2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西
破裂带地震构造图 Fig.
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2腾-景洪北西
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
,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
、水热蚀变岩石、
(
、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
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)等。
声明:以上例句、词类均由互联网资源自动生成,部
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.
2
-景洪北西向新生破裂带地震构造
Fig.
The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.
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
(硅
、盐
、钙
)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-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.
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 .
云南是中外著名的地
区,区内
山岩浆地
活动强烈,水
显示形式多样,有温
、
、沸
、水
蚀变岩石、
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
区,区内火山岩
活动强烈,水
显示形式多样,有温泉、
泉、沸泉、水
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。
2 Seismotectonic map of the Tengchong-Jinghong newly-generated rupture zone.
图2-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.
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)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
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
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)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)等。
声明:以上例句、词类均由互联网资源自动生成,部
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。