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Geoscience ›› 2015, Vol. 29 ›› Issue (6): 1371-1376.

• Engineering Geology and Environmental Geology • Previous Articles     Next Articles

Recognization and Interpretation of Pt and Pd Geochemical Anomaly in Stream Sediment in Hongyan Area, Western Guizhou Province, China

ZHANG Jie1, YANG Ke2,3,4, ZHAO Chuan-dong3,4, LIU Ying-han3,4, CHENG Hang-xin3,4   

  1. (1. Hebei Institute of Regional Geology and Mineral Resources Survey, Langfang, Hebei 065000, China; 2. School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China; 3. Institute of Geophysical & Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang, Hebei065000, China; 4. Key Laboratory of Geochemical Cycling of Carbon and Mercury in the Earth’s Critical Zone, Chinese Academy of Geological Sciences, Langfang, Hebei 065000, China)
  • Online:2015-12-24 Published:2016-02-29

Abstract:

Compared with the abundance of Pt and Pd in mafic and ultramafic rocks in China, the Emeishan flood basalts have higher geochemical backgrounds. These results suggest that the recognization of the Pt-Pd geochemical anomalies related mafic intrusive bodies with Pt-Pd minerlization is key technology from the Permian Emeishan flood basalt for exploration. Results from a stream sediment geochemical survey at a sampling density of 4-6 samples per square kilometer show that contrast values, computed Pt and Pd concentrations in stream sediment to those in different rocks, can effectively delineate Pt and Pd geochemical anomalies related mafic intrusive bodies from high geochemical background area. An extensive local geochemical anomalous belt of Pt, Pd, As, Sb, Hg, Cr, Ni and Pb was delineated over the contact area among limestone, basalt and fault of NE direction around Hongyan village using the stream sediment survey at a scale of 1∶50,000. A new concealed maficultramafic intrusive body containing PGE mineralization was predicted.

Key words: geochemical anomaly of Pt-Pd, Emeishan flood basalt rock, mafic and ultramafic rock

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