Geochemical evolution of the lithospheric mantle beneath the Styrian Basin (Western Pannonian Basin)

Author:

Aradi László Előd,Bali Enikő,Patkó Levente,Hidas Károly,Kovács István János,Zanetti Alberto,Garrido Carlos J.,Szabó Csaba

Funder

ELTE Institutional Excellence Program

Hungarian Ministry of Human Capacities

Hungarian Science Foundation

Ministry of Economy, Industry and Competitiveness

State Research Agency

CSFK Lendület Pannon LitH2Oscope Research group

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference108 articles.

1. The effects of pressure and temperature on the partitioning of Ti, Sr and REE between amphibole, clinopyroxene and basanitic melts;Adam;Chem. Geol.,1994

2. Petrogenesis and mantle source characteristics of Quaternary alkaline mafic lavas in the western Carpathian–Pannonian Region, Styria, Austria;Ali;Chem. Geol.,2013

3. Fluid-enhanced annealing in the subcontinental lithospheric mantle beneath the westernmost margin of the carpathian-pannonian extensional basin system;Aradi;Tectonics,2017

4. Composition and origin of upper-mantle fluids based on fluid inclusions in amphibole-rich harzburgite xenoliths from the Styrian Basin;Aradi,2019

5. An estimation of the least depleted spinel peridotite on the basis of olivine-spinel mantle array;Arai;Neues Jb. Mineral. Monat.,1987

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