摘要
本文首先通过追踪对比大量的地震反射资料，在T20－T40层序中确认了L27－1砂体的剖面特征和平面的总体形态，进而从沉积演化与陆坡形成的由表及里分析研究中，最终揭示出它的形成机理，并命名为L27－1水道浊积砂复合体，得出了比较满意的地质解释。
Based on tracing and analysing a great deal of reflection seismic data, the paper shows the characteristics of L27-1 sand in cross section and its figure. Analysing and studying on development of deposition and continental slope forming from outside to inside, the paper point out its forming principle and name it as L27-1 turbidite channel sand complex,which is more satisfactorg interpretation in geology turbidite.
出处
《中国海上油气（地质）》
1997年第4期281-288,共8页
China Offshore Oil and Gas(Geology)
