Konversi kedalaman dengan metode kue lapis (layer cake) di Zona Anomali kecepatan daerah X

Wahyu , Rah Kartiko (1997) Konversi kedalaman dengan metode kue lapis (layer cake) di Zona Anomali kecepatan daerah X. Undergraduate thesis, FMIPA UNDIP.

[img]PDF
Restricted to Repository staff only

1874Kb
[img]
Preview
PDF
16Kb
[img]
Preview
PDF
349Kb
[img]
Preview
PDF
500Kb
[img]
Preview
PDF
563Kb
[img]
Preview
PDF
582Kb
[img]
Preview
PDF
427Kb
[img]PDF
Restricted to Repository staff only

617Kb
[img]
Preview
PDF
325Kb
[img]
Preview
PDF
326Kb
[img]
Preview
PDF
542Kb

Abstract

Telah dilakukan penelitian mengenai anotnali kecepatan pada daerah "X" menggunakan metode Kue Lapis. Data yang diperlukan dalam penelitian ini adalah penampang seismik, data log den synthetic seismogram. Maksud peiiggunaan rnetode ini melakukan pem.bagian pada penampang seismik inenjadi 5 lapisan dad permukaan pengukuran sampai ke puncak forniasi yang dii-nginkan. Kemudian dilakukan intrepretasi untuk memperoleh peta waktu interval per lapisan. Langkah berikutnya menghitung kecepatan interval tiap lapisan pada masing-masing sumur dan harga-harganya diplotkan pada peta dasar untuk clibuat Peta Kecepatan Interval tiap lapisan. Selanjutnya dilakukan perhitungan kedaletman tiap lapisan pada masing-masing suinur dan harga-harganya diplotkan pada peta dasar untuk dibuat Peta Struktur Kedalaman tiap lapisan. Kemudian dilakukan analisa kecepatan pada daerah "X" tersebut. It had been about velocity anomaly for zones "X" make the Layer Cake Method. In this survey needs seismic section, well data, log data and synthetic seismogram. Means of this method is devide in sesimic section become 5 layers from datum to the top formation, it's needed and interpreted to yield Time Interval Map per layer. Then, it's computing interval velocity per layers for each wells and that values ploting in base map to make Interval Velocity Map per layers. Thereafter, to comput the depth per layers for each wells and values ploting in base map to make Depth Structure Map per layer. And then, it's analys velocity in that zone. This; document is Undip Institutional Repository Collection. The author(s) or copy ht owner(s) agree that UNDIP-IR may, without changing the content, translate the submission to any medium or format for the purpose of preservation. The author(s) or copyright owner(s) also agree that UNDIP-IR may keep more than one copy of this submission for purposes of security, back-up and preservation. ( http://eprints.undip.ac.id)

Item Type:Thesis (Undergraduate)
Subjects:Q Science > QC Physics
Divisions:Faculty of Science and Mathematics > Department of Physics
ID Code:30378
Deposited By:Mr UPT Perpus 1
Deposited On:28 Oct 2011 07:55
Last Modified:28 Oct 2011 07:55

Repository Staff Only: item control page