{"title":"基于地质约束的火山深部地热离散裂缝网络建模工作流程","authors":"J. Joonnekindt, A. Levannier","doi":"10.3997/2214-4609.202182028","DOIUrl":null,"url":null,"abstract":"Summary In this study, we propose a forward DFN modeling workflow to produce realistic fracture networks in volcanic environments for subsequent geothermal resource assessment. The DFN modeling uses geological constraints to drive the fracture distribution and characteristics. The work is illustrated using a simple synthetic model, although similar approaches have been used in the case of real projects. The fracture model parameters are presented together with the modeling results for each fracture sets. In particular, the host formation is deformed by the intrusion emplacement and fractures representing the layers folding, the intrusion pressure mechanical effect and the thermal cooling effect. Additional fractures have been added in relation to the fault slipping and the fault damage zone.","PeriodicalId":147283,"journal":{"name":"First EAGE Workshop on Geothermal Energy in Latin America","volume":"46 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-08-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Discrete Fracture Network modeling workflow using geological constraints for deep geothermal in volcanic context\",\"authors\":\"J. Joonnekindt, A. Levannier\",\"doi\":\"10.3997/2214-4609.202182028\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Summary In this study, we propose a forward DFN modeling workflow to produce realistic fracture networks in volcanic environments for subsequent geothermal resource assessment. The DFN modeling uses geological constraints to drive the fracture distribution and characteristics. The work is illustrated using a simple synthetic model, although similar approaches have been used in the case of real projects. The fracture model parameters are presented together with the modeling results for each fracture sets. In particular, the host formation is deformed by the intrusion emplacement and fractures representing the layers folding, the intrusion pressure mechanical effect and the thermal cooling effect. Additional fractures have been added in relation to the fault slipping and the fault damage zone.\",\"PeriodicalId\":147283,\"journal\":{\"name\":\"First EAGE Workshop on Geothermal Energy in Latin America\",\"volume\":\"46 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-08-19\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"First EAGE Workshop on Geothermal Energy in Latin America\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.3997/2214-4609.202182028\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"First EAGE Workshop on Geothermal Energy in Latin America","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.202182028","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Discrete Fracture Network modeling workflow using geological constraints for deep geothermal in volcanic context
Summary In this study, we propose a forward DFN modeling workflow to produce realistic fracture networks in volcanic environments for subsequent geothermal resource assessment. The DFN modeling uses geological constraints to drive the fracture distribution and characteristics. The work is illustrated using a simple synthetic model, although similar approaches have been used in the case of real projects. The fracture model parameters are presented together with the modeling results for each fracture sets. In particular, the host formation is deformed by the intrusion emplacement and fractures representing the layers folding, the intrusion pressure mechanical effect and the thermal cooling effect. Additional fractures have been added in relation to the fault slipping and the fault damage zone.