Titanium- and water-rich metamorphic olivine in high-pressure serpentinites from the Voltri Massif (Ligurian Alps, Italy): evidence for deep subduction of high-field strength and fluid-mobile elements-Reference-Cited by-同舟云学术

Titanium- and water-rich metamorphic olivine in high-pressure serpentinites from the Voltri Massif (Ligurian Alps, Italy): evidence for deep subduction of high-field strength and fluid-mobile elements

Published:2014-03 Issue:3 Volume:167 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

De Hoog Jan C. M.,Hattori Keiko,Jung Haemyeong

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-014-0990-x.pdf

Reference64 articles.

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3. Bali E, Audétat A, Keppler H (2013) Water and hydrogen are immiscible in Earth’s mantle. Nature 495:220–222

4. Berry AJ, Hermann J, O’Neill HSC, Foran GJ (2005) Fingerprinting the water site in mantle olivine. Geology 33:869–872

5. Catanzaro EJ, Champion CE, Garner EL, Marinenko G, Sappenfield KM, Shields WR (1970) Standard reference materials: boric acid; isotopic and assay standard reference materials. NBS Special Publication 260-17, 70 p. http://www.nist.gov/srm/upload/SP260-17.PDF

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