Abstract
Owing to their structural and hydrogeological setting, a great many of the volcanoes of the Rhenish massif and surrounding areas erupted phreatomagmatically, causing the formation of the many maars, diatremes and tuff-mantled plugs.-J.M.H.
Cite
CITATION STYLE
APA
Bussmann, E., & Lorenz, V. (1983). Volcanism in the southern part of the Hocheifel. Plateau Uplift: The Rhenish Shield - a Case History, 129–130. https://doi.org/10.1007/978-3-642-69219-2_17
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free