Age and geochemistry of the Naxiguole banded iron formation (BIF), NW China: recurrence of superior-type BIF in the Neoproterozoic-Reference-Cited by-同舟云学术

Age and geochemistry of the Naxiguole banded iron formation (BIF), NW China: recurrence of superior-type BIF in the Neoproterozoic

Author:

Sun Jinlei¹,Qian Ye¹²³,Li Yujin¹,Zhang Peng⁴,Qiao Jianfeng⁵,Shen Yanjie¹,Sun Fengyue¹

Affiliation:

1. College of Earth Sciences, Jilin University, Changchun, PR China

2. Shandong Provincial Engineering Laboratory of Application and Development of Big Data for Deep Gold Exploration, Weihai, PR China

3. Ministry of Nature Resources, Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Changchun, PR China

4. The Third Geological Exploration Institute of Qinghai Province, Xining, PR China

5. The Fifth Geological Exploration Institute of Qinghai Province, Xining, PR China

Funder

the Natural Science Foundation of Jilin Province

Shandong Provincial Engineering Laboratory of Application and Development of Big Data for Deep Gold Exploration

National Natural Science Foundation of China

Science and Technology Project of Department of Education, JilinProvince

Science and Technology Program of Qinghai Province

Self-determined Foundation of Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources

Publisher

Informa UK Limited

Subject

Geology

Link

Reference96 articles.

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