Comment on Rosenberg and Garcia: Estimating displacement along the Brenner Fault and orogen-parallel extension in the Eastern Alps, Int J Earth Sci (Geol Rundsch) (2011) 100:1129–1145     

Bernhard Fügenschuh  Neil S. Mancktelow  Stefan S. Schmid 《International Journal of Earth Sciences》2012,101(5):1451-1455

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Characteristics of collisional orogens with low topographic build‐up: an example from the Carpathians     

Liviu Matenco  Csaba Krézsek  Sandra Merten  Stefan Schmid  Sierd Cloetingh  Paul Andriessen 《地学学报》2010,22(3):155-165

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Sand,hearths, lithics and a bit of bioturbation: Site formation processes at Umhlatuzana rockshelter,South Africa     

Irini Sifogeorgaki  Hans Huisman  Panagiotis Karkanas  Viola C. Schmid  Gerrit L. Dusseldorp 《Geoarchaeology》2024,39(3):212-237

Umhlatuzana rockshelter is known for its continuous record of Middle and Later Stone Age lithic assemblages. This study presents multiproxy geoarchaeological data (micromorphology, X-ray diffraction and scanning electron microscopy with energy-dispersive spectroscopy) to reconstruct the depositional and post-depositional history of the site. Although the Stone Age deposits macroscopically appear homogeneous, micromorphological analysis reveals the existence of primary, unaltered depositional microlayering throughout the sequence. Sediments related to combustion activities on-site are observed in both the Holocene and Pleistocene deposits. Post-depositional geochemical alterations result in the formation of several phosphatic minerals that significantly affect the site's preservation conditions. One of those is vashegyite, a rare magnesium phosphate mineral related to acidic and moist sedimentary environments. Bioturbation features are prominent at the microscale, but sediment mixing does not seem to affect the vertical distribution of the artifacts. The observation of horizontal microlayering in both the Pleistocene and Holocene illuminates the dominant mechanism of sedimentation throughout the site's 70,000-year occupational history. It moreover shows that the lithics can be analysed as coherent assemblages.  相似文献