GEOLOGI DAERAH PANAS BUMI ULUBELU TANGGAMUS, LAMPUNG UTARA BERDASARKAN ANALISIS METODE MAGNETOTELLURIK (MT)

Authors

  • Saultan Panjaitan Pusat Survei Geologi

DOI:

https://doi.org/10.33332/jgsm.geologi.v20i2.163

Abstract

Low resistivities of 0 – 15 Πm are interpreted as impermeable zones, functiming as cap rocks wich is hydrothermal alteration estimated to cinsist of clay. The midle resistivity 15 – 70 Πm is interpreted as permeable reservoir rocks located at 1250 – 2000 metres depth. The resistivity > 1000 Πm are metamorphic carbonate rocks. Block I in south of Mt.Rendingan and Block II at around Pagaralam hot spring formed up flow zone fluid reservoir having temperature of more than 260ºC, and contained 80 % vapour faction.


Keywords: Geothermal,resistivity, impermeable, cap rock, hydrothermal alteration

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References

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Published

2010-04-15

Issue

Vol. 20 No. 2 (2010): Jurnal Sumber Daya Geologi

Section

Article

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