| 沉积方式与碎屑岩储层的层内非均质性 |
| |
| 引用本文： | 李琦. 沉积方式与碎屑岩储层的层内非均质性[J]. 成都理工大学学报(自然科学版), 1996, 0(Z1) |
| |
| 作者姓名： | 李琦 |
| |
| 作者单位： | 成都理工学院 |
| |
| 摘 要： | 砂体的韵律性和砂岩储层层内不连续薄隔层的存在导致砂岩储层层内渗透率差异，从而影响其层内非均质性。本文对八类沉积方式形成的砂体的内部韵律性及泥质薄夹层分布特征进行讨论，建立各类砂体沉积模式与碎屑岩储层层的非均质性的联系。
|
| 关 键 词： | 沉积方式，碎屑岩储层，层内非均质性，韵律性，渗透率 |
MODE OF DEPOSITION AND INTRAFORMATIONAL ANISOTROPIC PROPERTY OF RESERVOIR OF CLASTIC ROCK |
| |
| Li Qi. MODE OF DEPOSITION AND INTRAFORMATIONAL ANISOTROPIC PROPERTY OF RESERVOIR OF CLASTIC ROCK[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1996, 0(Z1) |
| |
| Authors: | Li Qi |
| |
| Affiliation: | Chengdu Institute of Techmology |
| |
| Abstract: | Rhythm intenal sand body and uncontinuous thin teparate bedding lead to the differ-ence of permeabitity inside reserwir of sand rock,thus affect its intraformational anisotropic propetty. The paper discasses the grain size rhythm intenal sandbody formed by 8 kinds of mode of depisition and distributed Character of the thin pelitic mezzanine,and establishes the relation of pattern of deposition betwen the Intraformational anisotropic property. |
| |
| Keywords: | Mode of deposition Intraformationed anisotropic property resrvoir of clastic rock rhythm permeability |
| 本文献已被 CNKI 等数据库收录！ |
