Results 201 to 210 of about 58,594 (258)
Unconventional water and hydrous mineral formation from dry minerals and H<sub>2</sub> fluids. [PDF]
Vitale Brovarone A +10 more
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Mantle melting and lithospheric structure beneath eastern Australia's Cenozoic volcanoes from 3D magnetotellurics. [PDF]
Margiono R, Heinson G.
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Trace element systematics constrain the origin of fluids that form gem-quality diamonds. [PDF]
Rakipov A +8 more
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Sulfur-enriched sub-arc fluids drive deep sulfur cycling in subduction zones. [PDF]
Tan DB +10 more
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Unicentric Adrenal Castleman Disease Mimicking an Adrenal Tumour. [PDF]
Han LA, Naung Y.
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Zircon behavior in the partially melted planetary mantle
Yakimenko A +3 more
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IEEE Power Engineering Review, 1983
Through differntial (Wollastoferometric) inter- erometric diagnostics, the radial distributions of temperature and air particle density (at various times within a current pulse) within the arc mantle, and the timewise distributions of arc size and mantle thickness have been obtained in the region upstream of the throat in a single flow orifice nozzle ...
Nanu Brates, David Benenson
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Through differntial (Wollastoferometric) inter- erometric diagnostics, the radial distributions of temperature and air particle density (at various times within a current pulse) within the arc mantle, and the timewise distributions of arc size and mantle thickness have been obtained in the region upstream of the throat in a single flow orifice nozzle ...
Nanu Brates, David Benenson
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Properties of the mantle cell and mantle cell lymphoma
Current Opinion in Hematology, 2002The major lymphoid inhabitant of the follicular mantle is the mantle cell, an immunologically naïve B cell. It is the putative cell of origin of mantle cell lymphoma (MCL), the cells of which have similar morphologic, immunophenotypic, and molecular characteristics to the normal B lymphocytes of the mantle zone.
John L, Frater, Eric D, Hsi
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Annual Review of Earth and Planetary Sciences, 1992
The mid-ocean ridge basalts (MORB) are depleted in trace elements due to the extraction of the crust, which is correspondingly enriched. The isotopic character of MORB indicates that the source region for these basalts has been depleted for some time (several billion years).
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The mid-ocean ridge basalts (MORB) are depleted in trace elements due to the extraction of the crust, which is correspondingly enriched. The isotopic character of MORB indicates that the source region for these basalts has been depleted for some time (several billion years).
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