| 李峰,张富良.滇西大平掌铜多金属矿床火山喷流沉积原因[J].地质与勘探,2001,(4):5-8 |
| 滇西大平掌铜多金属矿床火山喷流沉积原因 |
| VOLCANIC-EXHALATIVE-SEDIMENTARY GENESIS OF DAPINGZHANG CU-POLYMETAL DEPOSIT, WESTERN YUNNAN |
| 修订日期：2000-05-18 |
| DOI： |
| 中文关键词: 喷流沉积型矿床 矿床结构 成因 铜多金属矿床 成矿地质 金属元素 流体包裹体 |
| 英文关键词: Dapingzhang in western Yunnan,volcanic-exhalative-sedimentary deposit,mineralization texture,genesis |
| 基金项目: |
| 李峰 张富良 |
| [1]昆明理工大学，昆明650093 [2]云南地勘局第五地质大队，思茅665000 |
| 摘要点击次数: 2585 |
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| 中文摘要: |
| 大平掌矿床由上部层状块状硫化物矿体和下部细脉浸染状矿体组成，双层结构清楚。块状矿体中发育典型的草莓状和鲕状硫化物。成矿地质背景和矿石中的金属元素及REE配分形式、S同位素组成、流体包裹体特征等均与黑矿型矿床及现代海底热液活动区硫化物矿床相似。矿床典型的火山喷流沉积成因。 |
| 英文摘要: |
| There was a typical "two-layer structure" in Dapingzhang Cu-polymetal deposit, which was composed of the upper massive sulfide orebody and lower veinlet-disseminated sulfide orebody. Sulfides with framboidal and oolitic texture have been found from massive sulfide ore. The deposit is similar in geological setting, distribution patterns of metal elements and REE, sulfur isotopic composition, and fluid inclusion characteristics to the Kuroko-type deposit and modern sulfide deposits in some sea-floor hydrothermal activity regions. Based on the above evidences, it is suggested that metallogenesis was related to volcanic-exhalative-sedimentation. |
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