盆地流体的驱动机制包括压实驱动、重力驱动和密度(热对流)驱动三种机制,其基本特征及岩石学记录各有不同。
The drive mechanism includes three types: compaction drive, gravity drive and density (heat convection) drive. Their foundational features and lithological information are very different.
影响构造微裂缝发育的因素是:所处的构造应力部位,岩石成分成熟度、粒度、压实程度和早期填隙物含量。
The factors which influence the microfractures are the structural position, compositional maturity, grain size, the quantity of cements as well as specific compaction.
通过试验得出松散岩块在压实过程中,侧向压力随岩石块度及岩石强度的变化规律。
An experiment was arranged to detect how the lateral pressure changes as the lumpiness and strength of rock block vary during compacting.
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