{"title":"矿化与贫瘠侵入体:罗马尼亚黄金四边形的熔体包裹体研究","authors":"Luminita Grancea, Michel Cuney, Jacques L Leroy","doi":"10.1016/S1251-8050(01)01666-4","DOIUrl":null,"url":null,"abstract":"<div><p>Characterization of the genetic relations between magma suites and associated gold/base metal hydrothermal deposits is imperative to our understanding of the role of magmas in the mineralization process. Melt inclusions trapped in igneous phenocrysts were used to characterize calc–alkaline magmas associated with Valea Morii porphyry–copper deposit, Romania. A comparative study of mineralized intrusion versus barren intrusion reveals parameters that may influence the magmatic–hydrothermal connection. The present results emphasize the importance of the chemistry of residual melts (trapped in magmatic inclusions) rather than bulk magma compositions (derived from whole rock analysis) in determining the metal concentration in released magmatic fluid.</p></div>","PeriodicalId":100301,"journal":{"name":"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science","volume":"333 11","pages":"Pages 705-710"},"PeriodicalIF":0.0000,"publicationDate":"2001-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01666-4","citationCount":"5","resultStr":"{\"title\":\"Mineralised versus barren intrusions: a melt inclusion study in Romania's Gold Quadrilateral\",\"authors\":\"Luminita Grancea, Michel Cuney, Jacques L Leroy\",\"doi\":\"10.1016/S1251-8050(01)01666-4\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Characterization of the genetic relations between magma suites and associated gold/base metal hydrothermal deposits is imperative to our understanding of the role of magmas in the mineralization process. Melt inclusions trapped in igneous phenocrysts were used to characterize calc–alkaline magmas associated with Valea Morii porphyry–copper deposit, Romania. A comparative study of mineralized intrusion versus barren intrusion reveals parameters that may influence the magmatic–hydrothermal connection. The present results emphasize the importance of the chemistry of residual melts (trapped in magmatic inclusions) rather than bulk magma compositions (derived from whole rock analysis) in determining the metal concentration in released magmatic fluid.</p></div>\",\"PeriodicalId\":100301,\"journal\":{\"name\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"volume\":\"333 11\",\"pages\":\"Pages 705-710\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2001-12-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/S1251-8050(01)01666-4\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S1251805001016664\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1251805001016664","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Mineralised versus barren intrusions: a melt inclusion study in Romania's Gold Quadrilateral
Characterization of the genetic relations between magma suites and associated gold/base metal hydrothermal deposits is imperative to our understanding of the role of magmas in the mineralization process. Melt inclusions trapped in igneous phenocrysts were used to characterize calc–alkaline magmas associated with Valea Morii porphyry–copper deposit, Romania. A comparative study of mineralized intrusion versus barren intrusion reveals parameters that may influence the magmatic–hydrothermal connection. The present results emphasize the importance of the chemistry of residual melts (trapped in magmatic inclusions) rather than bulk magma compositions (derived from whole rock analysis) in determining the metal concentration in released magmatic fluid.
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