There are four basic principles in high-resolution sequence stratigraphy, which are base level change, substance conservation, volumetric partition, facies differentiation.
高分辨率层序地层学有四大基本原理，即基准面变化原理、物质守恒原理、沉积物体积分配原理和相分异原理。
These seismic facies show differentiation in horizontal distribution and are successive and evolutionary vertically.
各种地震相平面分布具有差异性、纵向上具有继承性和演化性。
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