New Zircon U-Pb Age of Granodiorite in Chifeng at the Northern Margin of North China Craton and Constraints on Plate Tectonic Evolution

作     者：CHEN Jingsheng LI Bin YANG Hao LIU Miao YANG Fan LI Wei WANG Yan CUI Tianri 

作者机构：Shenyang Geological Survey Center of China Geological Survey Shenyang 110034 Liaoning China College of Earth Sciences Jilin University Changehun 130061 Jilin China 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2018年第92卷第1期

页      面：410-413页

核心收录：

学科分类：07[理学] 

基　　金：financially supported by the China Geological Survey(grants No.DD20160048-05 12120113053400 and 12120114055501) 

主　　题：New Zircon U-Pb Age Granodiorite Plate Tectonic Evolution 

摘      要：Objective The North China Craton （NCC） is one of the oldest cratons in the world. The accretionary belt at its northern margin has been the focus of scholars both at home and abroad （Zhu Junbing and Ren Jishun, 2017）. In recent years, a series of Late Paleozoic-Mesozoic intrusions trending E-W have been discovered within the northern margin of the NCC, forming a magmatic belt. The study on the origin and tectonic setting of this magmatic belt not only has important significance for understanding the Late Paleozoic-Mesozoic tectonic evolution history of the northern margin of the NCC, but also can provide key constraints on the evolution of its surrounding Xing＇an- Mongolia orogenic belt and the Paleo-Asian Ocean. At present, no Devonian to early stage of Early Carboniferous intrusion has been reported within the northern margin of the NCC.