火山地热

火山地热火山地热
  1. 根据腾冲火山地热区实施的人工地震测深剖面资料,用有限差分反演和正向走时拟合方法确定了地壳二维P波速度结构。

    Based upon the deep seismic sounding profile conducted in the Tengchong volcano-geothermal area , a two-dimensional crustal P velocity structure is obtained by use of the finite-difference inversion and the forward travel-time fitting method .

  2. 腾冲火山地热区地壳具有低P波和S波速度、低电阻率、高热流值和低Q值,以及上地幔也具有低P波速度的特点。

    The crust of Tengchong volcano-geothermal area is characterized by low P-wave and S-wave velocity , low resistivity , high heat-flow value and low Q value . There is also a feature of low P-wave velocity in the upper mantle .

  3. 腾冲火山地热区的微震观测

    Microseismic observation in Tengchong volcano-geothermal region

  4. 腾冲热海是中国最著名的火山地热区,近期区内水热流体活动异常强烈。

    The Rehai area of Tengchong County , Yunnan Province is a well-known volcanic geothermal field in China .

  5. 腾冲火山地热区的水热活动显示强烈,小震微震活动频繁。

    In the Tengchong volcano-geothermal region , there are strong surface expressions of hydro-thermal activities and frequent microseismicity .

  6. 腾冲火山地热国家地质公园旅游开发研究

    Study the Value of Volcanoes and Terrestrial Heat Tengchong National Geological Park and Way of Realizing the Park 's Value

  7. 滇西两河金矿床产于新生代火山温泉地热环境中。

    The deposit formed in the volcano thermal-spring geothermal environments in Cenozoic .

  8. 在恶魔餐厅,肉类、禽类和鱼类都是使用火山的地热烤熟的。

    In El Diablo , the meat , poultry and fish are grilled using the volcano 's geothermal heat .

  9. 地壳上地幔是地球板块运动、海底扩张、地震、火山、地热等活动的主要场所。

    The crust and upper mantle are the main areas where the plate movements , ocean spreading , earthquakes , volcanoes , and geothermal activity occur .

  10. 羊八井热田是属于陆陆碰撞板缘非火山型高温地热田。

    The Yangbajing Geothermal Field is one of non volcanic high temperature geothermal fields .

  11. 因为火山泥是地热蒸汽把其从地下带上,悬浮并沉淀于矿物水池中,因此含有特别丰富的矿物元素。

    The contact the mud has had with volcanic gases and minerals from deep within the earth 's surface is the reason it is particularly rich in minerals .

  12. 塔里木盆地经历了复杂的热演化史,二叠纪的火山活动使地热梯度相对较高,但新生代地热梯度下降很快,现今地热梯度仅约为20℃/km;

    The thermal gradient at Permian had a relative high value because of the volcanic activity . It decreased rapidly at the Neocene to Quaternary . The present day 's thermal gradient is only 20 ℃ / km .

  13. 火山区突发性地热异常热红外传输机理研究

    Research on Transmission Mechanism of Thermal Infrared Remote Sensing for Abrupt Geothermal Anomaly in Volcanic Region

  14. 最后结合已有的地质和物探资料,还给出了长白山天池火山地区长白温泉地热系统的概念性模型。

    Combined with the known geological and geophysical data , the geothermal system structure model of the Changbai hot spring is established .