Figure 4. Interpretation of Conrad 823 profile across the Eastern Alboran Basin, showing the two negative flower structures at both sides of the Al-Mansour Seamount. Two markedly different reflective characters of the Upper Miocene to Holocene sediments are separated by the M-reflector (M). Within the Pliocene-Holocene sediments, other unconformities form as a result of active tectonics during this time. s.p. = shotpoints. Location in Figure 2.

Figure 4. Interpretation of Conrad 823 profile across the Eastern Alboran Basin, showing the two negative flower structures at both sides of the Al-Mansour Seamount. Two markedly different reflective characters of the Upper Miocene to Holocene sediments are separated by the M-reflector (M). Within the Pliocene-Holocene sediments, other unconformities form as a result of active tectonics during this time. s.p. = shotpoints. Location in Figure 2.