Rrb. Von Frese et al., Antarctic crustal modeling from the spectral correlation of free-air gravity anomalies with the terrain, J GEO R-SOL, 104(B11), 1999, pp. 25275-25296
We investigated the use of enhanced spectral correlation theory for modelin
g the crustal features of the Antarctic from regional observations of gravi
ty and terrain. The analysis considered 1 degrees-gridded free-air gravity
anomalies and topographic rock, ice, and water components for the region so
uth of 60 degrees S. We modeled terrain gravity effects at 150-km altitude
by Gauss-Legendre quadrature (GLQ) integration assuming densities of 2800 k
g/m(3) for rock, 900 kg/m(3) for ice, and 1030 kg/m(3) for seawater. These
effects are substantial relative to the free-air anomalies and must be comp
ensated by the effects of subsurface density variations. Significant terrai
n-correlated free-air anomalies were revealed by the wavenumber correlation
spectrum between the free-air anomalies and the modeled terrain gravity ef
fects, which we interpreted mostly to reflect possible isostatic imbalances
of the crust. Subtracting the terrain-correlated free-air anomalies from t
he total free-air anomalies and topographic gravity effects yielded terrain
-decorrelated free-air anomalies and the gravity effects of isostatically c
ompensated terrain features, respectively, which are uncorrelated with each
other. The compensating effects that annihilate the latter were attributed
to undulations of the Moho, which we estimated by inversion using GLQ inte
gration and a mantle-to-crust density contrast of 400 kg/m(3) The inversion
produced a Moho map with nearly 40 km of total relief that agrees very wel
l with deep seismic refraction soundings. For East Antarctica, a bimodal va
riation in crustal thickness was found: the crustal wedge between the easte
rn Weddell Sea (similar or equal to 330 degrees E) and the eastern flank of
the Gamburtsev Subglacial Mountains (similar or equal to 90 degrees E) has
a mean thickness of about 37 km, whereas the mean crustal thickness is nea
r 32 km for the northern half of the rest of East Antarctica up to the west
ern flank of the Transantarctic Mountains (similar or equal to 150 degrees
E). For West Antarctica and the oceanic regions, mean crustal thicknesses o
f about 30 km and 14 km, respectively, are inferred. The terrain-decorrelat
ed free-air anomalies may be related to long-wavelength, large-amplitude su
bcrustal density variations and to much shorter-wavelength, smaller-amplitu
de intracrustal density variations.