| 时永明,崔彬,贾维林.黑龙江省铁力市鹿鸣钼矿床地质特征[J].地质与勘探,2007,(2):19-22 |
| 黑龙江省铁力市鹿鸣钼矿床地质特征 |
| GEOLOGICAL FEATURES OF LUMING MOLYBDENUM DEPOSIT AT TIELI IN THE HEILONGJIANG PROVINCES |
| 修订日期：2006-02-15 |
| DOI： |
| 中文关键词: 地质特征 矿床成因 斑岩型 鹿鸣钼矿床 |
| 英文关键词: geological feature, ore genesis, porphyry type deposit, Luming Mo deposit |
| 基金项目:黑龙江省伊春-延寿地区铅锌多金属矿评价项目 |
| 时永明 崔彬 贾维林 |
| [1]中国地质大学,北京100083 [2]黑龙江省矿业集团有限责任公司,哈尔滨150036 [3]黑龙江省第五地质勘察院．黑河164300,哈尔滨150036 |
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| 中文摘要: |
| 鹿鸣钼矿床位于小兴安岭-张广才岭多金属成矿带内,矿体产在印支期二长花岗岩体中,矿床的围岩蚀变、元素地球化学特征、含矿岩体的岩石学特征等均具有斑岩型矿床的特点,且与国内同类型矿床具有可比性. |
| 英文摘要: |
| Luming Mo deposit occurs within the Xiaoxing'anlingZhangguancailing polymetallic mineralizing belt.Ore bodies are located in an Indosinian monzogranite intrusion.Wall-rock alteration and trace element geochemistry of the deposit as well as the petrology of the ore-bearing intrusion all demonstrate features of porphyry type deposit,and can be compared with the same type of deposits in China. |
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