The Skaergaard liquid line of descent revisited
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
http://link.springer.com/content/pdf/10.1007/s00410-008-0361-6.pdf
Reference71 articles.
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2. Ariskin AA (1999) Phase equilibria modeling in igneous petrology; use of COMAGMAT modeling for simulating fractionation of ferro-basaltic magmas and the genesis of high-alumina basalt. J Volcanol Geotherm Res 90:115–162. doi: 10.1016/S0377-0273(99)00022-0
3. Ariskin AA (2003) The compositional evolution of differentiated liquids from the Skaergaard layered series as determined by geochemical thermometry. Russ J Earth Sci 5:1–29
4. Ariskin AA, Barmina GS (1999) An empirical model for the calculation of spinel-melt equilibria in mafic igneous systems at atmospheric pressure: 2. Fe–Ti oxides. Contrib Mineral Petrol 134:251–263. doi: 10.1007/s004100050482
5. Ariskin AA, Barmina GS (2004) COMAGMAT: development of a magma crystallization model and its petrological applications. Geochem Int 42(Suppl 1):S1–S157
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