Geochemical evidence for the formation of a large Miocene „Travertine“ Mound at a sublacustrine spring in a Soda lake (Wallerstein Castle Rock, Nördlinger Ries, Germany)
Geochemical evidence for the formation of a large Miocene „Travertine“ Mound at a sublacustrine spring in a Soda lake (Wallerstein Castle Rock, Nördlinger Ries, Germany)
Pache, M., Reitner, J. & Arp, G.(2001). Geochemical evidence for the formation of a large Miocene „Travertine“ Mound at a sublacustrine spring in a Soda lake (Wallerstein Castle Rock, Nördlinger Ries, Germany). – Facies, 45, S. 211–230. [9 Abb., 3 Anh.]