Fig. 3
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Stratigraphic column, log and H2 content in % from the well PTRA-1. H2 amounts are derived from five samples. Two of these samples are listed in Table 1, obtained during the well test (860 to 912 m depth), with the reference depth (886 m) representing an average of the depth interval. They appear superimposed in the figure due to being from the same depth interval and exhibiting similar H2 values. The remaining three samples correspond to isojar samples collected from 1419, 1455, and 1491 m depth; therefore, the accuracy of their value is questionable as discussed in item 3 of the Appendix. However, after air correction, these values are included in the graph to indicate that the Espinhaço Sequence also holds H2 shows. GR corresponds to gamma ray, RLA_3 to resistivity, DT Vp to sonic, RHOZ to density and NPHI to neutron log.
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