| 1. | Basement structure of the north yellow sea basin
塔北隆起异常压力与油气成藏分析 |
| 2. | Analysis on water cut in mudstone and the abnormal formation pressure
泥岩地层产水与地层异常压力原因分析 |
| 3. | It is a zone of abnormal pressure
这是异常压力层 |
| 4. | Abnormally pressurized reservoir
异常压力储集层 |
| 5. | Review of new ideas of petroleum geology associated with abnormal fluid pressure system
评述异常压力研究中的石油地质学新思想 |
| 6. | Abnormal pressure is formed by uneven degradation causing a great elevation difference . 4
不均匀剥蚀情况可造成地形较大的高差，从而导致压力系数异常，形成异常压力。 |
| 7. | According to oil - gas accumulation mechanism under abnormal pressure , the hydrocarbon accumulation phases are classified , and the elects of the abnormal overpressure on reservoir type awl distribution are analyzed
依据异常压力成效机制对柴西南油气成藏阶段进行了划分，并分析了异常压力对油气藏类型和油气藏分布的控制作用。 |
| 8. | In beier depression , high pressure reached to 5mpa , and in different area the high pressure appear in different stratum ; on plane , the high pressure in the southern area of wuerxun was higher than that of in the northern area
贝尔凹陷，最大异常幅度为5mpa ，且其在不同地区出现的层位不同；横向上，乌尔逊凹陷南部异常压力大于乌尔逊凹陷北部。 |
| 9. | The analysis of tested pressure and the study of abnormal pressure characteristic in partial prospecting wells indicate that there exist various types of pressures in southwestern qaidam basin and abnormal overpressure in certain depth
摘要通过对部分探井测试压力的分析和异常压力特征的研究，发现柴达木盆地西部南区压力类型多样，在一定深度存在异常高压。 |
| 10. | The following are main conclusion and recognition : firstly , basing on the study mudstone compaction , drawing a conclusion is that the profile and plane feature of palaeo - pressure in y3 , on profile , the pressure ranged from 5mpa to 10mpa in the southern area of wuerxun . usually , high pressure was in n1 or t . in the northern area of wuerxun , high pressure almost reached to 5mpa , high pressure usually was in d1 or n2
在海拉尔盆地研究中，以此为切入点，通过大量实际工作，取得了如下初步的研究结论和认识：首先，通过压实研究，得出了地层在最大埋深状态下(伊敏组末) ，古压力的纵横向分布特征：纵向上，乌尔逊凹陷南部异常压力幅度在5 10mpa之间，最大异常压力一般出现在南屯组一段或铜钵庙组。 |
