Depositional Patterns and Tectonic Setting 青藏东北缘早第三纪盆地充填的沉积型式及构造背景以囊谦和下拉秀盆地为例
On the basis of macro depositional setting, micro sedimentary features and evolution regularity of sedimentary facies, sedimentary patterns of the research area have been established.
在综合考虑宏观沉积背景及微观沉积特征的基础上，根据沉积相的演化规律，建立了研究区沉积模式。
And the seismic sections corresponding to different depositional facies zones may present different characteristics of seismic phase, i. e. different patterns of seismic phase.
地震剖面上对应于不同沉积相带可能呈现出不同的地震相特征，即不同的地震相模式。
The difference of depositional supply of near thrust belt and far thrust belt made the depositional filling and stacking patterns of parasequences different.
逆冲带近端、远端与盆地中部沉积物源供给不同，决定了盆地内不同部位的层序发育样式和准层序的叠置形式不同。
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