全球性海平面变化;
It is supposed that tectonic subsidence, eustatic change of sea level and sediment supply rate are the controlling factors of sequence development in marine basins.
海相层序地层学中主要强调了构造沉降、海平面变化及物源补给因素对层序发育的控制作用。
Superposition between the basin basement flexure under load and eustatic change of sea level or subsidence due to compaction with different way should produce various types of tectono-depositional episode. There are also some backland basins and relict back-are basins associated with foreland basins during the Late Triassic.
盆地基底荷载挠曲变形与海平面升降或压实沉降过程以不同方式叠加,产生各种类型的构造沉积幕,与前陆盆地共生的还有后陆盆地和残留的弧后盆地。
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