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Fig. A.1. | Earth, Planets and Space

Fig. A.1.

From: Three-dimensional gravity modeling of Chicxulub Crater structure, constrained with marine seismic data and land boreholes

Fig. A.1.

Error bars for the bottom depth estimation of every layer. Those were obtained by perturbing density contrast by 5%. Procedure consisted in perturbing a single density at the time and storing separately the depth perturbation for every layer. After perturbing all density contrasts, e.g. we added all depth perturbations for Tertiary and doing a depth average for every prism. Contours are every 0.1 km, except bottom melt with 0.01 km interval.

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