Zhang Lian-Chan, Lan Cai-Yun, Wang Chang-Le, Peng Zi-Dong, Tong Xiao-Xue, Li Wen-Jun, Dong Zhi-Guo
Changes of oceanic environment before and after the Paleoproterozoic Great Oxidation Event(GOE): Evidence from petrography and geochemistry of banded iron formation(BIF)from the North China Craton
Zhang Ya-Guan, Du Yuan-Sheng, Liu Jian-Zhong, Wang Ze-Peng, Deng Chao
Phosphogenesis of phosphorite from the Sinian Doushantuo Formation in Guizhou Province and its coupling relation with the Neoproterozoic Oxygenation Event
Liu Jian-Zhong, Wang Ze-Peng, Du Yuan-Sheng, Zhang Ya-Guan, Wu Wen-Ming, Chen Guo-Yong, Fu Zhi-Kang, Wan Da-Xue, Wang Da-Fu, Tan Dai-Wei
Enrichment mechanism of phosphorite deposits and significant breakthrough in “Triunity Model”for ore prospecting in the Sinian Doushantuo Formation of eastern Kaiyang region,Guizhou Province
Sheng Hui, Duan Zheng-Ming, Liu Shan-Wei, Zeng Zhe, Feng Jian-Wei
Research advances,geological implication and application in Ordos Basin of the “pore-size controlled precipitation” in diagenesis of carbonate rock reservoir
Bao Zhi-Dong, Ji Han-Cheng, Liang Ting, Wei Ming-Yang, Shi Yan-Qing, Li Zong-Feng, Lu Kai, Xiang Peng-Fei, Zhang Hua, Yan Rui, Guo Yu-Xin, Li Zhuo-Lun, Wan Pu, Yang Zhi-Bo, Ma Xiao-Dong, Liu Rui, Liu Can-Xing, Zhong Xu-lin, Guo Xiao-Qi, Cai Zhong-Xian, Zhang Shui-Chang
Primary dolostones of the Meso-Neoproterozoic:Cases on typical platforms in China
Li Yun, Hu Zuo-Wei, Liu Can, Dong Jie, He Jing, Yuan Xiao-Qi, Wei Yang
Characteristics of authigenic carbonate minerals in carbonate concretions of the Chang 7 oil-bearing interval of Upper Triassic Yanchang Formation in Weibei area, Ordos Basin
Xiong Ying, Wu Kun-Yu, Tan Xiu-Cheng, Zhang Yong-Shu, Yang Bo, Ren Ling, Liu Ling, Liu Yun, Qiao Yan-Ping, Wang Xiao-Fang
Influence of lake-level fluctuation on the mixed saline lacustrine carbonate reservoir: A case study from the Upper Member of Paleogene Lower Ganchaigou Formation in the Yingxi area of Qaidam Basin
Xing Zhi-Feng, Zhou Hu, Lin Jia, Wang Min, Zheng Wei
Evolution of Microbially Induced Sedimentary Structures and their response to palaeoenvironment variation of the Lower Triassic Liujiagou Formation in Yiyang area,Henan Province