Crustal thickness estimation beneath the southern central Andes at 30°S and 36°S from S wave receiver function analysis

Details Crustal thickness estimation beneath the southern central Andes at 30°S and 36°S from S wave receiver function analysis Crustal thickness estimation beneath the southern central Andes at 30°S and 36°S from S wave receiver function analysis

Jul 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008geoji.174..249h&link_type=abstract

Geophysical Journal International, Volume 174, Issue 3, pp. 249-254.

Astronomy and Astrophysics

Astronomy

9

Body Waves, Subduction Zone Processes, Dynamics Of Lithosphere And Mantle, Crustal Structure, South America

Scientific paper

We have used the S wave receiver function (SRF) technique to investigate the crustal thickness beneath two seismic profiles from the CHARGE project in the southern central Andes. A previous study employing the P wave receiver function method has observed the Moho interface beneath much of the profiles. They found, however, that the amplitude of the P to S conversion was diminished in the western part of the profiles and have attributed it to a reduction of the impedance contrast at the Moho due to lower crustal ecologitization. With SRF, we have successfully detected S to P converted waves from the Moho as well as possible conversions from other lithospheric boundaries. The continental South American crust reaches its maximum thickness of ~70 km (along 30°S between 70°W and 68.5°W) beneath the Principal Cordillera and the Famatina system and becomes thinner towards the Sierras Pampeanas with a thickness of ~40 km. Negative phases, possibly related to the base of the continental and oceanic lithosphere, can be recognized in the summation traces at different depths. By comparing our results with data obtained from previous investigations, we are able to further constrain the thickness of the crust and lithosphere beneath the central Andes.

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