scholarly journals Morphology and features of Cambrian oncoids and responses to palaeogeography of the North China Platform

2020 ◽  
Vol 9 (1) ◽  
Author(s):  
En-Zhao Xiao ◽  
Ming-Xiang Mei ◽  
Shu Jiang ◽  
Tehseen Zafar
Keyword(s):  
North China ◽  
North China Platform ◽  
The North

The Upper Mantle Flow Beneath the North China Platform

1996 ◽  
pp. 649-659
Author(s):  
Rong-Shan Fu ◽  
Jian-Hua Huang ◽  
Zhe-Xun Wei
Keyword(s):  
Upper Mantle ◽  
North China ◽  
Mantle Flow ◽  
North China Platform ◽  
The North

The petrochemistry of the Lower Proterozoic metamorphic rocks from the Dabieshan-Lianyungang area, the southeastern margin of the North China Platform

1991 ◽  
Vol 55 (379) ◽  
pp. 263-276 ◽  
Author(s):  
Sang Longkang
Keyword(s):  
Continental Margin ◽  
North China ◽  
Active Continental Margin ◽  
The South ◽  
North China Platform ◽  
The North ◽  
Lower Proterozoic ◽  
Southeastern Margin ◽  
Tectonic Settings ◽  
North China Plate

AbstractBased on geological studies, 141 rock analyses and 5 trace element analyses of metabasites, the present paper deals with the rock association, chemical features, protolith formation and the original tectonic settings upwards through the Lower Proterozoic metamorphic strata in the Dabieshan-Lianyungang area, in the south-east of the North China Platform. The results of the study indicate that the lower and middle parts of the metamorphic strata comprise terrigenous clastics, phosphoritic and aluminous sedimentary formations which formed under stable continental margin conditions. In the middle-upper part a calc-alkaline volcano-sedimentary formation under the active continental margin was developed. The Lower Proterozoic meta-strata of sedimentary-volcanosedimentary origin from bottom upwards suggest that the tectonic evolution of the south-eastern margin of the North China Platform is a process from stabilization to mobilization. This process suggests a northward subduction of the Yangtze Plate under the North China Plate during the later part of the early Proterozoic.

Geophysical Features and Perspectives for Metallic Mineral Deposits along the North Edge of the North China Platform

2002 ◽  
Vol 45 (2) ◽  
pp. 232-246
Author(s):  
Wei-Wei JIANG ◽  
Zhi-Ning GUAN ◽  
Tian-Yao HAO ◽  
Lin-Ping HUANG
Keyword(s):  
North China ◽  
Mineral Deposits ◽  
North China Platform ◽  
The North ◽  
Metallic Mineral ◽  
North Edge ◽  
Geophysical Features

Interference fold patterns of the early Precambrian Rock Groups in the Songshan area, China

1982 ◽  
Vol 119 (5) ◽  
pp. 433-461 ◽  
Author(s):  
Shutian Suo ◽  
Ruqi Liu ◽  
Xingyuan Ma
Keyword(s):  
Large Scale ◽  
North China ◽  
Small Scale ◽  
Deformation History ◽  
North China Platform ◽  
Early Proterozoic ◽  
The North ◽  
Regional Deformation ◽  
History Of ◽  
Insight Into

SummaryThe Songshan area is located in the southern part of the North China platform, which is one of the most completely cratonized tectonic units of China. Its basement has experienced a complex evolutionary history and was eventually consolidated at the end of early Proterozoic time about 1.7 Ga ago.A systematic study has been made of the deformation history of the lower Proterozoic Songshan Group and the Archean Dengfeng Group. At least two widespread episodes of deformation can be recognised in the early Proterozoic Zhongyue tectonic cycle and three in the Archean Songyang cycle. Large scale and small scale interference patterns of the superimposed folding are investigated with the aim of recognizing possible regularities in their occurrence and of gaining an insight into the regional deformation history. Two important aspects of superimposition relationships are illustrated: the control of earlier structures upon later ones and the reform of the former by thelatter; their geometrical regularities are also dealt with respectively.

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