Elements

Journal: Elements

Abbreviation

Elements (Que. Print)

Publisher

Mineralogical Society of America

ISSN

1811-5209
1811-5217

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Publications1 - 10 of 21

Alteration of the Oceanic Lithosphere and Implications for Seafloor Processes
Bach, Wolfgang; Früh-Green, Gretchen L. (2010)
Elements
Formation and Exhumation of Ultrahigh-Pressure Terranes
Hacker, B. R.; Gerya, Taras; Gilotti, J. A. (2013)
Elements
Time constraints and tie-points in the quaternary period
Richards, David A.; Andersen, Morten B. (2013)
Elements
Perspectives on Metamorphic Processes and Fluids
Thompson, Alan Bruce (2010)
Elements
Microanalysis of fluid inclusions in crustal hydrothermal systems using laser ablation methods
Wagner, Thomas; Fusswinkel, Tobias; Wälle, Markus; et al. (2016)
Elements
Metal retention and transport on colloidal particles in the environment
Kretzschmar, Ruben; Schäfer, Thorsten (2005)
Elements
The Origin of the Earth
Halliday, Alex N. (2006)
Elements
The Mechanics of Metamorphic Fluid Expulsion
Connolly, James (2010)
Elements
Kimberlites: From Deep Earth to Diamond Mines
Giuliani, Andrea; Pearson, D. Graham (2019)
Elements
Kimberlites are rare, enigmatic, low-volume igneous rocks. They are highly enriched in magnesium, volatiles (CO2 and H2O) and incompatible trace elements and are thought to be the most deeply derived (>150 km) magmatic rocks on Earth. Kimberlites occur in ancient and thick continental lithosphere, forming intrusive sheets and composite pipes, commonly in clusters. Despite their rarity, kimberlites have attracted considerable attention because they entrain not only abundant mantle fragments but also diamonds, which can provide a uniquely rich picture of the deep Earth. This issue summarises current thinking on kimberlite petrology, geochemistry, and volcanology and outlines the outstanding questions on the genesis of kimberlites and associated diamond mines.
The Kos–Nisyros–Yali Volcanic Field
Bachmann, Olivier; Allen, Sharon R.; de Maisonneuve, Caroline Bouvet (2019)
Elements

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Journal: Elements

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