TY  - JOUR
A1  - Wendt, A. S.
A1  - Altenberger, Uwe
A1  - D'arco, 
T1  - Radial cracks around chromite inclusions in olivine : a new geothermobarometer based on the thermoelastic properties of chromite and forsterite-rich olivine
Y1  - 1998
ER  - 
TY  - JOUR
A1  - Oberhänsli, Roland
A1  - Wendt, A. S.
A1  - Goffe, B.
A1  - Michard, Andre
T1  - Detrital chromites in metasediments of East-Arabian continental margin in te Saih Hatat area : constraints for the palaeogeographic setting of the Hawasina and Semail basins (Oman Mountains)
Y1  - 1999
ER  - 
TY  - JOUR
A1  - Rohrmüller, J.
A1  - Kämpf, Horst
A1  - Geiss, E.
A1  - Grossmann, J.
A1  - Grun, I.
A1  - Mingram, Jens
A1  - Mrlina, J.
A1  - Plessen, Birgit
A1  - Stebich, M.
A1  - Veress, C.
A1  - Wendt, A.
A1  - Nowaczyk, Nobert
T1  - Reconnaissance study of an inferred Quaternary maar structure in the western part of the Bohemian Massif near Neualbenreuth, NE-Bavaria (Germany)
JF  - International journal of earth sciences
N2  - After a comprehensive geophysical prospecting the Quaternary MA 1/2 tina Maar, located on a line between the two Quaternary scoria cones Komorni could be revealed by a scientific drilling at the German-Czech border in 2007. Further geophysical field investigations led to the discovery of another geological structure about 2.5 km ESE of the small town Neualbenreuth (NE-Bavaria, Germany), inferred to be also a maar structure, being the fourth volcanic feature aligned along the NW-SE trending Tachov fault zone. It is only faintly indicated as a partial circular rim in the digital elevation model. Though not expressed by a clear magnetic anomaly, geoelectric and refraction seismic tomography strongly indicates a bowl-shaped depression filled with low-resistivity and low-velocity material, correlating well with the well-defined negative gravity anomaly of - 2.5 mGal. Below ca. 15 m-thick debris layer, successions of mostly laminated sediments were recovered in a 100 m-long sediment core in 2015. Sections of finely laminated layers, likely varves, rich in organic matter and tree pollen, were recognized in the upper (22-30 m) and lower (70-86 m) part of the core, respectively, interpreted as interglacials, whereas mostly minerogenic laminated deposits, poor in organic matter, and (almost) barren of tree pollen are interpreted as clastic glacial deposits. According to a preliminary age model based on magnetostratigraphy, palynology, radiocarbon dating, and cyclostratigraphy, the recovered sediments span the time window from about 85 ka back to about 270 ka, covering marine isotope stages 5-8. Sedimentation rates are in the range of 10 cm ka(-1) in interglacials and up to 100 cm ka(-1) in glacial phases. The stratigraphic record resembles the one from MA 1/2 tina Maar, with its eruption date being derived from a nearby tephra deposit at 288 +/- 17 ka, thus supporting the age model of the inferred Neualbenreuth Maar.
KW  - Eger Rift
KW  - Quaternary maar volcanism
KW  - Geophysical prospecting
KW  - Magnetostratigraphy
KW  - Palynology
KW  - Paleoclimate
Y1  - 2018
U6  - https://doi.org/10.1007/s00531-017-1543-0
SN  - 1437-3254
SN  - 1437-3262
VL  - 107
IS  - 4
SP  - 1381
EP  - 1405
PB  - Springer
CY  - New York
ER  -