Basin analysis


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Journal

Use of single-grain geochemistry of cryptic tuffs and volcaniclastic sandstones improves the tephrostratigraphic framework of Olduvai Gorge, Tanzania. (2013) Mchenry LJ, Stollhofen H, Stanistreet IG Journal article, Original article Salt kinematics and regional tectonics across a Permian gas field: a case study from East Frisia, NW Germany. (2013) Vackiner AA, Antrett P, Strozyk F, Back S, Kukla P, Stollhofen H Journal article, Original article Rotliegend im Saar-Nahe-Becken, am Taunus-Südrand und im nördlichen Rheingraben (2012) Boy JA, Haneke J, Kowalczyk G, Lorenz V, Schindler T, Stollhofen H, Thum H Book chapter / Article in edited volumes Plio-Pleistocene syn-sedimentary fault compartments underpin lake margin paleoenvironmental mosaic, Olduvai Gorge, Tanzania (2012) Stollhofen H, Stanistreet IG Journal article, Original article Ultrasonic logging across unconformities — outcrop and core logger sonic patterns of the Early Triassic Middle Buntsandstein Hardegsen unconformity, southern Germany. (2011) Filomena C, Stollhofen H Journal article, Original article Pleistocene to Recent rejuvenation of the Hebron Fault, south-western Namibia. (2009) White S, Stollhofen H, Stanistreet IG, Lorenz V Book chapter / Article in edited volumes Upper Rotliegend to Early Cretaceous basin development. (2008) Stollhofen H, Bachmann G, Barnasch J, Bayer U, Beutler G, Franz M, Kästner M, et al. Book chapter / Article in edited volumes Karoo unconformities in NW Namibia and their tectonic implications. (2000) Wanke A, Stollhofen H, Stanistreet IG, Lorenz V Journal article, Original article High resolution tephrostratigraphy, fossil record and age of Carboniferous-Permian glaciomarine mudstones within the Dwyka Group of southern Namibia. (2000) Bangert B, Stollhofen H, Geiger M, Lorenz V Journal article, Original article Tuffs, tectonism and glacially related sea-level changes, Carboniferous-Permian, Southern Namibia. (2000) Stollhofen H, Stanistreet IG, Bangert B, Grill H Journal article, Original article
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