| 1. | The minerals may have variously experienced reaction, resorption, and perhaps even growth, as they settled .
当矿物沉降之后，它们可能经历了多种反应作用，溶蚀作用甚至可能还有生长作用。 |
| 2. | The diageneses mainly comprise cementation , compaction and dissolition
主要成岩作用有机械压实作用、胶结作用和溶蚀作用。 |
| 3. | The dissolution process and the rock mass breakage of marlite slope in three gorges reservoir region
三峡库区泥质灰岩溶蚀作用与边坡岩体破坏 |
| 4. | Variation of mechanical property of marlite in process of karstification and weathering in three gorges region
三峡库区泥灰质岩石溶蚀作用的微观研究 |
| 5. | The physical properties are mainly dominated by thress factors : solution , sedimentary facies and buried depth
主要发育次生孔隙，储层物性受溶蚀作用、沉积相、埋藏深度三个因素的控制。 |
| 6. | When the environment condition of water changed or the chemical homeostasis was disturbed , corrosion and solution occured , and the travertine landscapes was rebuilt by conveying , scouring , and collapsing
当水环境条件改变或水化学动态平衡失调时，重溶蚀作用发生，搬运?冲刷?坍塌?重组形成新的钙华堆积景观。 |
| 7. | However , when the samples have different effective contact areas , the degrees of dissolution may depend on the swing of the pendulum between the dissolution velocity and their effective contact area
但当样品在水岩反应过程中有不同的比表面积时，溶蚀作用的强弱或快慢就取决于岩石溶蚀速率与水岩反应有效接触面积的消长关系。 |
| 8. | The major diagenetic events include mechanical compaction , chemical compaction , cementation , replacement and dissolution . the reservoir quality experienced from being destroyed to being enhanced during the whole diagenetic evolution process
主要的成岩作用有：机械压实作用，化学压实作用，胶结作用，交代作用以及溶蚀作用。 |
| 9. | These characteristics have close relation with transgression from eastern to western . 4 . reefs undermined various and complicated diagenesis , in which cementation , dolomitization and corrosion etc . play main roles in the history of reef diagenesis
4礁岩的成岩作用具多样性和复杂性，其中泥晶化、填积、胶结、白云化和溶蚀作用最为重要。 |
| 10. | Among them , phreatic , vadose and in the middle of convection zones undergone dissolution ( especially in vadose zone ) . the mixing and upper convection zones undergone cementation . the lower convection zone remained unaltered
其中渗流、潜流和深部对流带中部以溶蚀作用为主(潜流带最强烈) ，混合带和对流带上部以胶结作用为主，对流带下部成岩作用不活跃。 |
