稳定同位素方法可以有效地应用于深水碳酸盐岩的成岩作用研究。
Stable isotopic method can be used effectively in the diagenetic research of deep water carbonate rocks.
早成岩阶段的主要成岩作用是碳酸盐胶结作用以及压实作用引起的颗粒重排；
Main diagenesis of the syndiagenesis is carbonate cementation in the shallow lake sheet sands and rearrangement caused by compaction.
碳酸盐岩储集空间主要受成岩作用制约。
Reservoir space in carbonates is mainly controlled by diagenesis.
碳酸盐岩次生渗透性是成岩作用、构造作用、水动力作用及生物化学作用的综合结果。
The secondary permeability of carbonate rocks is the result of comprehensive process of diagenesis, tectonics, hydrodynamics as well as of biochemistry.
在碳酸盐岩的形成及演化过程中，沉积作用是基础，成岩作用是关键。
Sedimentation is the foundation and diagenesis is the key in the process of generation and evolution of carbonate reservoirs.
因而认为地表、近地表方解石充填过程是碳酸盐岩洞穴型储层的“保持性成岩作用”。
So, the calcite filling in surface and near-surface is "retention diagenesis" of carbonate cavern reservoir.
因而认为地表、近地表方解石充填过程是碳酸盐岩洞穴型储层的“保持性成岩作用”。
So, the calcite filling in surface and near-surface is "retention diagenesis" of carbonate cavern reservoir.
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