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. 2020 Aug 27;125(9):e2019JE006289. doi: 10.1029/2019JE006289

Table 1.

T‐test on Murray Fm. Members

PH HV K SI BP PP J
PH 0.006 0.460 0.445 0.453 0.129 0.053
HV 1.12E–06 2.85E–07 3.30E–05 1.55E–02 4.48E–11
K 0.942 0.888 8.60E–06 0.035
SI 0.882 1.14E–07 0.016
BP 1.69E–03 0.179
PP 1.11E–16
J

Note. A Welch's t test was used to determine if there is a significant difference between the means of the normalized H peak areas for the different members of the Murray formation. Pahrump Hills (PH), Hartmann's Valley (HV), Karasburg (K), Sutton Island (SI), Blunts Point (BP), Pettegrove Point (PP), and Jura (J). Two‐tailed p values (testing the alternative hypothesis that μA ≠ μB) are reported; p values passing 95% confidence are bolded.