Mesozoic tectono-magmatic evolution of the Tanlu Fault zone and its relationship with the destruction of the North China Craton

Author:

Kang Yuelan12,Shi Yuruo23,Anderson J. Lawford4,Yang Tianshui5,Zhang Haijun5

Affiliation:

1. National Natural History Museum of China, Beijing, China

2. Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China

3. Key Laboratory of Gold Mineralization Processes and Resource Utilization, MNR, Shandong Provincial Key Laboratory of Metallogenic Geological Process and Resource Utilization, Ji’nan, China

4. Department of Earth and Environment, Boston University, Boston, MA, USA

5. School of Earth Sciences and Resources, China University of Geosciences, Beijing, China

Publisher

Informa UK Limited

Subject

Geology

Reference219 articles.

1. Across-arc versus along-arc Sr-Nd-Pb isotope variations in the Ecuadorian volcanic arc

2. Evolution of the lithospheric mantle beneath the southeastern North China Craton: Constraints from mafic dikes in the Jiaobei terrain

3. Zircon U-Pb age and geochemistry of Mesozoic intermediate and felsic volcanic rocks from the Shandong segment (Jiaodong area) of the Tan-Lu fault;Cao G.Y.;Acta Petrologica Et Mineralogica,2014

4. Seismic evidence for significant lateral variations in lithospheric thickness beneath the central and western North China Craton

5. Temporal-spatial changes of tectonic subsidence for Cretaceous-Paleogene basins in the eastern North China Craton and their relations with the craton destruction;Chen Y.;Chinese Journal of Geology,2009

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