I. Okiyi, S. Ibeneme, E. Obiora, S. Onyekuru, A. I. Selemo, M. Olorunfemi
{"title":"尼日利亚东南部沉积盆地部分地区地热能资源评价","authors":"I. Okiyi, S. Ibeneme, E. Obiora, S. Onyekuru, A. I. Selemo, M. Olorunfemi","doi":"10.4314/IJS.V23I1.17","DOIUrl":null,"url":null,"abstract":"Depth (CPD)), and estimate geothermal gradient and heat flow required for the evaluation of the geothermal resources of the study area. Results from spectral analysis showed depths to the top of the magnetic source ranging between 0.45 km and 1.90 km; centroid depths of 4 km 7.87 km and CPD of between 6.15 km and 14.19 km. The CPD were used to estimate geothermal gradients which ranged from 20.3°C/km to 50.0°C/km","PeriodicalId":13487,"journal":{"name":"Ife Journal of Science","volume":"262 3","pages":"195-211"},"PeriodicalIF":0.0000,"publicationDate":"2021-05-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Evaluation of geothermal energy resources in parts of southeastern sedimentary basin, Nigeria\",\"authors\":\"I. Okiyi, S. Ibeneme, E. Obiora, S. Onyekuru, A. I. Selemo, M. Olorunfemi\",\"doi\":\"10.4314/IJS.V23I1.17\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Depth (CPD)), and estimate geothermal gradient and heat flow required for the evaluation of the geothermal resources of the study area. Results from spectral analysis showed depths to the top of the magnetic source ranging between 0.45 km and 1.90 km; centroid depths of 4 km 7.87 km and CPD of between 6.15 km and 14.19 km. The CPD were used to estimate geothermal gradients which ranged from 20.3°C/km to 50.0°C/km\",\"PeriodicalId\":13487,\"journal\":{\"name\":\"Ife Journal of Science\",\"volume\":\"262 3\",\"pages\":\"195-211\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-05-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Ife Journal of Science\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4314/IJS.V23I1.17\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Ife Journal of Science","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4314/IJS.V23I1.17","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Evaluation of geothermal energy resources in parts of southeastern sedimentary basin, Nigeria
Depth (CPD)), and estimate geothermal gradient and heat flow required for the evaluation of the geothermal resources of the study area. Results from spectral analysis showed depths to the top of the magnetic source ranging between 0.45 km and 1.90 km; centroid depths of 4 km 7.87 km and CPD of between 6.15 km and 14.19 km. The CPD were used to estimate geothermal gradients which ranged from 20.3°C/km to 50.0°C/km