English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

* Corresponding author : intan.manyoe@ung.ac.id Tel.:+6281280023410 Received: May 29, 2020; Accepted: Jun 18, 20 DOI 10.25299/jgeet.2020.5.2.5094  Abstract Volcano­tectonic events in Libungo can be the cause of the presence of geothermal potential. There is no detailed research on shallow subsurface conditions in Libungo that can show the distribution of shallow subsurface model of the Libungo geothermal area based on resistivity data. Resistivity data collection was carried ou in the Libungo hot springs area. The electrode configuration used is the Schlum values is calculated using current data, potential difference data and geometry factors. The results of the calculation of th resistivity values variation are plotted versus depth. Variations of resistivi of a single log, lithology distribution and 3D lithology model. The results showed that the shallow subsurface of the Libungo geothermal area was composed of andesite, volcanic breccia, silty clay and cl values ranging from 320 ­ 349 Ωm, has slightly fracture and is andesite dry. Volcanic breccia has a resistivity value of 177 Ωm, has a well to slightly fracture and is a volcanic breccia moist. to moist silty clay. Clay has resistivity values in the range 1.56 shallow subsurface area occurs in volcanic breccia, silty clay and clay. northern part of the Libungo geothermal area.

Subsurface Shallow Modelling Based on Resistivity Data in The Hot Springs Area of Libungo Geothermal, Gorontalo