{"title":"新墨西哥州莱利附近渐新世基性岩脉的岩石学和几何特征——岩脉向北延伸至科罗拉多高原东南边缘的标志","authors":"M. I. Dimeo","doi":"10.56577/sm-2006.961","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":203318,"journal":{"name":"New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume","volume":"57 19","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2006-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Petrography and geometry of Oligocene mafic dikes near Riley, New Mexico-indications of northward dike propagation into southeastern margin of the Colorado Plateau\",\"authors\":\"M. I. Dimeo\",\"doi\":\"10.56577/sm-2006.961\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":203318,\"journal\":{\"name\":\"New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume\",\"volume\":\"57 19\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2006-04-21\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.56577/sm-2006.961\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"New Mexico Geological Society, 2006 Annual Spring Meeting, Proceedings Volume","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.56577/sm-2006.961","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Petrography and geometry of Oligocene mafic dikes near Riley, New Mexico-indications of northward dike propagation into southeastern margin of the Colorado Plateau