Estimasi Ukuran Bulir Mineral Magnetik pada Batuan Peridotit Berdasarkan Peluruhan Anhysteretic Remanent Magnetization (ARM)

Rina Reida, Sudarningsih Sudarningsih, Totok Wianto

Abstract


A decaying measurement of Anhysteretic Remanent Magnetization
(ARM) has been undertaken to estimation the grain size of magnetic mineral
which carries remanent on peridotite igneous rocks. The samples are taken from
Desa Aranio, Kabupaten Banjar, South Kalimantan. The samples are taken in a
cylinder from with the diameter 2.54 cm and 2.2 cm in length by using Drill Model
D026-C. The giving, measuring and decaying process of ARM is done by
Molspin AF Demagnetizer, partial Anhysteretic Remanent Magnetization
(pARM), and Minispin Magnetometer. The estimation of grain size of magnetic
mineral is obtained by seeing ARM intensity decaying curve towards magnetic
field shown by the samples of peridotite igneous rocks. The ARM intensity
decaying curve show that the estimated peridotite rocks in research are
dominated by multidomain and the size are big, whereas the distribution of the
grain size is larger than 200 μm.

Keywords


peridotit, Anhysteretic Remanent Magnetization (ARM), magnetic grain size, multidomain

Full Text:

PDF


DOI: http://dx.doi.org/10.20527/flux.v6i2.3062

Article Metrics

Abstract view : 593 times
PDF - 7020 times

Refbacks

  • There are currently no refbacks.


Copyright (c) 2017 Jurnal Fisika FlUX

Creative Commons License
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

Association with:

Physical Society of Indonesia

Indexed by:

 

Creative Commons License
Jurnal Fisika FLux: Jurnal Ilmiah FMIPA Universitas Lambung Mangkurat is licensed under a Creative Commons Attribution-NoDerivatives 4.0 International License.