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| 山东省胶莱盆地东北缘宋家沟金矿地质特征及其成因初探 | |
| 引用本文： | 李洪奎,杨永波,于志臣,于学峰,倪振平,庞绪贵,李秀章. 山东省胶莱盆地东北缘宋家沟金矿地质特征及其成因初探[J]. 华北地质, 2002, 0(Z1) |
| 作者姓名： | 李洪奎 杨永波 于志臣 于学峰 倪振平 庞绪贵 李秀章 |
| 作者单位： | 山东省地质调查院 济南250013(李洪奎，倪振平，庞绪贵)，山东省第四地质矿产勘查院 维坊261021(杨永波)，山东省第三地质矿产勘查院 烟台264003(于志臣)，山东省地质科学院 济南250013(于学峰)，山东省地质调查院 济南250013(李秀章) |
| 基金项目： | 中国地质调查局“华北地台成矿规律和找矿方向综合研究项目”(编号 :2 0 0 110 2 0 0 0 38) |
| 摘 要： | 山东省宋家沟金矿位于胶莱盆地东北缘 ,产于莱阳群林寺山组断裂破碎带中。牟—即断裂带为切割莱阳群的断裂 ,对金矿起控制作用。早白垩纪晚期的火山—岩浆活动为深部含金热液的运移提供了通道 ,并在其有利的构造部位沉淀成矿。稀土元素特征和氧、硫同位素特征亦说明宋家沟金矿的物质来源以深源为主 (幔源及下地壳中的金 ) ,是早白垩世晚期的火山—岩浆活动作用的结果。 |
| 关 键 词： | 宋家沟金矿 地质特征 早白垩纪晚期 火山—岩浆活动 |
The Geological Characters and the Origin of Songjiagou Ore Deporsit in Jiaolai Basin, Shandong Province,China |
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| LI Hong-Kui, YANG Yong-bo, YU Zhi-chen, YU Xue-feng, NI Zhen-ping, PANG Xu-gui, LI Xiu-zhang. The Geological Characters and the Origin of Songjiagou Ore Deporsit in Jiaolai Basin, Shandong Province,China[J]. Geological Survey and Research, 2002, 0(Z1) | |
| Authors: | LI Hong-Kui YANG Yong-bo YU Zhi-chen YU Xue-feng NI Zhen-ping PANG Xu-gui LI Xiu-zhang |
| Affiliation: | LI Hong-Kui1, YANG Yong-bo2, YU Zhi-chen3, YU Xue-feng4, NI Zhen-ping1, PANG Xu-gui1, LI Xiu-zhang1 |
| Abstract: | Shandong Songjiagou Gold Deposit is loucated in the north-east edge of Jiaolai Basin where the fracture zone of Lisishan Formation, Caiyang Group appears. The ore is controlled by Mu-JI faulted zone which cuts Caiyang Group. The Glod-bearing hydrothermal solution moves up with the activies of early Cretaceous terminalvolcano-magma, and deposits in the favorable places. The lanthanon elements and sulfur and oxygen isotopic feature suggest that the ore materal comes from the deep place of Earth, and is related with the volcanic-magmatic activites in Cretaceous period. |
| Keywords: | Songjiagou gold deposit early Cretaceous late period geological characters materal origin volcanic-magmatic activities Shandong Province China |
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