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>(a) The broad geographical subdivision of the Taurides (after [<a href="/journals/geofluids/2017/3153924/#B33">33</a>]) and major tectonic structures in Turkey (KF = Kırkkavak Fault, EF = Ecemiş Fault, TLF = Tuz Lake Fault, EAF = East Anatolian Fault, NAF = North Anatolian Fault, BSZ = Bitlis Suture Zone) (modified from [<a href="/journals/geofluids/2017/3153924/#B34">34</a>]) and (b) location of the Kızılgedik study area in Aladağ (Adana, Turkey).</div>

Geofluids

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Figure 1

Figure 1: 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 1 | Processes Governing Alkaline Groundwater Chemistry within a Fractured Rock (Ophiolitic Mélange) Aquifer Underlying a Seasonally Inhabited Headwater Area in the Aladağlar Range (Adana, Turkey) 