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During the Voltaire cruise more than 1260 km of CHIRP data have been acquired, for more than 149 hours. These data were used to survey the coring site VC-1 (actually sampled by the cores ST-1 and ST-2) and the potential coring site VC-2, both along the seismic line BS-07A (Fig. 13). Fig. 14 shows the location of all lines acquired. Fig. 15 and Fig. 16 show the location of the two coring sites in respect to bathymetry.
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Figure 13:
line BS07A, acquired during the survey BIGSETS in 1998, showing the location of coring site VC-1 (VOL01) and the potential VC-2 (VOL02).
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Figure 14:
overall of total CHIRP acquisition.
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Figure 15:
location of the coring site VC-1 and bathymetry of the area.
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Figure 16:
location of the coring site VC-2 and bathymetry of the area.
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Figure 17:
location of coring site VC-1, stations 1 and 2 along the corresponding CHIRP profile.
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Figure 18:
location of the potential coring site VC-2, along the corresponding CHIRP profile.
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Some of the CHIRP lines provided also excellent images of different geological features:
- 1.
- A mud volcano (Fig. 19).
- 2.
- A possible gas pocket (Fig. 20).
- 3.
- One active fault south of Albufeira (Fig. 21).
- 4.
- Beautiful images of actual sea-bottom erosion at 54x vertical exaggeration (Fig. 22).
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Figure 19:
example of mud volcanoes, recorded during CHIRP acquisition.
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Figure 20:
example of possible gas pocket, recorded during CHIRP acquisition.
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Figure 21:
the Albufeira fault, recorded during CHIRP acquisition.
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Figure 22:
examples of sea-bottom erosion.
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2003-01-21