albitization [,ælbiti'zeiʃən]

albitization的基本解释

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钠长石化

与albitization相关的网络例句 [注：此内容来源于网络，仅供参考]

According to geological characteristics of mineral area,geological conditions of mineralization,geochemical characteristics,material sources of mineralization,mineralization patterns,as well as physical and chemical conditions of mineralization,it summarize the mineralization pattern and genesis of ore deposit of Xianghualing mining areas,considering that mineralization materials in this deposit mainly come from magma,genesis patterns of deposit include high-temperature gas-liquid Nb、Ta deposit related to albitization laying in or on the edge of granite rock bodies,median-high temperature Skarn Sn,Be deposit related to skarnized laying at the inner contact-belt of granite and carbonate rock bodies;median-high temperature cassiterite -sulphide mineral deposit related to skamized laying at outer contact-belt of granite and carbonate rock bodies and median-low temperature hydrothermal liquid Pb-Zn-Ag deposit related to silicification,fluorite, propylitization laying in wall rocks;Series of generalized magma- hydrothermal liquid type Sn-polymatellitic related to magmatic activity in Yanshan period as a whole.

通过对矿区地质特征、成矿地质条件、地球化学特征、成矿物质来源、成矿作用、矿化型式以及成矿物理化学条件的分析，总结了香花岭矿区的矿床成因以及成矿模式，认为香花岭锡多金属矿成矿物质主要来源于岩浆，矿床成因类型包括花岗岩体内及其边部产出的与钠长岩化有关的高温气液型Nb、Ta矿床、花岗岩体与碳酸盐岩内接触带产出的与矽卡岩化有关的中高温矽卡岩型Sn、Be矿床、花岗岩体与碳酸盐岩外接触带产出的与矽卡岩化有关的中高温锡石硫化物矿床以及围岩中产出的与硅化、萤石化、青磐岩化有关的中低温热液型铅锌银矿床，整体构成与燕山期岩浆活动有关的广义岩浆热液型锡多金属成矿系列

Secondary feldspar was related to the albitization process of feldspar, the albitization of plagioclase began at the early stage of diagenesis, and the albi.

次生长石与长石的钠长石化过程有关，斜长石钠长石化始于成岩早期，而钾长石的钠长石化则需较高的成岩条件才能进行。

Thermodynamics calculation of fluid/rock interaction illustrates that the sea water is heated and causes K-feldsparthization of rock when it is descending, and the hot fluid is cooled when it is moving and erupting and causes albitization of rock.

通过流体—岩石平衡反应的热力学计算，首次提出本区碱交代作用可能的机制：在水—岩反应过程中，下降的海水由于被加热，使岩石发生钠长石化；热的流体在运移和喷出过程中，随着温度的降低，使岩石发生钾长石化。

The formation water salinity, pH value and geothermal gradient near the belt are abnormal due to mixing process according to this study. The interaction between the fluids arid the rocks assumes the process of albitization in plagioclase.

泊尔江海子断裂附近地层水矿化度pH值及地温梯度等出现异常，研究认为，造成断裂带地层水异常是由于混合作用，断裂带以外主要的流体－岩石相互反应是斜长石的钠长石化过程。

与albitization相关的网络解释 [注：此内容来源于网络，仅供参考]

albitization：钠长石化

albitite 钠长岩 | albitization 钠长石化 | albitolite 火山沉积钠长岩

albitization：钠长化作用,钠长石化

"钠长岩","albitite" | "钠长化作用,钠长石化","albitization" | "钠长斑岩","albitophyre"

albitization;albitisation：钠长化(作用);钠长石化

钠长岩 albitite | 钠长化(作用);钠长石化 albitization;albitisation | 钠长斑岩 albitophyre

albitisation; albitization：钠长石化(作用)

"钠长岩","albitite" | "钠长石化(作用)","albitisation; albitization" | "钠长石化正长石","albitized orthoclase"