Fig. 7: Maximum crustal thickness variation versus ridge segment length. | Nature Communications

Fig. 7: Maximum crustal thickness variation versus ridge segment length.

From: Seismic evidence for uniform crustal accretion along slow-spreading ridges in the equatorial Atlantic Ocean

Fig. 7: Maximum crustal thickness variation versus ridge segment length.The alternative text for this image may have been generated using AI.

Maximum crustal thickness variation between centres and ends of second-order ridge segments versus the length of the corresponding first-order ridge segment in the Atlantic Ocean. The crustal thickness constrained by both active-source seismic data and gravity data is included. The blue squares show results from this study for the equatorial Atlantic. Data sources are given in Supplementary Table 3.

Back to article page