?url_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rft.title=METODE+INDUKSI+POLARISASI+UNTUK+MENENTUKAN%0D%0APERSEBARAN+DAN+SUMBERDAYA+HIPOTETIK+ENDAPAN%0D%0ATIMAH+PRIMER+PADA+ZONA+INTRUSI+GRANIT+DAERAH%0D%0AGUNUNG+BATUBESI+BELITUNG+TIMUR&rft.creator=Agus+Priyono%2C+1215051002&rft.subject=600+Teknologi+(ilmu+terapan)&rft.description=Geoelectric+research+has+been+carried+out+to+determine+the+distribution%0D%0Aand+hypothetical+resources+of+primary+lead+deposits+in+the+granite+intrusion%0D%0Azone+of+the+East+Belitung+Mountain+Batubesi+area.+The+intrusion+zone+is%0D%0Aindicated+as+a+vein+and+determines+the+amount+of+hypothetical+lead%0D%0Aresources.+The+data+used+is+secondary+data%2C+consisting+of+20+tracks+that+are%0D%0Adivided+into+3+blocks+with+20+meters+of+track+spacing.+The+results+of+2D+and%0D%0A3D+interpretations+show+that+the+intrusion+zone+as+the+place+where+primary%0D%0Atin+is+accumulated+tends+to+lead+north+of+the+study+area.%0D%0AThe+research+area+has+resistivity+values+that+tend+to+vary+in+the+range+of%0D%0A100+-+50%2C000+%CE%BCm.+The+surface+layer+of+the+study+area+is+an+alluvial+layer+with%0D%0Alithology+in+the+form+of+keralal+sand+and+sandy+loam+with+a+resistivity+value%0D%0Arange+of+200+-+500+%CE%BCm.+Alleged+potential+of+vein+containing+lead+(kasiterit)%0D%0Aminerals+is+at+a+resistivity+value+of+700+-+10%2C000+%CE%A9m+and+a+chargebility+value%0D%0Aof+3+-+25+msec.+The+magnitude+of+the+hypothetical+resource+in+the+form+of%0D%0Athe+primary+tin+carrier+cassiterite+mineral+layer+in+the+study+area+is+%C2%B1%0D%0A24%2C000%2C000+m3.%0D%0AKeyword+%3A+Granit+Intrusion%2C+resistivity%2C+chargebiliy%2C+tin.%0D%0A%0D%0A%0D%0ATelah+dilakukan+penelitian+geolistrik+untuk+menentukan+persebaran+dan%0D%0Asumberdaya+hipotetik+endapan+timah+primer+pada+zona+intrusi+granit+daerah%0D%0AGunung+Batubesi+Belitung+Timur.+Zona+intrusi+yang+diindikasikan+sebagai%0D%0Avein+dan+menentukan+besarnya+sumberdaya+hipotetik+timah.+Data+yang%0D%0Adigunakan+merupakan+data+sekunder%2C+terdiri+dari+20+lintasan+yg+dibagi%0D%0Amenjadi+3+Blok+dengan+spasi+lintasan+20+meter.+Hasil+interpretasi+2D+dan+3D%0D%0Amenunjukkan+bahwa+zona+intrusi+sebagai+tempat+terakumulasinya+timah%0D%0Aprimer+cenderung+mengarah+ke+utara+daerah+penelitian.%0D%0ADaerah+penelitian+memiliki+nilai+resistivitas+yang+cenderung+variatif%0D%0Adengan+kisaran+100+%E2%80%93+50.000+%CE%A9m.+Lapisan+permukaan+daerah+penelitian%0D%0Amerupakan+lapisan+alluvial+dengan+litologi+berupa+pasir+kerakal+dan%0D%0Alempung+pasiran+dengan+kisaran+nilai+resistivitas+200+%E2%80%93+500+%CE%A9m.+Dugaan%0D%0Apotensi+vein+yang+mengandung+mineral+pembawa+timah+(kasiterit)+berada%0D%0Apada+nilai+resistivitas+700+%E2%80%93+10.000+%CE%A9m+dan+nilai+chargebilitas+3+%E2%80%93+25+msec.%0D%0ABesar+sumberdaya+hipotetik+berupa+lapisan+mineral+kasiterit+pembawa+timah%0D%0Aprimer+pada+daerah+penelitian+adalah+%C2%B124.000.000+m%0D%0A3%0D%0A.+Kata+kunci+%3A+Intrusi+granit%2C+resistivitas%2C+chargebilitas%2C+timah.%0D%0A&rft.publisher=Fakultas+Teknik&rft.date=2019-06-27&rft.type=Skripsi&rft.type=NonPeerReviewed&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F56604%2F1%2FABSTRAK.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F56604%2F2%2FSKRIPSI%2520FULL.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F56604%2F3%2FSKRIPSI%2520TANPA%2520BAB%2520%2520PEMBAHAHAN.pdf&rft.identifier=++Agus+Priyono%2C+1215051002++(2019)+METODE+INDUKSI+POLARISASI+UNTUK+MENENTUKAN+PERSEBARAN+DAN+SUMBERDAYA+HIPOTETIK+ENDAPAN+TIMAH+PRIMER+PADA+ZONA+INTRUSI+GRANIT+DAERAH+GUNUNG+BATUBESI+BELITUNG+TIMUR.++Fakultas+Teknik%2C+Universitas+Lampung.+++++&rft.relation=http%3A%2F%2Fdigilib.unila.ac.id%2F56604%2F