Processes Governing Alkaline Groundwater Chemistry within a Fractured Rock (Ophiolitic Mélange) Aquifer Underlying a Seasonally Inhabited Headwater Area in the Aladağlar Range (Adana, Turkey)

<div>Field image of a large fracture system (crosscutting the highly fractured serpentinite rock in Kızılcadağ ophiolitic mélange) filled/sealed with chrysotile (i.e., fibrous asbestos) and secondary dolomite. Hammer for scale is 33 cm long.</div>

Geofluids

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Figure 5

Figure 5: Processes Governing Alkaline Groundwater Chemistry within a Fractured Rock (Ophiolitic Mélange) Aquifer Underlying a Seasonally Inhabited Headwater Area in the Aladağlar Range (Adana, Turkey) 

Figure 5 | Processes Governing Alkaline Groundwater Chemistry within a Fractured Rock (Ophiolitic Mélange) Aquifer Underlying a Seasonally Inhabited Headwater Area in the Aladağlar Range (Adana, Turkey) 