Genesis of carbonate aggregates in lamprophyres from the northeastern Transdanubian Central Range, Hungary: Magmatic or hydrothermal origin?-Reference-Cited by-同舟云学术

Genesis of carbonate aggregates in lamprophyres from the northeastern Transdanubian Central Range, Hungary: Magmatic or hydrothermal origin?

Published:2006-05-11 Issue:3-4 Volume:88 Page:479-497
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Mineralogy and Petrology

Author:

Azbej T.,Szabó C.,Bodnar R. J.,Dobosi G.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00710-006-0123-y.pdf

Reference43 articles.

1. Trace element and Nd–Sr isotopic composition of ultramafic lamprophyres from the East Antarctic Beaver Lake area

2. Azbej T (2002) Petrographic and geochemical study on carbonates in lamprophyres (in Hungarian). M.Sc. Thesis. Lithosphere Fluid Research Lab, Eötvös University, Budapest, p 102

3. Assimilation and metamorphism at a basalt-limestone contact, Tokatoka, New Zealand

4. Climate-controlled early dolomite, Late Triassic cyclic platform carbonates, Hungary

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