Gerhard Einsele
University of Tübingen
35 Papers
358 Citations
Gerhard Einsele is an academic researcher from University of Tübingen. The author has contributed to research in topics: Sediment & Structural basin. The author has an hindex of 18, co-authored 35 publications. Previous affiliations of Gerhard Einsele include University of Basel.
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Papers
Atmospheric carbon burial in modern lake basins and its significance for the global carbon budget
TL;DR: In this article, the authors investigated the contribution of lakes and artificial reservoirs in counteracting man-made CO 2 emissions in arid to semiarid climate which precipitate a major part of their atmosphere-derived dissolved inorganic carbon (DIC) as carbonate.
204
The Xigaze forearc basin: evolution and facies architecture (Cretaceous, Tibet)
Gerhard Einsele,Gerhard Einsele,B Liu,Sören Durr,Wolfgang Frisch,Guanghua Liu,H.P Luterbacher,Lothar Ratschbacher,W Ricken,Jobst Wendt,Andreas Wetzel,G Yu,H Zheng +12 more
TL;DR: The mid-Cretaceous to Eocene flysch deposits of the Xigaze forearc basin in southern Tibet were investigated in a 120 km segment along the Indus-Yarlung suture zone.
164
Terrestrial sediment yield and the lifetimes of reservoirs, lakes, and larger basins
TL;DR: In this paper, the mean rates of mechanical denudation, DRme, and clastic sedimentation, SRme, are related by the ratio of the drainage/lake area, Ad/Al.
105
Vergleich von marokkanischen Kreide-Küstenaufschlüssen und Tiefseebohrungen (DSDP): Stratigraphie, Paläoenvironment und Subsidenz an einem passiven Kontinentalrand
TL;DR: In this article, aufgrund ihrer zumeist reichen Fossilfuhrung eine weitgehende Korrelation von Ammoniten und Foraminiferenzonen gestatten.
86
Basaltic sill-sediment complexes in young spreading centers: Genesis and significance
TL;DR: In contrast to mature mid-oceanic ridges, where magmatic activity is little affected by the slow accumulation of sediments, in young spreading centers (such as that of the Guaymas Basin in the Gulf of California) the basaltic magma of “great magmatic pulses” forms dikes and sills within the uppermost few hundred metres of soft sediments as discussed by the authors.
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