Mt 2
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The document discusses several geophysical surveys conducted in various locations, including: 1) A gravity survey in Central Java and MT/AMT surveys along the Rhine-Bresse Transform Zone. 2) An AMT survey at Mount Patuha volcano in Indonesia and 2D resistivity modeling of hot springs. 3) The subsurface structure and thermal zone of Guntur volcano in Indonesia based on seismic and resistivity data.
![Guntur Volcano Subsurface Structure & Thermal Zone 1 . 0 1 . 5 0 . 5 - 0 . 5 0 . 0 0 . 0 0 . 5 1 . 0 1 . 5 2 . 0 1 0 0 0 0 3 0 0 0 3 0 0 3 0 3 1 0 0 0 1 0 0 1 0 1 [ o h m - m ] R E F E R E N C E G. GUNTUR [+199..] 3.5 ~ 8.5 km (seismic data) Hydrothermal zone Heat conduction Volcanic body (lava & pyroclastic) Sta. Citiis [+1523 m] SOUTH-SOUTHWESTING [km] EASTING [km] 0 . 0 0 . 5 1 . 0 1 . 5 2 . 0 1 . 0 1 . 5 0 . 5 - 0 . 5 0 . 0 Magma chamber GN_01 GN_02 GN_03 CMK GN_05 GN_06 Heat conduction PTR_01 [+1446.3 m] PTR_02 PTR_06 PTR_05 PTR_03 PTR_04 PTR_07 PTR_08 PTR_09 PTR_10 Tiltmeter/Watertube Station](https://image.slidesharecdn.com/mt-2-1206697462252900-5/85/Mt-2-9-320.jpg)
Mt 2
- 2. Central Java regional gravity
- 4. MT and AMT survey Rhine – Bresse Transform Zone
- 5. MT and AMT survey Rhine – Bresse Transform Zone
- 6. AMT survey at Cimanggu (Mt. Patuha)
- 7. 2-D resistivity section from 1-D smooth-modelling hot-spring hot-spring
- 8. 2-D resistivity section from 2-D smooth-modelling hot-spring hot-spring
- 9. Guntur Volcano Subsurface Structure & Thermal Zone 1 . 0 1 . 5 0 . 5 - 0 . 5 0 . 0 0 . 0 0 . 5 1 . 0 1 . 5 2 . 0 1 0 0 0 0 3 0 0 0 3 0 0 3 0 3 1 0 0 0 1 0 0 1 0 1 [ o h m - m ] R E F E R E N C E G. GUNTUR [+199..] 3.5 ~ 8.5 km (seismic data) Hydrothermal zone Heat conduction Volcanic body (lava & pyroclastic) Sta. Citiis [+1523 m] SOUTH-SOUTHWESTING [km] EASTING [km] 0 . 0 0 . 5 1 . 0 1 . 5 2 . 0 1 . 0 1 . 5 0 . 5 - 0 . 5 0 . 0 Magma chamber GN_01 GN_02 GN_03 CMK GN_05 GN_06 Heat conduction PTR_01 [+1446.3 m] PTR_02 PTR_06 PTR_05 PTR_03 PTR_04 PTR_07 PTR_08 PTR_09 PTR_10 Tiltmeter/Watertube Station
- 10. 2-D and 3-D interpretation of MT data in the Bajawa geothermal field Flores, Indonesia (Uchida et al, 2002)
- 12. MT World-wide
- 13. mapping frontier areas on a reconnaissance basis to delineate specific prospects for more expensive seismic detailing complementing seismic interpretation with additional structural or lithological information replacing seismic in difficult environments, i.e. in basins where productive sediments are overlain by thick basalts or volcanic sediments. Expected MT contributions in oil exploration