?url_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rft.title=ANALISIS+SIFAT+PETROFISIKA+BATUAN+MENGGUNAKAN%0D%0AMETODE+MULTIMINERAL+PROBABILISTIK+UNTUK%0D%0AKARAKTERISASI+RESERVOAR+PADA+SUMUR+A-1+DAN+A-2%0D%0ALAPANGAN+X%2C+CEKUNGAN+BONAPARTE&rft.creator=Alicya+Inmas+Mauladika%2C+1315051005&rft.subject=Teknologi+(General)&rft.description=%0D%0ASalah+satu+wilayah+di+Indonesia+yang+memiliki+sumber+daya+minyak+dan+gas+bumi+adalah+daerah+timur+Indonesia+yaitu+pada+Cekungan+Bonaparte.+Cekungan+Bonaparte+terletak+diantara+paparan+kontingen+Australia+dengan+paparan+Eurasia+(Sundaland).+Eksplorasi+minyak+dan+gas+bumi+dapat+dilakukan+dengan+menggunakan+salah+satu+metode+geofisika+yaitu+metode+Well+Logging.+Pada+penelitian+ini+dilakukan+analisis+petrofisika+secara+kualitatif+dan+kuantitatif+terhadap+data+yang+telah+diambil+dengan+menggunakan+metode+Well+Logging+pada+sumur+A-1+dan+A-2+yang+terletak+di+lapangan+X%2C+Cekungan+Bonaparte.+Analisis+kuantitatif+dilakukan+dengan+menggunakan+metode+Multimineral+Probabilistik+agar+mendapatkan+model+yang+mendekati+keadaan+bawah+permukaan+yang+sebenarnya.+Berdasarkan+analisis+kualitatif+pada+kedua+sumur%2C+jenis+litologi+batuan+adalah+batu+pasir%2C+kemudian+hidrokarbon+pengisinya+adalah+gas.+Untuk+sumur+A-1+terdapat+3+zona+prospek+dan+sumur+A-2+terdapat+3+zona+prospek.+Selanjutnya%2C+berdasarkan+analisis+kuantitatif%2C+pada+sumur+A-1+nilai+VClay+adalah+sebesar+32.5%25%2C+nilai+porositas+efektif+rata-rata+sebesar+9.6%25%2C+nilai+Sw+rata-rata+sebesar+15.4%25+dan+nilai+K+rata-rata+sebesar+2.13+md.+Kemudian+pada+sumur+A-2%2C+nilai+VClay+adalah+sebesar+34.3%25%2C+nilai+porositas+efektif+rata-rata+sebesar+7%25%2C+nilai+Sw+rata-rata+sebesar+63%25+dan+nilai+K+rata-rata+sebesar+1.1+md.+Nilai-nilai+parameter+tersebut+selanjutnya+digunakan+untuk+mencari+nilai+netpay.+Nilai+netpay+pada+sumur+A-1+lebih+besar+yaitu+75.59+meter+sedangkan+pada+sumur+A-2+adalah+40.84+meter.+%0D%0A%0D%0AKata+kunci%3A+well+logging%2C+multimineral%2C+vclay%2C+porositas+efektif%2C+netpay+%0D%0A%0D%0A%0D%0AABSTRACT%0D%0A%0D%0A%0D%0A%0D%0AOne+of+Indonesia%E2%80%99s+areas+that+has+oil+and+gas+resource+is+Bonaparte+Basin.+The+location+of+Bonaparte+Basin+is+between+Australia+Continent+and+Eurasia+Continent+(Sundaland).+Oil+and+gas+can+be+explored+use+geophysical+methods+such+as+well+logging.+This+research+has+done+qualitative+and+quatitative+analysis+of+well+log+on+A-1+Well+and+A-2+Well%2C+X+Field%2C+Bonaparte+Basin.+Quantitative+analysis+has+done+used+multimineral+probabilistic+method+to+get+the+subsurface+model+that+close+with+actual+condition.+Based+on+qualitative+analysis+of+both+wells%2C+the+lithology+type+is+sandstone+and+the+hidrocarbon+content+is+gas.+There+are+3+prospect+zones+in+A-1+Well+and+2+prospect+zones+in+A-2+Well.+Next%2C+based+on+quantitative+analysis%2C+in+A-1+Well%2C+VClay+value+is+32.5%25%2C+porosity+effective+average+value+is+9.6%25%2C+Sw+average+value+is+15.4%25+and+K+average+value+is+2.13+md.+Then%2C+on+A-2+Well%2C+VClay+value+is+34.3%25%2C+porosity+effective+average+value+is+7+%25%2C+Sw+average+value+is+63%25+and+K+value+is+1.1+md.+Those+parameter+values+are+used+to+find+the+netpay+value.+Netpay+value+in+A-1+Well+is+larger+than+A-2+Well%2C+that+is+75.59+meters+while+in+well+A-2+is+40.84+meters.%0D%0AKeyword%3A+well+logging%2C+multimineral%2C+vclay%2C+multimineral%2C+effective+porosity%2C++netpay+%0D%0A&rft.publisher=UNIVERSITAS+LAMPUNG&rft.date=2018-02-07&rft.type=Skripsi&rft.type=NonPeerReviewed&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F30553%2F1%2FABSTRAK.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F30553%2F2%2FSKRIPSI%2520FULL.pdf&rft.format=text&rft.identifier=http%3A%2F%2Fdigilib.unila.ac.id%2F30553%2F3%2FSKRIPSI%2520TANPA%2520BAB%2520PEMBAHASAN.pdf&rft.identifier=++Alicya+Inmas+Mauladika%2C+1315051005++(2018)+ANALISIS+SIFAT+PETROFISIKA+BATUAN+MENGGUNAKAN+METODE+MULTIMINERAL+PROBABILISTIK+UNTUK+KARAKTERISASI+RESERVOAR+PADA+SUMUR+A-1+DAN+A-2+LAPANGAN+X%2C+CEKUNGAN+BONAPARTE.++UNIVERSITAS+LAMPUNG%2C+FAKULTAS+TEKNIK.+++++&rft.relation=http%3A%2F%2Fdigilib.unila.ac.id%2F30553%2F