The hole then encountered a sequence of sands and clays hostingsalty waters which then, at about 235m, turned to brines hosted within coarse clastic sedimentsincluding a breccia‐conglomerate (see Figure 1). Conductivity measurements from brine samplesexceeded the 200 milli siemens/cm limits of the field recording instrument.
That looks good enough for me.
Ann: Brines Discovered in Maiden Drillhole, page-8
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