{"title":"富铌玄武岩:板块衍生熔融交代地幔橄榄岩部分熔融的产物","authors":"Niu Hecai, Zhang Hai-xiang, Zhang Boyou","doi":"10.11867/J.ISSN.1001-8166.2005.11.1234","DOIUrl":null,"url":null,"abstract":"Nb-enriched basalt is a kind of arc basalt that has special geochemical characteristics.It is silica-saturated with high Na_(2)O contents and differs from the typical arc basalt by the extremely high Nb(7×10~(-6)),TiO_(2)(1%～2%) and P contents with HFSE enrichment.In the primitive mantle-normalized trace element spider diagram,Nb-enriched basalts show weakly negative(sometime positive) Nb,Ta anomalies.The primitive mantle-normalized La/Nb ratios of the Nb-enriched basalts are smaller than 2(but smaller than 0.7,occasionally).It is derived from the partial melting of mantle peridotite metasomatized by slab melts.Since Nb-enriched basalts and adakites are the direct products of subducted oceanic slab,the characteristics of magma activity and interaction between slab melts and mantle wedge can be demonstrated by the studies of this association and the nature of the relative fluids and melts.","PeriodicalId":415150,"journal":{"name":"Advance in Earth Sciences","volume":"123 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2005-11-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"Nb-ENRICHED BASALT: THE PRODUCT OF THE PARTIAL MELTING OF THE SLAB-DERIVED MELTMETASOMATIZED MANTLE PERIDOTITE\",\"authors\":\"Niu Hecai, Zhang Hai-xiang, Zhang Boyou\",\"doi\":\"10.11867/J.ISSN.1001-8166.2005.11.1234\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Nb-enriched basalt is a kind of arc basalt that has special geochemical characteristics.It is silica-saturated with high Na_(2)O contents and differs from the typical arc basalt by the extremely high Nb(7×10~(-6)),TiO_(2)(1%～2%) and P contents with HFSE enrichment.In the primitive mantle-normalized trace element spider diagram,Nb-enriched basalts show weakly negative(sometime positive) Nb,Ta anomalies.The primitive mantle-normalized La/Nb ratios of the Nb-enriched basalts are smaller than 2(but smaller than 0.7,occasionally).It is derived from the partial melting of mantle peridotite metasomatized by slab melts.Since Nb-enriched basalts and adakites are the direct products of subducted oceanic slab,the characteristics of magma activity and interaction between slab melts and mantle wedge can be demonstrated by the studies of this association and the nature of the relative fluids and melts.\",\"PeriodicalId\":415150,\"journal\":{\"name\":\"Advance in Earth Sciences\",\"volume\":\"123 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2005-11-25\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Advance in Earth Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.11867/J.ISSN.1001-8166.2005.11.1234\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Advance in Earth Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.11867/J.ISSN.1001-8166.2005.11.1234","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Nb-ENRICHED BASALT: THE PRODUCT OF THE PARTIAL MELTING OF THE SLAB-DERIVED MELTMETASOMATIZED MANTLE PERIDOTITE
Nb-enriched basalt is a kind of arc basalt that has special geochemical characteristics.It is silica-saturated with high Na_(2)O contents and differs from the typical arc basalt by the extremely high Nb(7×10~(-6)),TiO_(2)(1%～2%) and P contents with HFSE enrichment.In the primitive mantle-normalized trace element spider diagram,Nb-enriched basalts show weakly negative(sometime positive) Nb,Ta anomalies.The primitive mantle-normalized La/Nb ratios of the Nb-enriched basalts are smaller than 2(but smaller than 0.7,occasionally).It is derived from the partial melting of mantle peridotite metasomatized by slab melts.Since Nb-enriched basalts and adakites are the direct products of subducted oceanic slab,the characteristics of magma activity and interaction between slab melts and mantle wedge can be demonstrated by the studies of this association and the nature of the relative fluids and melts.
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