| 1. | Scanty but growing evidence links the character of early diagenesis with specific depositional environments .
有关早期成岩作用的特征与特定沉积环境的关系，证据虽然不多，但却在不断增加。 |
| 2. | Study indicates that the formation and evolution of the porosity are controlled by diagenesis
研究表明：孔隙的形成和演化受成岩作用的控制。 |
| 3. | Finally regional distribution of reservoir has been predicted . study suggests that feixianguan formation is essentially controlled by sedimentation and diagenesis
研究表明，飞仙关组储层主要受沉积作用和成岩作用的控制。 |
| 4. | Reservoir properties are mainly controlled by sedimentary microfacies and diagenesis ; the effect of the tectonic movements on the reservoir is relatively limitted
研究区储层性质主要受沉积微相和成岩作用的控制，构造运动对本区储层性质的影响较有限。 |
| 5. | In this thesis , the chemical kinetic models with higher active energy enhanced by overpressure factors could be used for modeling the organic matter maturation and diagenetic history of the overpressured formation
本文通过在成岩反应的化学动力学模型中加入超压因子增加反应活化能，建立了超压条件下成岩作用的数值模拟系统。 |
| 6. | Pressure separation is usually controlled by the following factors , such as subsidence rate , sediment types and diagenesis during the diagenetic evolution , as a result the pressure gradient is uncontinuous
地层压力分隔化是由于沉积物在成岩演化过程中受各种因素，如沉积速率、沉积物类型以及成岩作用的影响，使地层中的流体压力梯度呈现出随深度变化不连续的一种现象。 |
| 7. | Abstract : pressure separation is usually controlled by the following factors , such as subsidence rate , sediment types and diagenesis during the diagenetic evolution , as a result the pressure gradient is uncontinuous
文摘:地层压力分隔化是由于沉积物在成岩演化过程中受各种因素，如沉积速率、沉积物类型以及成岩作用的影响，使地层中的流体压力梯度呈现出随深度变化不连续的一种现象。 |
| 8. | Nonce , the system of diagenetic numerical modeling for the stratum under the conditions of normal pressure has been set up . in lots of sags rich of petroleum in the basins of eastern china , such as qibei sag of bohaiwan basin , there are plenty of deep - buried overpressure reservoir
但在中国东部许多盆地的富油气凹陷，如渤海湾盆地歧北凹陷，油气藏分布在深层超压地层中，超压条件下成岩作用的数值模拟尚不完善，更不用说孔隙度预测了。 |
| 9. | Reefs are well developed in western hubei and eastern chongqing . through sedulous research , the whole acquaintance on types of reef builders , types of reef carbonatite , development and evolution of reef organisms , division of reef facies , distributing regularities of reefs and diagenesis has been concluded . according to the comprehensive studies , the following results and conclusions have been obtained
通过对鄂西渝东区上二叠统长兴组生物礁造礁生物、沉积相、成岩作用的研究，认清了礁体的主要造礁生物类型、主要岩石类型、生长演化、相带划分、分布规律以及成岩作用，可以得出以下结论和认识： 1生物礁主要分布于晚二叠世碳酸盐台地内部和台地边缘，可分为三种类型。 |
| 10. | The great number of pores of reef rocks disappeared due to multi - generational cementation in submarine and taphonomic environments . the pores in reef rocks are mainly secondary and the primary pores are almost filled up . the evolution of pores is wholly controlled by diagenesis , all in a word , the histoty of diagenesis is evolution of pores
礁灰岩中的大量孔隙被海底和埋藏成岩环境中多期胶结物充填而丧失，孔隙类型以次生孔隙为特征，原生孔隙基本被填实，孔隙演化完全受成岩作用的控制，成岩作用的发展史就是孔隙的演化史。 |
