In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的地热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、地热梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的地热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、地热梯度、气体成分、同生水盐度等控制着水合带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法不仅适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的地热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底压力、地热梯、气体成分、同生水盐等控制着水合物稳定带基底的深厚。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法不仅适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可成了与断裂有关的地热系统,而浅层天然气可沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底度和压力、地热梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法不仅适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可了与断裂有关的热系统,而浅层天然气可沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、热梯度、气体分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法不仅适于热钻井，而且也可以作为一种新的无套管护壁方法推广应。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

热异常、壳内存在低速层和高导层、强烈震频繁发生等现象说明，这一区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

熔钻进的实践证明，该方法不仅适用于钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

异常、壳内存在低速层和高导层、强烈震频繁发生等现象说明，这一区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的地热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、地热梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的地热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温和压、地热梯、气体成分、同生等控制着合物稳定带基底的深和厚。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践证明，该方法不仅适用于地热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

地热异常、地壳内存在低速层和高导层、强烈地震频繁发生等现象说明，这一地区是现代构造运动的活动区。

In the Shiting River rhombochasm,the geothermal system related to the faults may ha.

石亭江菱断陷中可能成了与断裂有关的热系统,而浅层天然气可能沿断裂泄漏了。

Submarine temperature, pressure, gas compositions, geothermal gradient and syngenetic water salinity control the depth of hydrate zone basement.Autochthonous bacteriogenic mod...

海底温度和压力、热梯度、气体成分、同生水盐度等控制着水合物稳定带基底的深度和厚度。

The practice of subterrene drilling indicates that this method not only adapts to geothermal well, but also is a new pipeless reinforcement method to be applied widely.

热熔钻进的实践，方法不仅适用于热钻井，而且也可以作为一种新的无套管护壁方法推广应用。

The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.

热异常、壳内存在低速层和高导层、强烈震频繁发生等现象说，这一区是现代构造运动的活动区。