Widespread volcanism associated with Middle Triassic carbonate platforms is well known,and in many cases referred as a partial cause of the disruption of platform development due to burial by volcanic material.It is n...Widespread volcanism associated with Middle Triassic carbonate platforms is well known,and in many cases referred as a partial cause of the disruption of platform development due to burial by volcanic material.It is no doubt that silicic explosive volcanism produced large volume of volcanic material accumulated in basins surrounding the carbonate platforms(Buchenstein basins)alternating with pelagic carbonates of basin facies.There are large numbers of mafic eruptive products associated with individual carbonate platforms such as the Latemar in the Dolomites in northern Italy.展开更多
基金Project supported by the Hungarian Research Found(OTKA T043341 BT)NZ-FRST Post-doctoral Fellowship(MAUX 405)(KN)and Massey University Research Fund(KN)Constructive reviews by Corina Risso(Buenos Aires)and Peter Suhr(Dresden)significantly elevated the quality of this report,many thanks for them.
文摘Widespread volcanism associated with Middle Triassic carbonate platforms is well known,and in many cases referred as a partial cause of the disruption of platform development due to burial by volcanic material.It is no doubt that silicic explosive volcanism produced large volume of volcanic material accumulated in basins surrounding the carbonate platforms(Buchenstein basins)alternating with pelagic carbonates of basin facies.There are large numbers of mafic eruptive products associated with individual carbonate platforms such as the Latemar in the Dolomites in northern Italy.
