安化渣滓溪锑矿床中白钨矿地质特征及控矿因素
工作区位于雪峰弧形构造成矿带中段,出露地层主要为新元古界板溪群五强溪组。矿床产于NE向分布的马家溪和岳溪2条平行断裂所挟持的上升断块内,主要赋存于五强溪组第二段第三层富含火山物质的碎屑岩内。成矿严格受到矿区西侧的NWW向F3断裂制约。所有钨的矿化均产于该断裂上盘。白钨矿主要赋存在凝灰质板岩、凝灰质砂岩及石英砂岩长石石英砂岩、杂砂岩等硬、脆岩石中的节理裂隙中,由于这些节理裂隙发育程度不等,导致矿化极不均匀。白钨矿的主要控矿因素为地层岩性、断裂构造和围岩蚀变等。...
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| Veröffentlicht in: | 低碳世界 2017 (20), p.45-46 |
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| creator | 杨智鹏 |
| description | 工作区位于雪峰弧形构造成矿带中段,出露地层主要为新元古界板溪群五强溪组。矿床产于NE向分布的马家溪和岳溪2条平行断裂所挟持的上升断块内,主要赋存于五强溪组第二段第三层富含火山物质的碎屑岩内。成矿严格受到矿区西侧的NWW向F3断裂制约。所有钨的矿化均产于该断裂上盘。白钨矿主要赋存在凝灰质板岩、凝灰质砂岩及石英砂岩长石石英砂岩、杂砂岩等硬、脆岩石中的节理裂隙中,由于这些节理裂隙发育程度不等,导致矿化极不均匀。白钨矿的主要控矿因素为地层岩性、断裂构造和围岩蚀变等。 |
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| fulltext | fulltext |
| identifier | ISSN: 2095-2066 |
| ispartof | 低碳世界, 2017 (20), p.45-46 |
| issn | 2095-2066 |
| language | chi |
| recordid | cdi_wanfang_journals_dtsj201720031 |
| source | Alma/SFX Local Collection |
| subjects | 地质特征 控矿因素 白钨矿 |
| title | 安化渣滓溪锑矿床中白钨矿地质特征及控矿因素 |
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