The formation of anomalouslow pressure resulted in uplift and denudation of strata and migration of fluid flow.
异常低压则主要归因于地层的抬升剥蚀和流体的运移。
2
Anomalous forcing is introduced into the model, representing the tropical low-frequency dipole convective pattern.
模式中引入了代表热带低频偶极型对流的异常强迫。
3
The analyzed results showed the relative anomaly at later stage is positive and negative at earlier stage for low resistivity zone and anomalous characters of high resistivity zone are opposite.