A. Buntoro, M. Nurcholis, B. Rahmad, A. H. Lukmana
{"title":"基于XRD分析的粘土成岩作用对井眼稳定性的影响——以印尼爪哇盆地东北部BJN-004井为例","authors":"A. Buntoro, M. Nurcholis, B. Rahmad, A. H. Lukmana","doi":"10.1063/5.0134883","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":433440,"journal":{"name":"4TH INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL AND ENERGY","volume":"241 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The impact of clay diagenesis on borehole stability based on XRD analysis: A case study of well BJN-004 in the North East Java basin area, Indonesia\",\"authors\":\"A. Buntoro, M. Nurcholis, B. Rahmad, A. H. Lukmana\",\"doi\":\"10.1063/5.0134883\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":433440,\"journal\":{\"name\":\"4TH INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL AND ENERGY\",\"volume\":\"241 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"4TH INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL AND ENERGY\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1063/5.0134883\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"4TH INTERNATIONAL CONFERENCE ON EARTH SCIENCE, MINERAL AND ENERGY","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1063/5.0134883","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}