Geochemical Characteristics and Prospecting Direction of the Hongwei-Xiongguan-Songheyi Dongshan Area in the Greater Xing'an Mountains, Heilongjiang Province
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摘要
The Daxinganling area collided during the Late Paleozoic. The study area Hongwei-Xiongguan-Songheyi Dongshan area is located at the superimposed transition site of the Paleozoic paleo-Asian tectonic-metallogenic domain and the Mesozoic-Cenozoic Pacific Ocean tectonicmineralization area. It is a good ore-forming fluid channel and has very good ore metallogenic geological conditions. The comprehensive research and metallogenic prediction of the geological background and geochemical characteristics of this area are carried out. It is believed that this area has good prospecting potential,and the prospecting area is circled. Suggestions for further prospecting work in this area are put forward.
The Daxinganling area collided during the Late Paleozoic. The study area Hongwei-Xiongguan-Songheyi Dongshan area is located at the superimposed transition site of the Paleozoic paleo-Asian tectonic-metallogenic domain and the Mesozoic-Cenozoic Pacific Ocean tectonicmineralization area. It is a good ore-forming fluid channel and has very good ore metallogenic geological conditions. The comprehensive research and metallogenic prediction of the geological background and geochemical characteristics of this area are carried out. It is believed that this area has good prospecting potential,and the prospecting area is circled. Suggestions for further prospecting work in this area are put forward.
The Daxinganling area collided during the Late Paleozoic. The study area Hongwei-Xiongguan-Songheyi Dongshan area is located at the superimposed transition site of the Paleozoic paleo-Asian tectonic-metallogenic domain and the Mesozoic-Cenozoic Pacific Ocean tectonicmineralization area. It is a good ore-forming fluid channel and has very good ore metallogenic geological conditions. The comprehensive research and metallogenic prediction of the geological background and geochemical characteristics of this area are carried out. It is believed that this area has good prospecting potential,and the prospecting area is circled. Suggestions for further prospecting work in this area are put forward.
引文
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[2]ZHAO PZ,XIE XJ,CHEN ZZ.Regional geochemical background and metallogenic belt division in the northern segment of the Daxing'anling metallogenic belt[J].Journal of Geology,2014,88(1):99-108．
[3]RUI ZY,SHI LD,FANG RH.Geology of non-ferrous metal deposits in the northern margin of the North China block and adjacent areas[M].Beijing:Geological Publishing House,1994:476．
[4]LIU JM,ZHANG R,ZHANG QZ.Regional metallogenic characteristics of the Greater Xing'an Mountains[J].Geoscience Front,2004,11(1):269-277．
[5]JIA PP,WEI JH,GONG QW,et al.Analysis on the background of ore-forming zone and prospecting prospect of copper-molybdenum deposit in Daxing'anling area[J].Geology and Exploration,2011,47(2):151-162．
[6]SHE HQ,LI HH,LI JW,et al.Metallogenic regularity and prospecting direction of Cu-Pb-Zn-Gold-Silver polymetallic deposit in the middle-north segment of the Greater Xing'an Mountains,Inner Mongolia[J].Journal of Geology,2009,83(10):1456-1472．
[7]SHAO HM,ZHANG FQ.Inner Mongolia Autonomous Region main metallogenic area(band)and metallogenic series[R].Hohhot:Inner Mongolia Autonomous Region Bureau of Geology and Mineral Exploration and Development,2001:42-52．
[8]HAN TC,ZHANG ZF,LV XB,et al.Study on the evaluation method of geochemical anomaly in the middle section of the eastern Tianshan Mountains[J].Geology and exploration,2011,47(5):885-893．
[9]GENG GH.Application of factor analysis in geochemical data processing[J].Geology and Exploration,2014,50(S1):1365-1373．
[10]LIU XY,HUANG ZX,HAO SH,et al.Geochemical characteristics and prospecting direction of Qinjiagou soil in Kulunqi,Inner Mongolia[J].Geology and exploration,2014,50(S1):1338-1343．
[11]LIAO YX,LUO W,TANG PK,et al.Anomaly evaluation and prospecting direction of 1:50,000 water system sediments in Wugang,Guangdong Province[J].Geophysical and Geochemical Exploration,2014,38(1):10-17.