{"title":"利用自电位和水平视电阻率测量确定格立克地区宗古尔达克硬煤盆地的不连续面","authors":"Ibrahim Onur , Fethi Ergüder","doi":"10.1016/0167-9031(90)90933-J","DOIUrl":null,"url":null,"abstract":"<div><p>Self Potential (SP) and horizontal apparent resistivity measurements were made along a NW-SE oriented line perpendicular to the surface trace of the discontinuity in the Gelik District of the Zonguldak Coal Field. The dip angles and locations of the lateral discontinuities in the survey area were found by interpreting the SP and resistivity anomalies. Also, the boundary between Cretaceous and Carboniferous strata was determined and a cross-section along the NW-SE line was constructed.</p></div>","PeriodicalId":100929,"journal":{"name":"Mining Science and Technology","volume":"11 3","pages":"Pages 245-252"},"PeriodicalIF":0.0000,"publicationDate":"1990-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0167-9031(90)90933-J","citationCount":"0","resultStr":"{\"title\":\"Determination of discontinuities using self potential and horizontal apparent resistivity measurements in the Zonguldak Hardcoal Basin, Gelik District\",\"authors\":\"Ibrahim Onur , Fethi Ergüder\",\"doi\":\"10.1016/0167-9031(90)90933-J\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Self Potential (SP) and horizontal apparent resistivity measurements were made along a NW-SE oriented line perpendicular to the surface trace of the discontinuity in the Gelik District of the Zonguldak Coal Field. The dip angles and locations of the lateral discontinuities in the survey area were found by interpreting the SP and resistivity anomalies. Also, the boundary between Cretaceous and Carboniferous strata was determined and a cross-section along the NW-SE line was constructed.</p></div>\",\"PeriodicalId\":100929,\"journal\":{\"name\":\"Mining Science and Technology\",\"volume\":\"11 3\",\"pages\":\"Pages 245-252\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1990-11-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0167-9031(90)90933-J\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Mining Science and Technology\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/016790319090933J\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mining Science and Technology","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016790319090933J","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Determination of discontinuities using self potential and horizontal apparent resistivity measurements in the Zonguldak Hardcoal Basin, Gelik District
Self Potential (SP) and horizontal apparent resistivity measurements were made along a NW-SE oriented line perpendicular to the surface trace of the discontinuity in the Gelik District of the Zonguldak Coal Field. The dip angles and locations of the lateral discontinuities in the survey area were found by interpreting the SP and resistivity anomalies. Also, the boundary between Cretaceous and Carboniferous strata was determined and a cross-section along the NW-SE line was constructed.
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