| 华北地台花岗岩和地层中金含量与金成矿的关系 |
| |
| 引用本文： | 胡受奚,徐金方.华北地台花岗岩和地层中金含量与金成矿的关系[J].高校地质学报,1998,4(2):121-126. |
| |
| 作者姓名： | 胡受奚 徐金方 |
| |
| 作者单位： | [1]南京大学地球科学系 [2]山东省地质矿产局 |
| |
| 摘 要： | 华北地台的热液金矿床经常产于绿岩带中的花风岩内外接触带和变质岩中，因而许多人认为花岗岩和地层就是金矿床的矿源层和矿源岩。显然，他们瓣假设是建筑在这些岩石金的含量高于地壳、上地壳和区域背景含量上的，这样，这些花岗岩和地层可提供足够的金来形成金矿床，因而，这些地层和花岗夺被称为矿源层或矿源岩。随着金定量分析方法的改进和精度的提高 0.1×10^-9，大量测试资料表明，绿岩带中的变质岩和地层中金的丰度常较低，平均1.06×10^-9～2.3×10^-9，而与金矿有关的花岗岩金的含量更低，平均为0.6×10^-9～1．4×10^-9。并且随着花岗岩化和混合岩化程度增加而降低。因此，矿源层和矿源岩并不是前人所认为的那样，花岗岩形成过程和早期深部的成矿流体的碱交代作用过程是促使金活化转移的重要机制，也是形成金矿的主导因素。
|
| 关 键 词： | 花岗岩 矿源层 地层 金矿床 活化转移 成矿 |
| 收稿时间： | 1998-06-20 |
| 修稿时间： | 1998-06-20 |
RELATIONS OF GOLD ABUNDANCE IN THE GRANITES AND STRATA TO GENESIS OF GOLD DEPOSITS |
| |
| Hu Shou-xi,Chen Fu-jing,Xu Jin-fang,Guo Kang-heng,Li Shi-mei.RELATIONS OF GOLD ABUNDANCE IN THE GRANITES AND STRATA TO GENESIS OF GOLD DEPOSITS[J].Geological Journal of China Universities,1998,4(2):121-126. |
| |
| Authors: | Hu Shou-xi Chen Fu-jing Xu Jin-fang Guo Kang-heng Li Shi-mei |
| |
| Institution: | 1. Department Earth Sciences，Nanjing University，Nanfing 210093; 2. Bureau of Geology and Mineral Resources, Shandong Province; 3. Geological Survey Team No.1, Bureau of Geology and Mineral Resources, Henan Province |
| |
| Abstract: | The hydrothermal deposits of gold in North China Platform are commonly associated with granites and metamorphic rocks or strata in the greenstone belts, which are thought to be the source of gold by many geologists. Their hypotheses are founded on the higher abundance levels of gold in these rocks or strata celled as source rocks end source beds to support their theories that the gold was derived from these granites or strata to form deposits.
Owing to the improvement of quantitative measuring method, many analytical data for gold with reasonable accuracy (0.1×10-9)accumulated. It shows that the gold abundance in the metamorphic rocks or strata is rather low, (1.06～ 2.3× 10-9 in average), and in the relevant granites is only 0.6～ 1.4×10-9 in average.
The gold content decreases with increasing granitization and migmatization or amount of fe1sic minerals. This shows that the source rocks or source beds are ambiguous and nonspecific. The granite-formation end alkali-metasomatism are the main mechenism for mobilization of gold which leads to formation of gold deposits. |
| |
| Keywords: | granite source bed gold deposit mobilization |
| 本文献已被 CNKI 维普 等数据库收录！ |
| 点击此处可从《高校地质学报》浏览原始摘要信息 |
| 点击此处可从《高校地质学报》下载免费的PDF全文 |
