【摘 要】
:
The Central part of the North China Craton known as the Trans North China Orogen (TNCO) divides the North China Craton (NCC) into two tectonic domains:the Eastern and Western Blocks.The TNCO preserves
【机 构】
:
School of Earth Sciences and Resources,China University of Geosciences Beijing,29 Xueyuan Road,Beiji
【出 处】
:
The International Conference on Continental Dynamics(2014年大陆
论文部分内容阅读
The Central part of the North China Craton known as the Trans North China Orogen (TNCO) divides the North China Craton (NCC) into two tectonic domains:the Eastern and Western Blocks.The TNCO preserves the record of crustal evolution,cratonization,and magmatism- metamorphism-deformation,and offers a classic region to evaluate subduction-collision tectonics during late Neoarchean through Paleoproterozoic.The region also witnessed major Mesozoic magmatism,lithospheric thinning and metallogeny.
其他文献
Hailaer Basin is a Mesozoic faulted-depression basin which undergoes three periods of superimposition and reformation.The basin can be divided into extending faulted-depression in the bottom,strike-sl
The Qinling Orogenic Belt marks the irregular suture between the North China Craton (NCC) and the Yangtze Craton.Traditionally,the Orogenic Belt is subdivided into the south and north belts by the Sha
The Xitieshan volcanogenic massive sulfide (VMS) deposit (64 Mt of 12.96 %Zn,1.53 %Pb,1.41 %Cu,359.1 g/t Ag,1.81 g/t Au)(Hou and Cook,2009;Sun,1992) is one of the biggest base metal deposits China.Thi
1 Introduction Shuangwang gold deposit,located at in the Devonian strata at the northwing of the anticline,is located at the Wangjialeng the sub-basin of the Late Paleozoic pull-apart basin in the Fen
Tarim basin is the biggest and complex oil-bearing superimposed basin in China,which is surrounded by Tianshan-Beishan,West Kunlun and Altun mountain belts respectively to the north,south,and southeas
The Qinling Orogen that is located between the North China Craton (NCC) and the Yangtze Craton (YZC) underwent multi-stage tectonic evolutions and consists mainly of the North Qinling Belt (NQB) and t
As one of the most famous orogen of China,Qinling orogen has long been regarded as an important boundary dividing the North and South China.After two ophiolite mélange zones were recognized in the lat
The Qinling-Dabie-Sulu orogen was formed by the joining of the North and South China blocks,but the exact timing of the closure of the Paleo-Tethys ocean is still a matter of debate.Along with the con
1.Introduction The Yangyang deposit is one of the biggest iron deposits in the Republic of Korea which produced up to 8 million metric tons of iron ore with an average of 60 wt.%Fe.The Yangyang deposi
The formation and destruction of continental crust involve processes that are directly associated with plate tectonics.However,when plate tectonics started on Earth and whether it operated like modern