华南板块

广州华南板块大楼盘开发引发的区域结构二元化初步研究

The pilot research of region structure duality due to great building-muster of South China block in Guangzhou

分隔华北板块和华南板块的秦岭造山带内部存在两条缝合带，指示其经历了多期裂解和碰撞。

The Qinling orogen , dividing the North China block and the South China block , is thought to have evolved by the multistage rifting and collision over a prolonged history , with two mountain chains and two sutures .

这些年龄值与苏鲁超高压变质带内已有的多硅白云母~（40）Ar/~（39）Ar年龄基本一致，表明郯庐断裂带形成于华北与华南板块的碰撞造山期。

These ages are basically consistent with phengite ~ ( 40 ) Ar / ~ ( 39 ) Ar ages obtained from inner parts of the Sulu orogenic belt , indicating that the Tan-Lu fault zone was developed during the period of collision between the North and South China plates .

华南板块泥盆纪层序地层及海平面变化

Devonian sequence stratigraphy and sea-level changes within the South China plate

华南板块的内部结构和原生金刚石的地质意义

South China intraplate texture and geological significance of original diamond

楼市：华南板块，谁是最大的赢家？

Property : South China Plate , who is the biggest winner ?

泥盆纪华南板块古地理的位置及其漂移

The Paleogeographical Position and Drifting of the Southern China Plate in Devonian

海西-印支期华南板块的沉积特点

Evolution of sedimentation of South China plate in the Hercynian Indosinian stage

从华南板块构造演化探讨中国南方油气藏分布的规律性

Study on the distribution characteristics of petroleum deposits from the plate tectonic evolution in South China

贵州紫云运动与泥盆纪末华南板块海退事件的因果关系研究

Research on Causality of Guizhou Ziyun Movement and the Regression of Late Devonian South China Plate

混合岩穹隆中所残余含柯石英榴辉岩表明了胶东半岛和苏鲁地区具有相同的构造演化过程，烟台青岛五莲断裂不是华南板块与华北板块间的缝合带。

The Yantai Qingdao Wulian fault was not a suture between the North China and South China Blocks .

扬子板块与华南板块对接带萍乡区段构造特征

Tectonic characteristics in the Pingxiang area in the junction belt between the Yangtze plate and South China plate

加里东运动以后，扬子和华夏陆块拼合成统一的华南板块。

After the Caledonian orogeny , the Yangtze plate and the Cathaysia landmass were matched together to be the united plate of south China .

前陆沉积与变形构造也表明该断裂带在华北与华南板块碰撞中就发生了活动。

The foreland sediments and structures also show the activity of the fault zone during the collision of the North and South China plates .

与华南板块东南缘白垩纪的古地磁数据对比表明，晚白垩世海南地块仍是华南板块的一部分。

Compared with the Cretaceous paleomagnetic data from the southeastern Huanan Block , Hainan Island is a part of the Huanan Block in Late Cretaceous .

泥盆纪时期，随着古特提斯洋的开启，于华南板块南、西、北缘形成被动陆缘构造背景。

The passive continental margina are formed in southern , western and northern margins of Huaxia Plate during Devonian because of the opening of Old Tethys .

随着华南板块各个大盘开发进度的不断推进，各大发展商的明争暗斗也逐渐进入白热化。

South China plate with the constant progress in promoting the development of various industries , major developers businesses have gradually entered hotter by the day .

扬子地块西南缘，属华南板块南部，跨扬子陆块和南华活动带两个大地构造单元。

SW Margin of the Yangtze Block , belonged to South part of the South China Plate , spans two geotectonic units of Yangtze Landmass and South China active zone .

这些发现为研究本区加里东期的大地构造环境和变形特点、扬子板块与华南板块的相互作用提供了新资料。

These findings provide new information for the study of the Caledonian tectonic setting and deformation features in the area and the interaction between the Yangtze and South China plates .

郯庐断裂带在华北与华南板块碰撞之后是否发生过大规模左行平移及其准确的时间，仍然是存在着争议的重要问题。

It is still debatable whether or not large-scale left-lateral displacement took place along the Tan-Lu fault belt after collision of the North and South China plates and when the displacement happened .

安徽省绩溪县榧树坑金矿床处于华南板块北东缘的皖浙坳褶带，白际岭天日山断裂与绩溪宁国断裂之间。

The Feishu Keng gold deposit , Jixi , Anhui lies in the Wan-Zhe depression-folding zone at the northeast fringe of South China Plate , between the Baljiling-Tianmushan fault and Ningguo fault .

由此可见，中古生代是南秦岭，华南板块和冈瓦纳大陆地质演化过程中一个非常重要的时期。

Accordingly , it can be concluded that the Middle Paleozoic is a very important period in the evolution of South Qinling belt , the South China block , as well as Gondwana .

是一个典型的代表广州市华南中国板块等等。

Is a typical representative of the Guangzhou South China plate and so on .

华南、华北板块古生物特征与演化

Characteristics and evolution of fossils in South China and North China plates

华南二叠系形成于基底构造不均一的陆表海盆地，古特提斯海的演化控制着华南板块上二叠纪的构造格局及沉积、聚煤作用。

Permian System of Southern China formed in the epicontinental basin which there are unhomogeneous basal structure . On the Southern China plate , the permian structural frame and sedimentation and coal - accumulation , were controlled by evolution of Tethys sea .