Abstract
The Wet Chemistry Labs on Phoenix gave pH, conductivity, ions, and evidence that the salts have previously interacted with water and contain high levels of carbonates. Carbonate results show the need for more extensive laboratory work and equilibrium modeling.
Cite
CITATION STYLE
APA
Cohen, S. C., & Darby, D. J. (2003). Tectonic plate coupling and elastic thickness derived from the inversion of a steady state viscoelastic model using geodetic data: Application to southern North Island, New Zealand. Journal of Geophysical Research: Solid Earth, 108(B3). https://doi.org/10.1029/2001jb001687
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