Tube-like schlieren structures in the Fürstenstein Intrusive Complex (Bavarian Forest, Germany): Evidence for melt segregation and magma flow at intraplutonic contacts-Reference-Cited by-同舟云学术

Tube-like schlieren structures in the Fürstenstein Intrusive Complex (Bavarian Forest, Germany): Evidence for melt segregation and magma flow at intraplutonic contacts

Published:2010-05 Issue:3-4 Volume:116 Page:321-339
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Dietl C.,de Wall H.,Finger F.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference41 articles.

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4. Zircon and titanite geochronology of the Fürstenstein granite massif, Bavarian Forest, north-west Bohemian Massif: pulses of the late Variscan magmatic activity;Chen;European Journal of Mineralogy,2004

5. Flow and fabric development during the diapiric rise of magma;Cruden;Journal of Geology,1990

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