1) geothermal reservoir
热储层
1.
4 geothermal reservoirs can be used, and the reservoir at the lower part of Guantao formation has the highest exploration value.
可被利用的热储层有4个,最有开发利用价值的是馆陶组下段热储,该热储层顶板埋深约1100m,底板埋深约1700m,热储层厚度530~580m,含水层累积厚度158~175m,单井涌水量1500~2000m3/d,出口水温62~67℃,矿化度5000mg/L左右,具腐蚀性,结垢性弱,具较好的开发利用价值。
2.
Through analysis and study on hydro-geological condition,geothermal reservoir characterisics and geothermal field charactersitics of geothermal resource in Zhangdian area of Zibo city,on the basis of studying forming model of geothermal field,geothermal field model in Zhangdian geothermal field is established,and forming mechanism of Zhangdian geothermal field is illustrated as well.
通过对淄博张店地区地热资源形成的水文地质条件、热储层特征及地温场特征等分析研究,并对张店地热田形成模式进行了探讨,建立了张店地热田热储概念模型,阐明了张店地热田形成的机理。
2) reservoir
[英]['rezəvwɑ:(r)] [美]['rɛzɚ'vwɑr]
热储层
1.
This paper has studied the composing of geothermal system in East Plain of Henan province,divided the geothermal reservoir and analyzed their burying and distributing characteristics.
在平面上按照构造单元区域将河南省东部平原地热系统分为 8个亚系统 ,垂向上按照埋藏深度划分为上、中、下三个热储层 。
3) hot reservoir
热储层
1.
The hot reservoir is mainly composed of the lower part of Minghuazhen Formation and Guantao Formation in Neogene period and Dongying Formation in Paleogene period.
通过已有地质资料及近年的勘查项目研究成果,对东明地热田的地热资源的地质背景、热储特征、地球物理化学特征等进行了研究分析,认为东明地热田属于层控型低温地热田,热储层主要为新近纪明化镇组下部、馆陶组、古近纪东营组地层,该区的地温梯度主要受构造控制,断裂导热是形成该地温场的一个重要因素,地下热水水平方向水化学组分变化甚微,具有明显的垂直分带性,地热水水源主要为渗入的溶滤水。
4) heat storage layer
储热层
1.
The terrestrial heat is very obvious,the heat storage layer is growing,has abundant geothermic resources and is equipped with the condition of the geothermic well to be forming.
渭河盆地北缘地质构造相对简单,地热异常明显,储热层发育,有丰富的地热资源,具备地热井成井条件。
5) thermal storage beds
热液储层
6) thermal energy storage in the same layer
同层热储
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。
参考词条