{"title":"意大利风成火山弧下地壳岩浆储层的岩浆上升速率和深度:从捕虏体中的流体和熔体包裹体推断","authors":"M. Frezzotti, A. Peccerillo, Rossana Bonelli","doi":"10.1016/S1871-644X(03)80030-X","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":333257,"journal":{"name":"Developments in Volcanology","volume":"113 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"16","resultStr":"{\"title\":\"Magma ascent rates and depths of crustal magma reservoirs beneath the Aeolian volcanic Arc (Italy): Inferences from fluid and melt inclusions in xenoliths\",\"authors\":\"M. Frezzotti, A. Peccerillo, Rossana Bonelli\",\"doi\":\"10.1016/S1871-644X(03)80030-X\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":333257,\"journal\":{\"name\":\"Developments in Volcanology\",\"volume\":\"113 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"16\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Developments in Volcanology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1016/S1871-644X(03)80030-X\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Developments in Volcanology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1016/S1871-644X(03)80030-X","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Magma ascent rates and depths of crustal magma reservoirs beneath the Aeolian volcanic Arc (Italy): Inferences from fluid and melt inclusions in xenoliths