Volcanism in the southern part of the Hocheifel.

1Citations
Citations of this article
3Readers
Mendeley users who have this article in their library.
Get full text

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?

Save time finding and organizing research with Mendeley

Sign up for free