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1)  layered reservoir
层状储集层
2)  lenticular reservoir
透镜状储集层
3)  massive conglomeratic reservoir
块状砾岩储集层
4)  deep reservoir
深层储集层
1.
The effect of the abnormal pressure on deep reservoir evolution is discussed by lab experiments of compaction,diagenesis,pressolution-cementation,breakup and plastic deformation of sandstone and mudstone,etc.
在分析东濮凹陷深层异常高压形成及分布的基础上,利用实验手段从压实成岩、溶蚀-胶结作用和砂岩、泥岩的破裂及塑性变形等多方面探讨了异常高压对深层储集层演化的影响,认为异常高压发育不仅有利于深层储集层孔、渗条件的保存,而且通过物理和生物化学两种作用改善了储集层物性,东濮深层成藏有较好的储集层条件,预示其深层有较广阔的勘探前景。
5)  massive reservoir
块状储层
1.
A set of technical methods for geologic modeling suitable to massive reservoir was studied.
通过对礁灰岩成因环境的分析,结合地震属性认识储层空间分布特征,揭示了块状地质体与垂向加积碎屑岩储层地质建模方面的特殊性,探索了适合块状储层地质建模的技术方法,取得了较好的效果。
6)  sedimentary geothermal field
层状热储
1.
,Based on experiences of geothermal exploration and research,combining with ac- tual exploration and research degree,a new method of allowable geothermal production calculating for sedimentary geothermal fields has been put forward in this paper.
鲁西北地热田层状热储中的地下热水,是深层承压水。
补充资料:储层描述(见油气田储层评价)


储层描述(见油气田储层评价)
reseroir evaluation of oil and gas field

  储层描述(reseroir evaluation of 011 and gasfield)见油气田储层评价。
  
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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