这主要是由于其原始强度较高引起的。

It is due to its' high initialize strength.

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当发射光照到相机的传感器上时，每个像素点抓取一个特定的波长，并对匹配波长的光线进行电子放大。 从仅有几个光子的微弱的原始信号，放大到可见的强度。

That amplifies the original dim signal, composed of just a few photons, until it becomes visible.

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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.

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