paleozoic poles for NCB were placed in the Atlantic, and the NCB located in the southern hemisphere at about 15 degrees in the Early Paleozoic.
与此相应，华北地块位于南纬15°左右．
16.
A CONTRAST RESEARCH BETWEEN THE BAIDENG SHALLOW-SEA FACIES AND QINGLONGSHAO CONTINENTAL FACIES PHOSPHORITE IN YUNNAN PROVINCEE
云南白登浅海相磷块岩与青龙哨陆相磷块岩的对比研究
17.
The deposition of the foreland basin and the intracontinental shortening are the response to the Indosinian collision and convergence between the Yangtze and Cathaysian blocks.
这些指示扬子和华夏陆块在印支期发生了强烈陆内碰撞与会聚及前陆盆地的沉积作用。
18.
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。