Probabilistic longevity estimate for the Lusi mud volcano, East Java
Probabilistic longevity estimate for the Lusi mud volcano, East Java
Journal of the Geological Society of London (March 2011) 168 (2): 517-523
- Asia
- carbonates
- clastic sediments
- depth
- exploration
- Far East
- geologic hazards
- Indonesia
- Java
- mass movements
- mud
- mud volcanoes
- mudflows
- natural hazards
- new methods
- porosity
- pressure
- probability
- rates
- risk assessment
- sediments
- statistical analysis
- subsidence
- thickness
- East Java
- Prupuh Formation
- Lusi mud volcano
- Upper Kalibeng Formation
A new method for estimating the duration of a mud volcano eruption is applied to the Lusi mud volcano in East Java. The estimate is based upon carbonates at depths in the range 2500-3500 m being the water source, with an estimated area of 100-600 km (super 2) , thickness of 0.2-1.0 km, porosity of 0.15-0.25, an initial pressure between 13.9 and 17.6 MPa, and a separate, shallower source of mud (c. 1200-1800 m depth). The resulting 50 percentile for the time it takes for flow to decline to <0.1 Ml day (super -1) is 26 years. By analogy with natural mud volcanoes it can be expected to continue to flow at lower rates for thousands of years. Assuming subsidence rates of between 1 and 5 cm day (super -1) , land surface subsidence of between c. 95 and c. 475 m can be expected to develop within the 26 year time period.