J. Rao

发表

The formation of the world-class Zhuxi scheelite skarn deposit: Implications from the petrogenesis of scheelite-bearing anorthosite

J. Mao, Shiwei Song, Guiqing Xie, 2018, Lithos.

Indicator element selection and geochemical anomaly mapping using recursive feature elimination and random forest methods in the Jingdezhen region of Jiangxi Province, South China

J. Rao, Y. Ouyang, Jianguo Chen, 2020 .

Prospectivity mapping for “Zhuxi-type” copper-tungsten polymetallic deposits in the Jingdezhen region of Jiangxi Province, South China

J. Rao, Y. Ouyang, Jianguo Chen, 2017 .

Partial-melting of fertile metasedimentary rocks controlling the ore formation in the Jiangnan porphyry-skarn tungsten belt, south China: A case study at the giant Zhuxi W-Cu skarn deposit

Yongfeng Zhu, J. Mao, Shiwei Song, 2018 .

In situ LA-ICP-MS U–Pb geochronology and trace element analysis of hydrothermal titanite from the giant Zhuxi W (Cu) skarn deposit, South China

J. Mao, Shiwei Song, Guiqing Xie, 2018, Mineralium Deposita.

Petrogenesis of Scheelite-Bearing Albitite as an Indicator for the Formation of a World-Class Scheelite Skarn Deposit: A Case Study of the Zhuxi Tungsten Deposit

J. Mao, Shiwei Song, Guiqing Xie, 2020 .

Muscovite 40Ar−39Ar age and its geological significance in Zhuxi W(Cu) deposit, northeastern Jiangxi

Zaiyu Yao, Guohua Chen, J. Rao, 2019, Journal of Central South University.

Correction to: Using the catchment-based fractal model to delineate geochemical anomalies associated with Cu-W polymetallic deposits in the Zhuxi, Jiangxi Province

J. Rao, Y. Ouyang, 2018, Arabian Journal of Geosciences.

Using the catchment-based fractal model to delineate geochemical anomalies associated with Cu-W polymetallic deposits in the Zhuxi, Jiangxi Province

J. Rao, Y. Ouyang, 2018, Arabian Journal of Geosciences.

Geochronology and geochemistry of the granites from the Zhuxi W-Cu ore deposit in South China: Implication for petrogenesis, geodynamical setting and mineralization

Xiaofei Pan, Yan Li, Guohua Chen, 2018 .