Geothermal prospecting in the Semporna Peninsula with emphasis on the Tawau area

702001-101060-857-B
Author : Lim Peng Siong, Francis Intang & Chan Fook On
Publication : Bulletin of the Geological Society of Malaysia
Page : 135-155
Volume Number : 29
DOI : https://doi.org/10.7186/bgsm29199104

Bulletin of the Geological Society of Malaysia, Volume 29, July 1991, pp. 135 – 155

 

Geothermal prospecting in the Semporna Peninsula with emphasis on the Tawau area

LIM PENG SIONG, FRANCIS INTANG & CHAN FOOK ON

Geological Survey of Malaysia, Kota Kinabalu, Sabah

 

Abstract: Thermal manifestations in the Semporna Peninsula include hot springs, seepages, mud pools and old steaming ground. Mapping of these thermal features showed that they are structurally controlled.

The chemistry of the thermal waters indicate the presence of two types of waters - near neutral sodium chloride and sulphate waters. Thermal waters from the Apas Kiri area are near-neutral sodium chloride waters and the C1/B and C1/F ratios suggest they have a common source of geothermal fluid. The thermal water from upper Tawau is acid sulphate type and its chemistry suggests it is steam-heated water or ground water mixed with gas (H2S). The chemistry of thermal waters from Balung and Sungai Jepun areas suggests they are acid sulphate waters which may have come from a far away source and come into contact with and neutralised by cold ground water. The upper Tawau and Balung springs may indicate the perimeter of a field centered on the Maria Volcanic Complex.

The Apas Kiri area is underlain mainly by Quaternary dacitic lava, tuff and agglomerate. The surface thermal manifestations cover an area of 3 km2. The volcanic rocks are calcitised, chloritised, argillised and pyritised. Around the thermal features, the rocks are strongly argillised and calcitised.

Several characteristics of the Apas Kiri thermal waters e.g. chloride contents, C1/B ratio and geothermometer suggest high subsurface temperature. The C1/B ratio also suggests the reservoir rocks are andesitic.

Total heat loss from the Apas Kiri 2, Apas 5 and Sungai Jepun areas have been tentatively estimated as 28.65, 0.75 and 15.05 MW-Thermal respectively.

https://doi.org/10.7186/bgsm29199104