Spectacular Mantle Xenoliths Derived from "Oceanic Kimberlite", Malaita, Solomon Islands: A Unique Window into the Earth's Deep Interior

Author:

ISHIKAWA Akira

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference26 articles.

1. Allen, J.B. and Deans, T. (1965) : Ultrabasic eruptives with alnöitic-kimberlitic affinities from Malaita, Solomon Islands. Minralogical Magazine, 34, 16-34.

2. Brey, G.P. and Köhler, T. (1990) : Geothermobarometry in four-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers. Journal of Petrology, 31, 1352-1378.

3. Derivation of Large Igneous Provinces of the past 200 million years from long-term heterogeneities in the deep mantle

4. Coffin, M.F. and Eldholm, O. (1994) : Large igneous provinces: crustal structure, dimensions, and external consequences. Reviews of Geophysics, 32, 1-36.

5. Collerson, K.D., Hapugoda, S., Kamber, B.S. and Williams, Q. (2000) : Rocks from the mantle transition zone: majorite-bearing xenoliths from Malaita, Southwest Pacific. Science, 288, 1215-1223.

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