地震沉积学的内涵与外延

Seismic Sedimentology of Connotation and Denotation

从地震沉积学的产生至今,它已成为继地震地层学、层序地层学之后的1门新兴边缘交叉学科。提出地震岩石学、地震储层学和地震地貌学构成了地震沉积学的三大核心内容。叙述了在沉积学理论指导下,利用地球物理技术揭示岩相、储层和沉积体系的展布形态及其内部结构,进而实现对有利区带预测的研究思路。指出,它比地震地层学和层序地层学的研究更加精细和准确。

Seismic sedimentology from the production date,it has become the seismic stratigraphy,sequence stratigraphy after a new edge of the cross-disciplinary.Proposed seismic lithology,seismic geomorphology and seismic reservoir study of seismic sedimentology constitute the three cores content.Described in the deposition under the guidance of theory,the use of geophysical techniques to reveal facies and depositional systems reservoir spread morphology and internal structure,thus achieving a favorable zone for the prediction of research ideas.That it is more than seismic stratigraphy and sequence stratigraphy of the study is more precise and accurate.