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Basement structure, lighology and permeability at Kawerau and Ohaaki geothermal fields, New Zealand


Publisher
Elsevier Science
Year
2002
Weight
354 KB
Volume
43
Category
Article
ISSN
0140-6701

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Predicting subsidence at Wairakei and Oh
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A ®nite-element model coupling compaction and ¯uid ¯ow processes in porous materials has been applied to the subsidence bowls at Wairakei and Ohaaki geothermal ®elds to provide a basis for predicting subsidence. Most of the subsidence is due to slow drainage of relatively impermeable (H0.05±0.3 mD),