financially supported by the National Natural Science Foundation of China (Grant No.41203023);National Basic Research Program of China (Grant No.2007CB411301)
The upper Qigeblaq Formation (Fm) dolostones and the Yurtus Fm phosphatic cherts, black shales, limestones, and dolostones are widely distributed in the Precambrian/Cambrian transitional succession of the Aksu-Wushi...
supported by National Natural Science Foundation of China(Grant No.41203023);National Basic Research Program of China(Grant No.2007CB411301)
A chert-phosphorite unit from the Sugetbrak section in the Tarim Basin was analyzed for rare earth elements(Ce,Eu),redox sensitive proxies,and carbon isotopic compositions(??13C carb and??13C org)in the lower Yurtus F...
supported jointly by the National Basic Research Program of China (No. 2007CB411301);Doctoral Fund of Ministry of Education of China (No. 20060284039)
In order to better understand the paleoceanographic sedimentary environment of the Lower Cambrian black shales extensively distributed in South China, outcropped along the present southern margin of the Yangtze Platfo...
supported by National Basic Research Program of China (Grant No. 2007CB411301);the Bureau of China Geological Survey (Grant No. 1212010611806);ISTO
The Chinese Tianshan belt is a major part of the southern Central Asian Orogenic Belt, extending westward to Kyrgyzstan and Kazakhstan. Its Paleozoic tectonic evolution, crucial for understanding the amalgamation of C...