pyritization

pyritization的基本解释

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黄铁矿化

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

Rare elements and REE are mainly enriched in gray-black trachyte and less in other rocks. In addition, schistosity, pyritization, silicification and carbonation in gray-black trachyte are contributed to enrich rare element and REE. It is suggested that alkaline rocks in Hongyang area have the characteristics of subvocanics, and alkaline rocks in Hongyang and Miaoya areas all came from upper mantle and mixed with some substances of crust. Intrusion of alkaline rocks is related to the occurrence, development and evolvement of the deep rupture zone in the areas.

稀土、稀有元素主要富集于灰黑色粗面岩中，而在其他岩石类型中相对较少，同时岩石的片理化、黄铁矿化、硅化和碳酸盐化对稀土、稀有元素有进一步的富集作用；提出了本区的碱性岩组合具有次火山岩相的特征，讨论了本区碱性岩的成因，认为其与湖北庙垭地区的碱性岩可能均来自上地幔，并不同程度地混染了大陆壳的物质成分，其形成时代与断裂构造带的发生、发展和演化基本同步。

The relationship of ore-forming fluid salinity-aqueous cation lg demonstrated that water-rock reaction was also one of the potential gold deposition mechanisms besides mixing with meteoric water. All of these were consistent with that sericitization and pyritization hydrothermal alteration were extensively/intensively distributed (as high as 33%), gold grade linearly correlated with degree of alteration,∑REE depletion and δ〓O enrichment

成矿流体盐度-液相主要阳离子组分1g演化规律研究表明，除与大气降水的混合-稀释外，水-岩相互作用也可能是造成金沉淀的重要因素，这与本文所研究金矿床中绢云母化、黄铁矿化等热液蚀变广泛发育(可高达33％)，Au品位与热液蚀变程度、REE亏损量及δ〓O富集规模表现出较为明显的线性关系等一系列地质事实相吻合

The main types of the wall-rock alteration are silicification,potash-alteration,pyritization,sericitization,chloritization and carbonatization,of which the strong silicification,potash-alteration and pyritization are closely related to gold mineralization.

流体—岩石反应引发的围岩蚀变是造成萑香洼金矿床金沉淀成矿的主要原因。

It occurs in granodioritic porphyre and granitic porphyre and the spatial distribution of the jade veins are controlled by lithology. The raw jade is in multi-colors with scaly blastic and massive textures under microscope. Wallrock alteration is developed and characterized by zoning as sericitization, kaolinization and pyritization.

玉石矿脉的空间分布受岩性控制，赋存于花岗闪长斑岩或花岗斑岩中；玉石原石色彩多样，岩石以显微鳞片变晶结构和块状构造为主；矿区围岩蚀变发育，具有绢云母化、高岭土化和黄铁矿化的蚀变分带现象。

The main alterations related to gold mineralization are pyritization、silicification and carbonatization.

与金矿化有关的蚀变类型主要有黄铁矿、毒砂化、硅化、碳酸岩化和粘土岩化等。

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

pyritization：黄铁矿化

作用的初期会有一系 黄铁矿化(pyritization)的产物生成. 由於 复铁矿有机碳(TOC)、全 (TS)、全 铁(FeT)、1N 盐酸可萃取之铁(FeA)(一) 以布 安散射仪测 phase D、霰石(aragonite)、白云石(dolomite)和镁矿(magnesite)的弹性系 . Phase D 是唯一可能存在地球下地幔的() 磷灰石(apatite)之酸性溶解:天然磷灰石在酸性环境之对 溶

pyritization：黄铁矿化(作用)

黄铁矿层状矿床 pyritic bedded deposit | 黄铁矿化(作用) pyritization | 五角十二面体 pyritohedron