为了保持原始地震记录的相对强度，可以稳定的海底反射波作参考层，估算目的层的补偿值。
In order to preserve the relative intensity in - formation in raw seismic data, we can consider the sea-bottom reflection as reference layer to estimate the compensation value of target stratum.
相同的方法签名出现在每个参考架构层的不同服务上。
The same method signatures appear on different services residing within each of the reference architecture layers.
自动化活动与SOA参考体系结构中的服务层对应。
Automated activities correspond to the services layer in the SOA reference architecture.
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