2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向
裂带地震构造图 Fig.
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向
裂带地震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热区,区内火山岩浆地热活动强烈,水热显示形式多样,有温
、热
、沸
、水热蚀变岩
、
(硅
、盐
、钙
和硫
)等。
声明:以上例句、词性分类均由互联网资源自动成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪
西向新生破裂带地震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要
东—
东—
东东向,接近
平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热区,区内火山岩浆地热活动
,
热显示形式多样,有温泉、热泉、沸泉、
热蚀变岩石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪
西向新生破裂带
震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要为
—
—
向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的
热区,区内火山
热活动强烈,水热显示形式多样,有温泉、热泉、沸泉、水热蚀变
石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新生破裂带地震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热区,区内火山岩浆地热活动强烈,水热显示形式多样,有温泉、热泉、沸泉、水热蚀变岩石、泉华(硅华、盐华、钙华和硫华)
。
:以上
、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新生破裂带地震
图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山
应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热
,
内火山岩浆地热活动强烈,水热显示形式
,有温泉、热泉、沸泉、水热蚀变岩石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新生破裂
构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的
区,区内火山岩浆
活动强烈,水
显示形式多样,有温泉、
泉、沸泉、水
岩石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新
带地震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热区,区内火山
浆地热活动强烈,水热显示形式多样,有温
、热
、沸
、水热蚀变
、
华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新生破裂带地震
造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火
造应力场主要为北北东—北东—北东东向,接近水平的压应力场。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热
,
内火
岩浆地热活动强烈,水热显示形式多
,有
泉、热泉、沸泉、水热蚀变岩石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西向新生破裂带地震构造图 Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
腾火山区构造
主要为北北东—北东—北东东向,接近水平的压
。
It is inferred from the thermometry of geyserite and adarce inclusions that underground temperatures for the hot spring system in Tengchong are .
云南腾是中外著名的地热区,区内火山岩浆地热活动强烈,水热显
多样,有温泉、热泉、沸泉、水热蚀变岩石、泉华(硅华、盐华、钙华和硫华)等。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。