Rasimeng, Syamsurijal and Haerudin, Nandi and Harmen, Harmen (2007) Penentuan Lithologi Batuan Bawah Permukaan Menggunakan Metode Resistivitas Sounding di Daerah Prospek Geothermal Gunung Rajabasa. In: Seminar Nasional Hasil Penelitian dan Pengabdian Masyarakat Universitas Lampung 2007, September 2007, Bandar Lampung.

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Abstract

The Rajabasa is one of volcano strato with level of activity type B which located in province Lampung. Existence of fluid geothermal in north caster (Sukamandi and Kecapi), south caster (Kunjir and coast Wartawan) and south-east caster (Simpur) be form of desorption of temperature dissociation energy of diatomic pickings coming from within the mount body. The geothermal fluid comes from a source interpreted as magma chamber. Resistivity methods with configuraton schlumberger done to interpret lithology of rock around district manisfestation "Belerang Kering" (Sukamandi). Based on result of analysis obtained layer controlling fluid flow geothermal is high porosity rock layer so that loaded by fluid geothermal. The sandstone layer lays in various depth of 3-14 meter from surface. Besides lithologi rock also occupied by clay-tuff, gravel, and volcano deposit as top soil. While below sandstone layer there is rock layer which more compact (andesitic-basaltic?) as basement rock.

Item Type:	Conference or Workshop Item (Paper)
Subjects:	T Technology > TN Mining engineering. Metallurgy
Divisions:	Fakultas Teknik (FT) > Prodi Teknik Geofisika
Depositing User:	HARMEN
Date Deposited:	22 May 2023 01:06
Last Modified:	22 May 2023 01:06
URI:	http://repository.lppm.unila.ac.id/id/eprint/51931

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