Metadata
Author: springer
Data
English[en]
A continuous marine environment existed in the Hettangian-Tithonian span, with volcanic events in the Bajocian, Callovian, Kimmeridgian, and Tithonian.
Spanish[es]
Hay un desarrollo marino continuo entre el Hettangiano y el Titoniano y facies evaporíticas en el Oxfordiano-Kimmeridgiano.