Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和作用的控制，其对储层的改程度与沉积相带及不整合面的离密切相关。

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，这一地区是现运动的活动区。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和造作用的控制，其对储层的改造程度与沉积相带及不整合面的离密切相关。

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象说明，这一地区是造运动的活动区。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和构造作用的控制，其对储层的改造沉积相带及不整合面的离密切相关。

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。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉和构造作用的控制，其对储层的改造程度与沉及不整合面的离密切关。

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、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。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作受沉积和构造作制，其对储层改造程度与沉积相带及不整合面离密切相关。

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、强频繁发生等现象说明，这一区是现代构造运动活动区。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和构作用的控制，其对储层的度与沉积相带及不整合面的离密切相关。

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，这一地区是现代构运动的活动区。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和构造作用，其对储层改造程度与沉积相带及不整合面离密切相关。

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、震频繁发生等现象说明，这一区是现代构造运动活动区。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和构造作用的控制，其对储层的改造程度与沉积带及面的离密。

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。

Dissolution is controlled by both sedimentation and tectonization, and the converted degree on reservoirs is closely related to sedimentary facies and the distance from unconformity interfaces.

溶解作用受沉积和构造作用的控，储的改造程度与沉积相带及不整合面的离密切相关。

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、地壳内存在低速和高、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。