浙江某金银矿床黃铁矿的穆斯堡尔谱参数及其地质意义
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Mosabauer Parameters of Pyrite from a Certain Gold一Silver Ore Deposit in Zhe jiang Province and Their Geological Significance
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    摘要:

    本文根据黄铁矿及有关矿物的晶体结构和穆斯堡尔谱参数的特点、对浙江某金银矿床及有关矿床的黄铁矿中杂质元素含量及其对黄铁矿结构与穆斯堡尔谱参数的影响,得出黄铁矿的四极分裂值QS的变化主要由黄铁矿中呈类质同象存在的杂质元素的含量不同所致的结论。由于黄铁矿中这些杂质元素的含量具有指示矿床成因、矿化阶段、矿床分带以及矿物组合的意义,因而黄铁矿的穆斯堡尔谱参数也就具有这些方面的意义,这可作为黄铁矿的一个新的标型特征并可在矿床的找寻、评价和勘探工作中应用。

    Abstract:

    Eleven pyrite samples from a certain gold-silver ore deposit in Zhejiang province have been examined to find out the relationship between such isomorphous impurities in pyrite as Co,Ni, As, Sb and the 57Fe Mossbauer parameters at 298 ºK. As a result, the following conclusions have been reached. (1)The relationship between the electric quadrupole splitting (QS) of pyrite and its arsenic content obtained by means of linear regression of six pyrite samples with available quantitative arsenic analyses is QSpr=0.612+ 0,00925As(at%).Antimony impurity has a similar but a bit smaller effect on the QS of pyrite. (2)The linear equation for the relationship between the QS of pyrite and its cobalt content obtained from the QS and Co contents of pyrite as well as synthesized Co0.25Fe0.75S2 and Co0.99 Fe0.01 S2 is QSpy-co=0.608一 0,0087Co (at%).Nickel impurity has a similar but somewhat larger effect on the QS of pyrite, (3)The QS of pyrite depends on the atomic percentage ratio of its impurities(As+Sb)/(Co+Ni),i, e.,the QS value increases with the growing ratio. (9)As the contents of impurities in pyrite are related to formation condition, the QS of pyrite might find application in such aspects of ore research as the genesis of ore deposits, the division of ore-forming stages, the metallogenic zoning and the mineral assemblages, and therefore can surely play its role in the prospecting, evaluation and exploration of ore deposits,

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刘平,1988,浙江某金银矿床黃铁矿的穆斯堡尔谱参数及其地质意义[J].岩石矿物学杂志,7(2):167~175. Liu Ping,1988,Mosabauer Parameters of Pyrite from a Certain Gold一Silver Ore Deposit in Zhe jiang Province and Their Geological Significance[J]. Acta Petrologica et Mineralogica,7(2):167~175.

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