{"title":"由地球自转惯性力和软流层反作用力引起的岩石圈地球动力学的力学-数学模型,变形稳定性损失","authors":"","doi":"10.15372/fpvgn2019060108","DOIUrl":null,"url":null,"abstract":"","PeriodicalId":196311,"journal":{"name":"Фундаментальные и прикладные вопросы горных наук","volume":"37 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"MECHANICAL-MATHEMATICAL MODEL OF LITHOSPHERIC GEODYNAMICS CAUSED BY INERTIAL FORCES OF THE EARTH ROTATION AND REACTION FORCES OF ASTHENOSPHERIC LAYER, LOSS OF DEFORMATION STABILITY\",\"authors\":\"\",\"doi\":\"10.15372/fpvgn2019060108\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\",\"PeriodicalId\":196311,\"journal\":{\"name\":\"Фундаментальные и прикладные вопросы горных наук\",\"volume\":\"37 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/fpvgn2019060108\",\"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/fpvgn2019060108","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
MECHANICAL-MATHEMATICAL MODEL OF LITHOSPHERIC GEODYNAMICS CAUSED BY INERTIAL FORCES OF THE EARTH ROTATION AND REACTION FORCES OF ASTHENOSPHERIC LAYER, LOSS OF DEFORMATION STABILITY