Provenance of Palaeozoic sediments during subduction of Palaeotethys: detrital zircon ages and the analysis of olistoliths from Chios Island, Greece.

Journal article


Publication Details

Author(s): Meinhold G, Lehnert O, Reischmann T, Kostopoulos D, Matukov D, Sergeev S
Journal: Palaeogeography, Palaeoclimatology, Palaeoecology
Publication year: 2008
Volume: 263
Pages range: 71-91
ISSN: 0031-0182


FAU Authors / FAU Editors

Lehnert, Oliver PD Dr.
Professur für Paläontologie (Schwerpunkt Faziesanalyse)


External institutions with authors

Georg-August-Universität Göttingen
Max-Planck-Institut für Chemie (Otto Hahn Institut) / Max Planck Institute for Chemistry
National and Kapodistrian University of Athens


How to cite

APA:
Meinhold, G., Lehnert, O., Reischmann, T., Kostopoulos, D., Matukov, D., & Sergeev, S. (2008). Provenance of Palaeozoic sediments during subduction of Palaeotethys: detrital zircon ages and the analysis of olistoliths from Chios Island, Greece. Palaeogeography, Palaeoclimatology, Palaeoecology, 263, 71-91. https://dx.doi.org/10.1016/j.palaeo.2008.02.013

MLA:
Meinhold, Guido, et al. "Provenance of Palaeozoic sediments during subduction of Palaeotethys: detrital zircon ages and the analysis of olistoliths from Chios Island, Greece." Palaeogeography, Palaeoclimatology, Palaeoecology 263 (2008): 71-91.

BibTeX: 

Last updated on 2019-02-01 at 13:50