Creation of Secondary Porosity in Dolostones by Upwelling Basement Water in the Foreland of the Alpine Orogen

<div>Sulphur isotopic composition of primary anhydrite in the Sulfatschichten (Middle Muschelkalk), the Dolomit der Anhydritgruppe (DAG), the Trigonodus Dolomit (TD), and the Keuper compared to those of secondary anhydrite fracture-fillings in the Hauptmuschelkalk (HMK), TD, and Keuper. <sup>1</sup>[<a href="/journals/geofluids/2019/5210404/#B20">20</a>], <sup>2</sup>[<a href="/journals/geofluids/2019/5210404/#B38">38</a>], <sup>3</sup>[<a href="/journals/geofluids/2019/5210404/#B56">56</a>].</div>

Geofluids

fig13

Figure 13

Figure 13: Creation of Secondary Porosity in Dolostones by Upwelling Basement Water in the Foreland of the Alpine Orogen 