强制海退沉积作用及其地质意义  

SEDIMENTATION AND GEOLOGIC SIGNIFICANCE OF FORCED REGRESSION

作　　者：沙旭光[1] 刘健[2] 程新民[1] 周良勇[2] 

机构地区：[1]吉林大学地球科学学院,长春130061 [2]青岛海洋地质研究所,青岛266071

出　　处：《海洋地质动态》2006年第11期13-17,共5页Marine Geology Letters

摘　　要：较为全面地回顾了强制海退概念的提出及对传统层序地层学发展的推动作用;结合国内外对强制海退沉积的最新研究进展,探讨了沉积层序体系域四分法的可行性和强制海退体系域的主要沉积特征。The concept of forced regression and its significance for traditional sequence stratigraphy have been generally reviewed by the authors during this study. The feasibility of quartation for system tract and main sedimentary characteristics of forced regression system tract have been discussed, based on the new advances in researches on forced regressive deposits at home and abroad.

关 键 词：层序地层学 强制海退 体系域 海平面变化 第四纪 

分 类 号：P736.21[天文地球—海洋地质]