SURFACE GEOCHEMISTRY OF SOIL IN THE DEERBUER PbZn DEPOSIT
WANG Ge 1,2,SUN Zhongjun 3,WU Ronggao 4,YANG Shaoping 3,KONG Mu 3,LIU Huazhong 3
1.School of Earth Science and Resources, China University of Geosciences, Beijing100083, China; 2.Inner Mongolia Bureau of Geology and Mineral Resources Exploitation; Hohhot010020, China; 3.Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang065000, China; 4.No. 2 Geophysical Exploration Party, Shaanxi Bureau of Geology and Mineral Resources, Xi'an710016, China
The Deerbuer PbZn deposit is located in a forest and swamp area. Element geochemistry of soil in the low temperature and rich organic matter environment was studied. It is shown that element geochemistry is influenced by rock, soil granularity, ironmanganese oxides, organic matter and acid precipitation, and that modes of occurrence of elements in eluvial and humus layers are mainly ironmanganese oxides which play a significant role in element enrichment. The adsorption of organic matter is affected by soil granularity, horizon, and organic matter content.
王戈, 孙忠军, 吴荣高, 杨少平, 孔牧, 刘华忠. 得耳布尔铅锌矿土壤表生地球化学特征[J]. 物探与化探, 2010, 34(1): 30-31.
WANG Ge, SUN Zhong-Jun, WU Rong-Gao, YANG Shao-Ping, KONG Mu, LIU Hua-Zhong. SURFACE GEOCHEMISTRY OF SOIL IN THE DEERBUER PbZn DEPOSIT. Geophysical and Geochemical Exploration, 2010, 34(1): 30-31.