Gialanella P.; Heller F.; Haag M.; Nurgaliev D.; Borisov A.; Burov B.; Jasonov P.; Khasanov D.; Ibragimov S.; Zharkov I.
(1997)
The Late Permian is characterized palaeomagnetically by the transition from the long-lasting Permo-Carboniferous reversed polarity superchron (PCRS; also called: Kiaman reversed superchron) to the subsequent Permo-Triassic ...