Identifikasi Batu Andesit dengan Metode Geolistrik menggunakan Konfigurasi Schlumberger 2D di Kecamatan Pengaron,  Kabupaten Banjar Provinsi Kalimantan Selatan

Simamora, Selvy Tiurma; Wahyono, Sri Cahyo; Siregar, Simon Sadok

dc.contributor.author	Simamora, Selvy Tiurma
dc.contributor.author	Wahyono, Sri Cahyo
dc.contributor.author	Siregar, Simon Sadok
dc.date.accessioned	2022-04-26T03:34:29Z
dc.date.available	2022-04-26T03:34:29Z
dc.date.issued	2015-10-05
dc.identifier.issn	978-623-7533-39-9
dc.identifier.uri	https://repo-dosen.ulm.ac.id//handle/123456789/23928
dc.description.abstract	ABSTRACT- Identification of andesite stone layers research has been carried out using the Schlumberger configuration geoelectric 2D method in Pengaron District, Banjar District, South Kalimantan Province. Measurements were made of five lines with a length of 270 m. The research objective is to model 2D cross sections, determine the type of lithology and depth and thickness of andesite in the study area. Based on the results of research data found three layers namely top soil (gravel), Clay and andesite rocks with resistivty values 39.0–1000 Ωm were indicated as clay, gravel and andesite spread almost dise all tracks with a thickness of 10–86 m and depth of andesite are at a depth of 10–55 m.	en_US
dc.language.iso	en	en_US
dc.publisher	'Lambung Mangkurat University Press	en_US
dc.subject	2D geoelectric method; Andesite Stone; Pengaron; Resistivity.	en_US
dc.title	Identifikasi Batu Andesit dengan Metode Geolistrik menggunakan Konfigurasi Schlumberger 2D di Kecamatan Pengaron, Kabupaten Banjar Provinsi Kalimantan Selatan	en_US
dc.type	Article	en_US