|
|||||
|
|
| 长白山天池火山主断裂活动与热液蚀变带 | |
| 引用本文： | 刘明军,顾梦林,孙振国,魏海泉,金伯禄.长白山天池火山主断裂活动与热液蚀变带[J].中国地震,2004,20(1):64-72. |
| 作者姓名： | 刘明军 顾梦林 孙振国 魏海泉 金伯禄 |
| 作者单位： | 1. 中国地震局地球物理勘探中心,郑州市文化路104号,450002 2. 中国地震局地质研究所,北京市德外祁家豁子,100029 3. 吉林省地质矿产局第六地质调查所,延吉,133001 |
| 基金项目： | 科技部“十五”攻关计划“吉林东部活动火山灾害预测研究”课题，中国地震局地球物理勘探中心论著号 :RCEG2 0 0 2 16 |
| 摘 要： | 在野外考察中发现，天池破火山口内壁同一层位不同段的近水平向红褐色、砖红色热液蚀变带顶界面有明显高差热液蚀变顶界面，北段(靠近天文峰)比南段(朝鲜境内靠近将军峰)高出约110m。热液蚀变带顶界面可作为判断构造运动的标志面。北段与南段顶界面的高差，反映了自热液蚀变以来，天池火山北东向主断裂六道沟-天池-甑峰山断裂北西盘的抬升幅度大于南东盘，这可能是天池北西部较南东部地形坡度更陡、水系更发育的内在原因。北西向主断裂——白山镇-天池-金策断裂北东盘的抬升幅度大于南西盘。由热液蚀变和古风化壳特征观察到的北东向主断裂的近期垂向活动速率大于北西向主断裂的活动速率。这两条在天池交叉的主断裂将天池火山切割成4个块体，它们的抬升幅度从大到小依次为北、西、东、南块体。北块体抬升幅度最大，这与深地震测深、大地电磁探测等得出的天池北部岩浆囊较浅的结果有较好的对应关系和一定的成因联系。 |
| 关 键 词： | 天池火山 主断裂 破火山口内壁 热液蚀变 差异抬升 |
| 文章编号： | 1001-4683(2004)01-064-09 |
Activity of Main Faults and Hydrothermal Alteration Zone at the Tianchi Volcano, Chabgbaishan |
|
| Liu Mingjun,Gu Menglin,Sun Zhenguo,Wei Haiquan,Jin Bolu.Activity of Main Faults and Hydrothermal Alteration Zone at the Tianchi Volcano, Chabgbaishan[J].Earthquake Research in China,2004,20(1):64-72. | |
| Authors: | Liu Mingjun Gu Menglin Sun Zhenguo Wei Haiquan Jin Bolu |
| Institution: | Liu Mingjun 1) Gu Menglin 1) Sun Zhenguo 1) Wei Haiquan 2) Jin Bolu 3) 1) |
| Abstract: | It is discovered in a field survey that the elevation of nearly horizontal top planes of brown and red hydrothermal alteration zones are varied obviously at different segments on the same layer of caldera wall, and that the elevation at the northern segment next to the Tianwen Peak is about 110 m higher than one at the southern segment next to the Jiangjun Peak in Korea. The authors show here that the top plane of hydrothermal alteration zone can be treated as a mark to assess tectonic activity. The elevation difference of the top planes of hydrothermal alteration in the two segments shows that, from generation of hydrothermal alteration up to now, the total uplift height in the NW block is bigger than in the SE block along the main fault in NE trend, the Liudaogou-Tianchi-Zenfengshan fault that passes between the two segments. It also explained why the topography in the northwestern side of Tianchi is steeper and with more river channels than in the southeastern side of Tianchi. The uplift height in the NE block is bigger than in the SW block along the main fault in NW trend,the Baishanzhen-Tianchi-Jince fault. It seems that the recent activity rate of the main fault in NE trend is bigger than that of the main fault with NW trend by observing hydrothermal alteration and paleosoil. The two main faults that cross at Tianchi cut the Tianchi volcano into 4 blocks, that is, north block, west block, east block and south block in order of successively decreasing of uplift value respectively. The uplift value of north block that is obtained by analyzing elevation difference of top planes of hydrothermal alteration is the biggest. Deep seismic sounding and magnetotelluric survey show that there are low velocity and low resistivity bodies that may be shallower magma chambers in the north part of Tianchi. All of these results are in consistent with each other and there may be some connections of causes. |
| Keywords: | Tianchi volcano Main fault Caldera inner wall Hydrothermal alteration Different uplift |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |