1) fluid flow
流体活动
1.
Evidences of fluid flow along Lanliao Fault Zone in Dongpu Depression;
东濮凹陷兰聊断裂带流体活动的证据
2.
Evidences of fluid flow along fault zones in Shengbei Fault Zone of Dongying Depression;
断裂带流体活动证据的确定——以东营凹陷胜北断裂带为例
3.
Distinct fluid flow and transport pathways generally occur in abnormal high pressure (AHP) systems of sedimentary basins.
另一方面,自生石英流体包体均一温度大部分在105～145℃之间,频数呈多峰式展布,可能显示幕式流体活动。
2) fluid activity
流体活动
1.
Mass transfer and microtexture of retrograded Qinglongshan eclogite:evidence of fluid activity;
青龙山榴辉岩的退变质显微结构及相关的物质迁移——南苏鲁榴辉岩退变质过程中流体活动的证据
2.
This paper discusses the relations between fluid movement and geothermal structure\|calorific effects of fluid movement, geochemical effects of geothermal abnormality, fluid activity\|geothermal transference and their models.
本文对流体活动与地温结构的相互作用关系流体活动的热效应、地温异常导致的地球化学效应、流体活动 -地热传输的耦合过程及其模拟进行了研究。
3) fluid movement
流体活动
1.
Based on studying of these special structure bodies and fluid movements for gas hydrate formation,six types of tectonic-controlled gas hydrate reservoirs including accretionary prism,buried anticline,basin-edge slope,fault-folded,slide and dirpir are summarized.
通过对这些特殊构造体与天然气水合物成藏关系的研究,结合流体活动对水合物形成的影响,总结出陆缘地区有增生楔型、盆缘斜坡型、埋藏背斜型、断褶型、滑塌型及底辟型等六类构造控制型水合物矿藏。
2.
Its applications were discussed in the analyses and research of basin fluid diagenetic mineralogical age, fluid field character, evolution of formation water origin, reservoir heterogeneity, fluid movement trace, temperature and salinity of ancient fluid, distinguishing between sea facies and lake facies, diagenetic environment.
该文从原理出发,综合前人的研究,论述了其在盆地流体成岩矿物年代学分析、流体场特征分析、地层水成因演化研究、储层非均质性研究、流体活动示踪、古流体温度、盐度分析、海相、湖相区分、成岩环境分析等方面的应用。
4) fluid action
流体活动
1.
While much attention has been paid to fluid action in mafic HP to UHP eclogites in continental and oceanic subduction zones, less is focused on felsic UHP gneiss in continnetal subduction zones.
板块俯冲和折返过程中的流体活动是碰撞造山带变质作用、同碰撞岩浆作用乃至成矿作用的重要内容之一,也是理解地球演化,包括全球水循环、深俯冲板块的命运、碰撞造山带内的岩浆岩成因,以及洋壳和陆壳再循环等问题的关键。
2.
In order to understand the process of the formation of low-ultra low permeable reservoir and the relationship between the development of reservoir physical property (including surface wettability) and the time of fluid filling, this paper analysis the character of fluid action which is discussed in terms of fluid flow regime, action time and palaeotemperature.
松辽盆地古龙凹陷葡萄花油层属于低-超低渗储层,为了解低-超低渗储层的形成过程、储层的物性(包括表面润湿性)演化及其与油气充注时间的关系,本文从流体的流动方式、活动期次与活动时间及其古温度等几个方面开展了流体活动特征研究。
5) thermal fluid activity
热流体活动
1.
Characteristics of fluid inclusions on thermal fluid activity in oil-and gas-bearing basins;
含油气盆地中热流体活动的流体包裹体依据
2.
The main characters of the thermal fluid activity are recognized as follow: many types and stages of veins are widely developed;vitrinite reflectivity of different areas varies apparently with the depth;there was a high temperature field during the formation of the thermal fluid.
海拉尔盆地贝尔凹陷布达特群热流体活动频繁,主要特征如下:多种类型、多期次脉体的发育;受局部热流体作用,不同地区镜质体反射率随深度的变化明显;热流体在形成过程中具有较高的温度场。
6) Hydrothermal fluids flow
活动热流体
1.
Hydrothermal fluids flow have significance to petroleum geology: (1)changed the fields of temperature and pressure; (2) significantly enh.
根据热流体活动通道 ,将沉积盆地活动热流体类型划分为侧向对流型、垂向对流型和侧向 -垂向对流复合型。
补充资料：HeⅡ的二流体模型（two-fluidmodelofHeⅡ）
HeⅡ的二流体模型（two-fluidmodelofHeⅡ）
在低于λ点相变温度Tλ附近，毛细管中测出液HeⅡ的黏性系数η比正常的HeⅠ液体的要小1011倍，但在旋转圆柱容器中测出的η值比正常HeⅠ的相关不大，这个矛盾由Tisza于1938年提出二流体模型和1941年朗道独立地从量子流体力学给出了更完善的二流体模型予以解释，并解释了其他实验现象。这个模型认为HeⅡ液体由密度为ρs，而流速vs是无旋的`(\nabla\timesbb{v}_s=0)`、黏性系数ηs=0，且是零熵的超流部分(s)，和具有正常液体性质的正常部分(n)这两个部分组成，而液体HeⅡ的总密度ρ=ρs ρn，ρs和ρn随温度T的变化如下：
实际上，正常和超流部分同是4He原子组成，正常流体用热激发产生的声子或旋子这两种准粒子来描绘（参见“朗道超流的唯象理论”），在0＜T＜Tλ间是正常和超流这两种不同性质液化按不同比例的混合液体，两者之间没有摩擦。超流液体不需要压力差照常可在通道中流动。二流体模型解释了热机械效应等，还预言了在HeⅡ液体中存在第二声波，即熵波或称热波，并为实验所证实。
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