Table 1.
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.