Fig. 1From: On the detection of the Wilkes Land impact craterThe values of gravity disturbances Δg (mGal) for the whole Antarctica. The Wilkes Land (WL) anomaly (between longitudes 100 and 130°E, geodetic latitudes 60 and 75°S) is clearly visible as a semicircular feature with positive anomaly in its center and flanking negative semiring anomaly around, namely from southern directions. For more details see Figs. 7, 8, 9, 10, 11 and 12Back to article page