The origin of reaction textures in mantle peridotite xenoliths from Sal Island, Cape Verde: the case for “metasomatism” by the host lava-Reference-Cited by-同舟云学术

The origin of reaction textures in mantle peridotite xenoliths from Sal Island, Cape Verde: the case for “metasomatism” by the host lava

Published:2006-04-19 Issue:6 Volume:151 Page:681-697
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Shaw Cliff S. J.,Heidelbach Florian,Dingwell Donald B.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/s00410-006-0087-2.pdf

Reference33 articles.

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2. Brearley M, Scarfe CM, Fujii T (1984) The petrology of ultramafic xenoliths from Summit Lake, near Prince George, British Columbia. Contrib Mineral Petrol 88:53–63

3. Brey GP, Köhler T (1990) Geothermobarometry in four-phase lherzolites II. New thermobarometers and practical assessment of existing thermobarometers. J Petrol 31: 1353–1378

4. Buening DK, Buseck PR (1973) Fe–Mg lattice diffusion in olivine. J Geophys Res 78:6852–6862

5. BVSP (1981) Ultramafic xenoliths in terrestrial volcanics and mantle magmatic processes, basaltic volcanism on the terrestrial planets. LPI, pp 282–310

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