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Geochemistry of the Rare Earth elements in spilites from the oceanic and continental crust

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TLDR
In this paper, analytical data including major elements, the Rare Earths, Ni, Cu, Zn, Rb, and Sr are presented for twenty-three spilites from the Mid-Atlantic Ridge, the Hercynian part of the Variscan geosyncline in Germany, and several localities in Switzerland.
Abstract
Analytical data including major elements, the Rare Earths, Ni, Cu, Zn, Rb, and Sr are presented for twenty-three spilites from the Mid-Atlantic Ridge, the Hercynian part of the Variscan geosyncline in Germany, and several localities in Switzerland. Low grade metamorphism (up to approximately 400° C) and spilitization of basaltic rocks apparently do not alter the original Rare Earth element (REE) distributions. This fact permits comparison of the spilites and unaltered tholeiitic basalts from the Mid-Atlantic Ridge. The relative REE distributions thus appear suitable for delineating the original basalt types of spilites formed by metamorphism.

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Geochemical discrimination of different magma series and their differentiation products using immobile elements

TL;DR: In this article, the abundance and distribution of selected minor and trace elements (Ti, Zr, Y, Nb, Ce, Ga and Sc) in fresh volcanic rocks can be used to classify the differentiation products of subalkaline and alkaline magma series in a similar manner to methods using normative or major-element indices.
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Geochemical magma type discrimination: application to altered and metamorphosed basic igneous rocks

TL;DR: In this article, five minor and trace elements, known to be chemically stable during alteration and metamorphism, have been combined in a set of binary diagrams that distinguish fresh tholeiites from alkali basalts.
Journal ArticleDOI

Rare Earth Elements in Petrogenetic Studies of Igneous Systems

TL;DR: In this paper, a detailed knowledge of the geochemistry of systems involving fluids, minerals, and melts would be required, and this knowledge is not available, thus, it is necessary to make inf erences based on the inf ormation we have.
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Hydrothermal Mobilisation of the Rare Earth Elements – a Tale of “Ceria” and “Yttria”

TL;DR: Although rare earth elements have been thought by many to be immobile in hydrothermal fluids, we have known since the first attempts to separate them in the early nineteenth century that they are soluble in aqueous solutions as mentioned in this paper.
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Identification of ore-deposition environment from trace-element geochemistry of associated igneous host rocks

TL;DR: In this article, the authors identify the tectonic environment of formation of volcanogenic massive sulphide deposits and porphyry tin and copper deposits from the geochemical characteristics of the associated igneous rocks.
References
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Journal ArticleDOI

Chemical Characteristics of Oceanic Basalts and the Upper Mantle

TL;DR: In this article, it was shown that oceanic tholeiites are either complete melts of the upper mantle or are generated from a mix of this tholeite and a magnesium-rich peridotite or dunite in proportions up to perhaps 1:4.
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Chemical Characteristics and Origin of Oceanic Ridge Volcanic Rocks

TL;DR: Oceanic ridge volcanic rocks alkali metal, alkaline earth, rare earth, nickel and major element content, observing partial melting as mentioned in this paper. But this is not the case for all volcanic rocks.
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Rare earth elements and the island arc tholeiitic series

TL;DR: The island arc tholeiitic series as mentioned in this paper is the most dominant in many western Pacific and Atlantic Island arcs and represents the earliest stages in arc evolution. But it is chemically inappropriate to call many of the rocks in island arcs calc-alkaline and they suggest they be known as the "island arc thoeitic series" and they differ from normal thoeiitic features by having a higher percentage of intermediate and acid members and too little normative olivine, for example, to have been in equilibrium with peridotite.
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Meteoritic, solar and terrestrial rare-earth distributions.

TL;DR: Meteoritic, solar and terrestrial rare earth distribution abundance in chondritic or ordinary stony meteorites was studied in this paper, where the distribution of rare earth abundance in meteorites is analyzed.
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