dc.contributor.author | Siti Erisa Dwi Jaya | |
dc.date.accessioned | 2014-01-20T05:55:39Z | |
dc.date.available | 2014-01-20T05:55:39Z | |
dc.date.issued | 2014-01-20 | |
dc.identifier.nim | NIM071810201104 | |
dc.identifier.uri | http://repository.unej.ac.id/handle/123456789/18301 | |
dc.description.abstract | he Research was done in Pakauman, which is at Grujukan, Bondowoso Subprovince
interpreting subsurface megalithic site condition with 2D resistivity geoelectric. This
research was done by using Wenner Schlumberger configuration which has good
resolution either horizontal or vertical. The proccess of observation data used
software Res2Dinv. It gain caused the resistibility distribution contour layer of
subsurface megalithic site. The resistivity value has ranged among 100-200Ωm and
it was in 0.50-1.00 meter. This value based on tabel of resistivity which is
represented by Telford. The research gained, is a kind of andesit rock that is the part
of megalithic site. The result of this research is geoelectrical resistivity 2D method
applicables for knowing part of megalithic site which is assumed that buried in
subsurface area.
, geoelectrical resistivity 2D, Andecite rock | en_US |
dc.language.iso | other | en_US |
dc.relation.ispartofseries | 071810201104; | |
dc.subject | PERMUKAAN SITUS MEGALITIKUM | en_US |
dc.title | INTERPRETASI BAWAH PERMUKAAN SITUS MEGALITIKUM DI BONDOWOSO DENGAN MENGGUNAKAN METODE GEOLISTRIK RESISTIVITAS 2D | en_US |
dc.type | Other | en_US |