{"title":"从特拉华盆地、德克萨斯州西部和新墨西哥州东南部的段间地温梯度全盆地图推断深埋元古代基底侵入岩的控制","authors":"Chesney Petkovsek, Paul Mann, A. Pepper","doi":"10.1190/image2022-3751854.1","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":341517,"journal":{"name":"Second International Meeting for Applied Geoscience & Energy","volume":"26 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-08-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Control of deeply-buried Proterozoic basement intrusive rocks inferred from a basin-wide maps of interval-specific geothermal gradient, Delaware Basin, west Texas, and southeastern New Mexico\",\"authors\":\"Chesney Petkovsek, Paul Mann, A. Pepper\",\"doi\":\"10.1190/image2022-3751854.1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":341517,\"journal\":{\"name\":\"Second International Meeting for Applied Geoscience & Energy\",\"volume\":\"26 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-08-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Second International Meeting for Applied Geoscience & Energy\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1190/image2022-3751854.1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Second International Meeting for Applied Geoscience & Energy","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1190/image2022-3751854.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Control of deeply-buried Proterozoic basement intrusive rocks inferred from a basin-wide maps of interval-specific geothermal gradient, Delaware Basin, west Texas, and southeastern New Mexico