{"title":"塔什塔戈和谢勒盖什矿床分段开采条件下采场边缘部分岩爆危险区的确定","authors":"A. Konurin, V. Shtirts, E. Khristolyubov","doi":"10.15372/fpvgn2020070113","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":196311,"journal":{"name":"Фундаментальные и прикладные вопросы горных наук","volume":"80 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"DETERMINATION OF ROCKBURST-HAZARDOUS ZONES FROM THE EDGE PARTS OF THE STOPING AREA IN SUBLEVEL MINING SYSTEM UNDER CONDITIONS OF THE TASHTAGOL AND SHEREGESH DEPOSITS\",\"authors\":\"A. Konurin, V. Shtirts, E. Khristolyubov\",\"doi\":\"10.15372/fpvgn2020070113\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":196311,\"journal\":{\"name\":\"Фундаментальные и прикладные вопросы горных наук\",\"volume\":\"80 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\":\"Фундаментальные и прикладные вопросы горных наук\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.15372/fpvgn2020070113\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Фундаментальные и прикладные вопросы горных наук","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15372/fpvgn2020070113","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
DETERMINATION OF ROCKBURST-HAZARDOUS ZONES FROM THE EDGE PARTS OF THE STOPING AREA IN SUBLEVEL MINING SYSTEM UNDER CONDITIONS OF THE TASHTAGOL AND SHEREGESH DEPOSITS