1) Tengchong Rehai volcanic geothermal region
腾冲热海火山地热区
1.
Violent hydrothermal explosions had occurred in the Tengchong Rehai volcanic geothermal region in history.
腾冲热海火山地热区历史上曾发生过强烈的水热爆炸活动,但前期一度沉寂。
2) area of Tengchong volcano
腾冲火山地区
1.
Valuable seismic recordings acquired and establishment of network for recording microshocks in the area of Tengchong volcano have been summarized in this paper, which include system property of the observation, network layout, and seismic recordings.
本文综述了腾冲火山地区微震观测台网的建立与所取得的具有研究价值的地震记录。
3) Tengchong Rehai
腾冲热海
1.
Isolation and identification of seven thermophilic and anaerobic bacteria from Hot Springs in Tengchong Rehai
腾冲热海七株高温厌氧菌的分离及鉴定
4) Tengchong volcano area
腾冲火山区
1.
The source mechanism of the three earthquakes occurred in Tengchong volcano area is determined by this method.
采用 F- K方法得到了发生在腾冲火山区的 3个地震的震源机制 ,结果表明地震 1和地震 2是走滑断裂 ,地震 3是逆断层。
2.
Through focal mechanism analyses of mid small earthquakes occurred in Tengchong volcano areas, the spatial distribution of tectonic stress field, focal types and fracture types have been studied.
通过对腾冲火山区强震和中小地震震源机制解分析 ,对火山区构造应力场方向空间分布 ,以及震源类型和破裂特征作了研究。
5) Tengchong volcanic area
腾冲火山区
1.
A temporary seismic monitoring network composed of 15 mobile digital seismographs was set up in the Tengchong volcanic area in June-Sept.
2002年6～9月,一个由15台流动数字地震仪组成的布设在腾冲火山区的临时地震监测台网,记录到了16个发生在近代火山活动十分活跃的马鞍山火山至热海地区内的小震。
2.
This paper introduces the results of micro-earthquake observation by digital mobile seismic observation network disposed in Tengchong volcanic area during the period from June 6 to September 13, 2002.
20 0 2年 6月 13日至 9月 13日腾冲火山区流动数字化地震台网记录了腾冲火山区及周边地区的 2 92次地震事件。
3.
The tomographic result shows that there is a P wave low velocity zone (LVZ) in the upper crust beneath the Tengchong volcanic area.
根据 1 999年腾冲火山区人工地震探测资料 ,用层析成像方法反演了腾冲火山区上地壳三维 P波速度结构 。
6) Tengchong volcano
腾冲火山区
1.
D pattern of velocity structure in crust and upper mantle at different depths in Tengchong volcano areas and nearby has been reconstructed by chromatography that from data of several thousand earthquakes recorded at 30 stations, which happened in 1984-1998.
结果给出 ,在腾冲火山区下面地壳内约 3～ 9km存在低速带 ,扰动量达 - 10 % ;10～ 15km深度为高波速带 ,扰动量达 7 3% ;16～2 4km深度为低波速带。
2.
The seismic parameters around Tengchong volcano areas and nearby have been measured by digital data.
利用数字化地震记录资料 ,测定了腾冲火山及其周围地区的地震基本参数 ,结果表明 ,腾冲火山区内的地震活动以微震为主 ,震级多数在 1～ 2 5级之间 ,且地震活动频度低 ;而周围地区的构造地震活动频繁 ,且强度大。
补充资料：腾冲热海
腾冲热海位于腾冲县城西南20公里处，面积约为 9平方公里，较大的气泉、温泉群共有80余处，其中10个温泉群的水温达90℃以上，到处都可以看到热泉在呼呼喷涌。世界上有温泉的地方很多，但像腾冲热海这样面积之广、泉眼之多实属罕见。
热海中最典型的是“大滚锅”。它的直径3米多，水深1.5米，水温达97℃，昼夜翻滚沸腾，四季热气蒸腾。在澡塘河，有一个地质断裂带和一条大河交叉形成一个飞泻轰鸣的瀑布，下面有十几处热泉、汽泉昼夜喷薄而出，水汽交融，蒸腾弥漫，如烟如雾。现在热海建有多家疗养院、浴室，并建起了一些娱乐设施，前来旅游、治疗者每日不断。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条