Figure F8. In situ temperature in Brazos-Trinity Basin IV, Sites U1319 and U1320. Temperature/dual pressure (T2P) probe temperature reached equilibrium with the formation temperature at the end of the deployment (Table T2). Davis-Villinger Temperature-Pressure Probe (DVTPP) temperature did not equilibrate with the formation temperature at the end of the deployment. In situ temperatures were estimated using 1/t extrapolation (Table T2). Red = temperature measurements subjected to influence of tool movements during dissipation phase.
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