New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the Eastern Central Asian Orogenic Belt(NE China)

被引：0

作者：

DU Qingxiang ^{[1
,2
]}

HAN Zuozhen ^{[1
,2
]}

SHEN Xiaoli ^{[1
,2
]}

HAN Chao ^{[1
,2
,3
]}

SONG Zhigang ^{[1
,2
]}

GAO Lihua ^{[1
,2
,3
]}

HAN Mei ^{[1
,2
]}

ZHONG Wenjian ^{[1
,2
]}

YAN Junlei ^{[1
,2
]}

机构：

[1] College of Earth Science and Engineering, Shandong University of Science and Technology

[2] Shandong Provincial Key Lab of Depositional Mineralization and Sedimentary Minerals, Shandong University of Science and Technology

[3] Key Laboratory for Sedimentary Basin and Oil and Gas Resources, Ministry of Land and Resources

来源：

Acta Geologica Sinica(English Edition) | 2017年 / 05期

基金：

中国国家自然科学基金; 高等学校博士学科点专项科研基金;

关键词：

Th; NE China; New Evidence of Detrital Zircon Ages for the Final Closure Time of the Paleo-Asian Ocean in the Eastern Central Asian Orogenic Belt; OHS; NCC; Pb;

D O I：

暂无

中图分类号：

P542.2 []; P597.3 [];

学科分类号：

070902 ; 070904 ;

摘要：

Objective The NE China is located in the eastern segment of the Central Asian Orogenic Belt(CAOB),which is a large accretionary orogen between the Siberian Craton and the North China Craton(NCC).Many researches have discussed about the evolution of the Paleo-Asian Ocean(PAO)in the eastern CAOB.However,the timing of the

引用

页码：1910 / 1914

页数：5