| 1. | Development program of abnormal high pressure and low permeability reservoirs
异常高压特低渗透油藏的开发方案 |
| 2. | Numerical simulation of abnormal pressure and low permeability carbonate reservoirs in kenjiyake
肯基亚克异常高压特低渗透碳酸盐油藏数值模拟 |
| 3. | A simple pore pressure estimation method for a disequilibrium compaction shale using sonic velocity
利用声速检测欠压实泥岩异常高压的简易方法与应用 |
| 4. | It was primarily formed by undercompaction , hydrocarbon generation and tectonic compression
柴北缘异常高压主要由欠压实作用、生烃作用及构造挤压作用形成。 |
| 5. | Kela2 gas field is an abnormal pressure gas reservoir with the pressure coefficient of more than 2 . 0
摘要克拉2气田是一个异常高压气藏，压力系数在2 . 0以上。 |
| 6. | Analysis of current of abnormal high pressure distribution characteristicsistic and discuss which cause of formation in kuqa depression of tarim basin
塔里木盆地库车拗陷现今异常高压分布特征及其成因 |
| 7. | This model can be used to determine the permeability , porosity , net pay thickness and ogip without chart matching
运用该方法不需要进行图版拟合就可以确定出异常高压气藏的渗透率、孔隙度、有效厚度和地质储量。 |
| 8. | This paper analyzes the cause of the formation of original abnormal high pressure and proposes an effective method to ensure cementing quality
分析了原始异常高压层形成的原因，制定了保证固井质量的有效措施。 |
| 9. | Hut different structural units have different characteristics in initial horizon , initial depth of abnormal pressure and their section features
各构造单元在异常高压初始层位、初始深度、剖面特征等方面又有不同特点。 |
| 10. | Abnormal high pressure is found from neogene to jurassic in leughu - nanbaxian strnctural belt in the northern margin of qaidam basin , and mostly occurs in undercompaction shale
摘要柴北缘冷湖南八仙构造带从新近系到侏罗系普遍存在异常高压，且通常发育在欠压实泥岩中。 |
