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Typical Results

In the example of Figure 5, a set of Gulf of Mexico stations' measured heat flows are plotted as a frequency bar chart. A generally well-behaved (Gaussian-like) distribution is typically observed in such a set, with a few outliers that are considered anomalies. In this sample set, the values are generally lower than the corrected heat flows of 41-47 mW/m2 obtained by Nagihara et al (1996). This is expected due to the higher sedimentation rates in this part of the Gulf of Mexico basin.

Figure 5. Distribution of measured heat flow values for Gulf of Mexico stations.

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