波兰下西里西亚Rędziny锡石的地球化学及成因

Q4 Earth and Planetary Sciences

Mineralogia Pub Date : 2007-01-01 DOI:10.2478/V10002-007-0028-3

A. Pieczka, B. Gołębiowska, J. Parafiniuk

{"title":"波兰下西里西亚Rędziny锡石的地球化学及成因","authors":"A. Pieczka, B. Gołębiowska, J. Parafiniuk","doi":"10.2478/V10002-007-0028-3","DOIUrl":null,"url":null,"abstract":"Abstract.Thegeochemistryofcassiteritemayindicateitsorigin.IncassiteritefromRedziny,FeandTiare major substitutes for tin, whereas Nb, Ta and Mn do not occur in significant amounts. Tungsten, whichconcentratesonlyinsomecassiteritedomainsinamountsthatmayexceed1wt.%,iscommonlyclosetozero.ThedistributionofTi,anelementmobileunderstronglyreducingconditions,indicatesthattheformationofthe oldest cassiterite preceded a sphalerite-chalcopyrite-ferrokesterite paragenesis, and that the latter wasfollowedbycassiteritecoevalwitharsenopyrite.Bothcassiteritesprecipitatedunderconditionsofverylowoxygen fugacity, probably below log f (O) 2 = –40. The younger cassiterite, present in oxidized assemblages,crystallized under increasing f (O) 2 .Theco-variationsFe+Mn vs .Nb+TaandHf vs . Zr clearly and une-quivocally point to a hydrothermal origin for the cassiterite from Redziny that can be linked topost-magmatic activity developed around the Karkonosze granite intrusion. Key-words : cassiterite, quartz veins, Redziny, Lower Silesia, Poland, geochemistry, origin","PeriodicalId":18686,"journal":{"name":"Mineralogia","volume":"53 1","pages":"219-230"},"PeriodicalIF":0.0000,"publicationDate":"2007-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"10","resultStr":"{\"title\":\"Geochemistry and Origin of the Cassiterite from Rędziny, Lower Silesia, Poland\",\"authors\":\"A. Pieczka, B. Gołębiowska, J. Parafiniuk\",\"doi\":\"10.2478/V10002-007-0028-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract.Thegeochemistryofcassiteritemayindicateitsorigin.IncassiteritefromRedziny,FeandTiare major substitutes for tin, whereas Nb, Ta and Mn do not occur in significant amounts. Tungsten, whichconcentratesonlyinsomecassiteritedomainsinamountsthatmayexceed1wt.%,iscommonlyclosetozero.ThedistributionofTi,anelementmobileunderstronglyreducingconditions,indicatesthattheformationofthe oldest cassiterite preceded a sphalerite-chalcopyrite-ferrokesterite paragenesis, and that the latter wasfollowedbycassiteritecoevalwitharsenopyrite.Bothcassiteritesprecipitatedunderconditionsofverylowoxygen fugacity, probably below log f (O) 2 = –40. The younger cassiterite, present in oxidized assemblages,crystallized under increasing f (O) 2 .Theco-variationsFe+Mn vs .Nb+TaandHf vs . Zr clearly and une-quivocally point to a hydrothermal origin for the cassiterite from Redziny that can be linked topost-magmatic activity developed around the Karkonosze granite intrusion. Key-words : cassiterite, quartz veins, Redziny, Lower Silesia, Poland, geochemistry, origin\",\"PeriodicalId\":18686,\"journal\":{\"name\":\"Mineralogia\",\"volume\":\"53 1\",\"pages\":\"219-230\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2007-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"10\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mineralogia\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2478/V10002-007-0028-3\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mineralogia","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2478/V10002-007-0028-3","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}

引用次数: 10

摘要

Abstract.Thegeochemistryofcassiteritemayindicateitsorigin。来自redziny, fean和tian的inassite是tin的主要替代品，而Nb, Ta和Mn的含量并不高。钨、iscommonlyclosetozero whichconcentratesonlyinsomecassiteritedomainsinamountsthatmayexceed1wt. %。强还原条件下的元素流动ti的分布表明，最古老锡石的形成先于闪锌矿-黄铜矿-铁铁矿共生，后者之后是锡石与毒砂的共生。这两种化合物都是在氧逸度很低的条件下析出的，可能低于log f (O) 2 = -40。较年轻的锡石，存在于氧化组合中，随着f (O) 2的增加而结晶。Zr清晰而独特地指出了来自Redziny的锡石的热液起源，这可以与Karkonosze花岗岩侵入周围的顶部岩浆活动联系起来。关键词:锡石，石英脉，红锌，下西里西亚，波兰，地球化学，成因

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

Geochemistry and Origin of the Cassiterite from Rędziny, Lower Silesia, Poland

Abstract.Thegeochemistryofcassiteritemayindicateitsorigin.IncassiteritefromRedziny,FeandTiare major substitutes for tin, whereas Nb, Ta and Mn do not occur in significant amounts. Tungsten, whichconcentratesonlyinsomecassiteritedomainsinamountsthatmayexceed1wt.%,iscommonlyclosetozero.ThedistributionofTi,anelementmobileunderstronglyreducingconditions,indicatesthattheformationofthe oldest cassiterite preceded a sphalerite-chalcopyrite-ferrokesterite paragenesis, and that the latter wasfollowedbycassiteritecoevalwitharsenopyrite.Bothcassiteritesprecipitatedunderconditionsofverylowoxygen fugacity, probably below log f (O) 2 = –40. The younger cassiterite, present in oxidized assemblages,crystallized under increasing f (O) 2 .Theco-variationsFe+Mn vs .Nb+TaandHf vs . Zr clearly and une-quivocally point to a hydrothermal origin for the cassiterite from Redziny that can be linked topost-magmatic activity developed around the Karkonosze granite intrusion. Key-words : cassiterite, quartz veins, Redziny, Lower Silesia, Poland, geochemistry, origin

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

Mineralogia Earth and Planetary Sciences-Geology

CiteScore

0.80

自引率

0.00%

发文量

期刊介绍： - original papers in the scope of widely understood mineralogical sciences (mineralogy, petrology, geochemistry, environmental sciences, applied mineralogy etc.) - research articles, short communications, mini-reviews and review articles