Rit (Vísindafélag Íslendinga) - 01.06.1971, Page 84

Rit (Vísindafélag Íslendinga) - 01.06.1971, Page 84
84 GUÐMUNDUR PÁLMASON Akranes-Hvalfjördur), while the station 63 (CP) is in the relatively high delay time area to the east of lake Thingvallavatn. The dif- ference in delay times hetween stations 63 (CP) and 64 is to be ex- pected from the difference in the structure overlying layer 3 under the two stations. The arrival times of the P3-wave (Báth’s P2-wave) at stations 12, 34 and 63 give an apparent P3-wave velocity of 6.52 km/sec. It may safely be assumed that all the more distant stations on profiles CP and WP record the P4-wave as the first arrival. Varia- tions in the P4-wave delay time are then probably due to variations in depth to layer 4 or to variations in the overlying structure. The delay time of the P4-wave at the shot point in Graenavatn is somewhat uncertain. The profile Graenavatn-Eyjafjöll indicates a value of ahout 1.09 sec, while profiles CP and WP indicate a value below 1.0 sec. If the delay time is assumed to be 1.0 sec, the depth to layer 4 at the shot point will be about 8.7 km. This is in good agree- ment with other results in SW-Iceland and it will therefore be as- sumed that the P4~wave delay time at Graenavatn is 1.0 sec. The following depths to layer 4 are then found under the profile WP, taking into account the overlying structure. Table 6.4. Station Distance km t - x/7.2 sec Delay time sec Depth km Shot point 0 1.00 8.7 102 101.72 1.96 0.96 9.5 165 164.60 2.37 1.37 15.6 206 206.21 2.24 1.24 13.4 253 253.44 2.12 1.12 14.0 The relatively sharp increase in depth to layer 4 between stations 102 and 165 is noteworthy. It occurs in an area where the depth to layer 3 is relatively great. Since there is still some uncertainty in the true value of the P4-wave velocity, there will he a corresponding un- certainty in absolute depths computed on the basis of delay times from unreversed profiles (cf. sect. 5.6). The main features of the depth variation will, however, not be changed when a more accurate value of P4-wave velocity has been found. The relatively great depth to layer 4, which is indicated ahove for the distant part of profile WP, should show up on the profile Vestur-
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