Earth Science Frontiers ›› 2012, Vol. 19 ›› Issue (3): 84-92.

• Article • Previous Articles     Next Articles

The significance of different scale copper geochemical anomalies and large ore deposit prediction in the middlelower Yangtze River.

  

  1. 1. Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China 2. Key Laboratory of Applied Geochemistry, Chinese Academy of Geological Sciences, Langfang 065000, China
  • Received:2012-04-10 Revised:2012-04-20 Online:2012-05-25 Published:2012-05-25

Abstract:

Based on the 1∶200000 regional geochemical data of copper element as the foundation in the middlelower Yangtze River, the different scales of geochemical anomaly map can be used for different purposes. (1)The 1∶200000 geochemical anomalies can be used for outlining anomalous target area of a deposit and forecasting large deposits. Twelve of 13 large deposits fell in threetier structure of geochemical anomalies in the study area; the correlation coefficient between the ore reserves of known deposits and areal productivity of geochemical anomalies is 0.94; the correlation coefficient of known deposit reserves and geochemical anomalous areas is 0.95, showing a good correlation between the size of ore reserve and the scale of regional geochemical anomalies. (2)The 1∶500000 geochemical anomalies can be used to delineate anomalous target areas of an orefield, to predict the favorable mining area in a metallogenic belt. (3)The 1∶1000000 geochemical anomalies can be used to delineate a large ore district or a metallogenic belt target for ore district prediction. If we consider an area greater than 1000 km2 including three deposits as an ore district, then, there are three large ore districts in the middlelower Yangtze River: Maanshan  Nanjing ore district, Jiujiang  Ruichang  Daye ore district and Dexing  Huangshan Anqing  Tongling ore district (actually containing two Dexing and Tongling ore districts). Large deposits often occurred in the areas with multilayered geochemical anomalies, and the geochemical anomaly in a large ore district has at least a 3 layered structure; there exists a corresponding correlation between the concentration centers and the large deposits. The discovery of these laws provides an important geochemical marker for predicting new large ore district in different mineralization areas.

Key words:  the middlelower Yangtze River, geochemical anomalies, prediction, copper element

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