?url_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rft.title=IDENTIFIKASI+STRUKTUR+BAWAH+PERMUKAAN+MENGGUNAKAN%0D%0AMETODE+MAGNETOTELLURIK+2D+DI+DAERAH+CEKUNGAN%0D%0ABINTUNI+SEBAGAI+POTENSI+HIDROKARBON&rft.creator=RIRIN+YULIANTI%2C+1315051050&rft.subject=Teknologi+(General)&rft.description=Penelitian+metode+Magnetotellurik+(MT)+dilakukan+pada+daerah+prospek%0D%0Ahirdokarbon+di+Cekungan+Bintuni%2C+Propinsi+Papua+Barat.+Penelitian+ini+bertujuan%0D%0Amengidentifikasi+struktur+bawah+permukaan+berdasarkan+penampang+resistivitas+2%0D%0Adimensi.+Proses+pengolahan+data+penelitian+ini+antara+lain%3B+(i)+proses+transformasi%0D%0Adata+dari+domain+waktu+ke+domain+frekuensi+dengan+trasformasi+Fourier.+(ii)%0D%0Aproses+filtering+dengan+robust%2C+dimana+robust+ini+terdiri+dari+tiga+jenis+yaitu%0D%0ARobust+No+Weight%2C+Robust+Rho+Variance+dan+Robust+Ordinary+Coherency.+(iii)%0D%0Aseleksi+XPR+dan+format+data+diubah+menjadi+EDI+file.+(iv)+inversi+untuk%0D%0Amendapatkan+model+penampang+resistivitas+2D.+Hasil+yang+didapatkan+pada%0D%0Apenelitian+ini+berdasarkan+penampang+resistivitas+2D+yaitu+pada+formasi+Klasafet%0D%0Amemiliki+nilai+resistivitas+yaitu+1+%E2%80%93+20+%CE%A9m+pada+kedalaman+0+hingga+1000+meter%0D%0Adi+bawah+permukaan+dengan+litologi+sebagai+batu+lempung+yang+diidentifikasikan%0D%0Asebagai+caprock%2C+pada+formasi+Kemblengan+nilai+resistivitas+20+%E2%80%93+90+%CE%A9m+pada%0D%0Akedalaman+3500+meter+di+bawah+permukaan+dengan+litologi+batu+pasir+gampingan%0D%0Ayang+diidentifikasikan+sebagai+reservoir%2C+pada+formasi+Kemum+nilai+resistivitas+20%0D%0A%E2%80%93+32+%CE%A9m+pada+kedalaman+6000+meter+di+bawah+permukaan+dengan+litologi+batu%0D%0Apasir+yang+diidentifikasikan+sebagai+basement.%0D%0AKata+Kunci+%3A+Hidrokarbon%2C+Magnetotellurik+2+dimensi%2C+Reservoir%0D%0A%0D%0A%0D%0A%0D%0AABSTRACT%0D%0A%0D%0AMagnetotelluric+research+was+done+in+hydrocarbon+prospect+area+of+Bintuni+basin%2C%0D%0AWest+Papua+province.+The+purpose+of+this+research+is+to+identificate+hydrocarbon%0D%0Aprospect+in+subsurface+structure+using+2D+resistivity+section.+Data+processing+step%0D%0Afor+the+research+are%3B+(i)+Data+transformation+from+time+domain+to+frequency%0D%0Adomain+using+Fourier+transformation.+(ii)+Filtering+process+using+Robust+No%0D%0AWeight%2C+Robust+Rho+Variance+and+Robust+Ordinary+Coherency.+(iii)+XPR%0D%0Aselection+and+formatting+data+into+EDI+file.+(iv)+2D+resistivity+section+modeling%0D%0Ausing+inversion.+The+result+of+this+research+based+on+2D+resistivity+section+in%0D%0AKlasafat+formation+have+resistivity+value+about+1+%E2%80%93+20+%CE%A9m.+From+0+until+1000%0D%0Ameter+below+the+surface+the+main+lithology+is+claystone+that+identified+as+caprock.%0D%0AKemblengan+formation+have+resistivity+value+about+20+%E2%80%93+90+%CE%A9m+in+3500+meter%0D%0Aunder+surface+with+main+lithology+lime-sandstone+and+identified+as+a+reservoir.%0D%0ATipuma+formation+have+resistivity+value+about+0.62+%E2%80%93+2+%CE%A9m+in+8000+meter+under%0D%0Asurface+with+main+lithology+claystone.+Kemun+formation+have+resistivity+value%0D%0Aabout+20+%E2%80%93+32+%CE%A9m+in+6000+meter+under+surface+with+main+lithology+sandstone+and%0D%0Aidentified+as+a+basement.%0D%0AKeywords%3A+2D+Magnetotelluric%2C+Hydrocarbon%2C+Reservoir.&rft.publisher=UNIVERSITAS+LAMPUNG&rft.date=2017-08-18&rft.type=Skripsi&rft.type=NonPeerReviewed&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F28329%2F1%2FABSTRAK.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F28329%2F2%2FSKRIPSI%2520FULL.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F28329%2F3%2FSKRIPSI%2520TANPA%2520BAB%2520PEMBAHASAN.pdf&rft.identifier=++RIRIN+YULIANTI%2C+1315051050++(2017)+IDENTIFIKASI+STRUKTUR+BAWAH+PERMUKAAN+MENGGUNAKAN+METODE+MAGNETOTELLURIK+2D+DI+DAERAH+CEKUNGAN+BINTUNI+SEBAGAI+POTENSI+HIDROKARBON.++UNIVERSITAS+LAMPUNG%2C+FAKULTAS+TEKNIK.+++++&rft.relation=http%3A%2F%2Fdigilib.unila.ac.id%2F28329%2F