Identification of Diorite Intrusion Distribution Using Gravity, Geomagnetic, and Audio Magnetotellurics Methods

Journal article

S. Hikmahtiar, M. Wildan, B. Bayu, I. Iko, T. Tino
2015

Cite

APA Click to copy
Hikmahtiar, S., Wildan, M., Bayu, B., Iko, I., & Tino, T. (2015). Identification of Diorite Intrusion Distribution Using Gravity, Geomagnetic, and Audio Magnetotellurics Methods.

Chicago/Turabian Click to copy
Hikmahtiar, S., M. Wildan, B. Bayu, I. Iko, and T. Tino. “Identification of Diorite Intrusion Distribution Using Gravity, Geomagnetic, and Audio Magnetotellurics Methods” (2015).

MLA Click to copy
Hikmahtiar, S., et al. Identification of Diorite Intrusion Distribution Using Gravity, Geomagnetic, and Audio Magnetotellurics Methods. 2015.

BibTeX Click to copy

@article{s2015a,
  title = {Identification of Diorite Intrusion Distribution Using Gravity, Geomagnetic, and Audio Magnetotellurics Methods},
  year = {2015},
  author = {Hikmahtiar, S. and Wildan, M. and Bayu, B. and Iko, I. and Tino, T.}
}

Abstract

There are so many complex geological appearances having been discovered by professional Geoscientist in Bayat. Therefore, we conducted an integrated study with three methods, gravity, geomagnetic, and magnetotellurics in this area to identify the distribution of subsurface diorite intrusion by calculating the result of field measurement and correlating it with geological data. There is a controversy about how this lithology contact could be developed whether this subsurface unconformity was formed by stratigraphic or structural boundaries. Measurement of those three methods is used to reinforce each other. Density values derived from the measurement of the relative gravity values are strengthened by rock susceptibility and resistivity values through a magnetic method survey and magnetotellurics.