Abstract
Silicic lavas with no basal breccia: origin of the thinly jointed basal facies of low-Ti dacites in the Paraná-Etendeka Large Igneous Province
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
