Chemically homogeneous spin transition zone in Earth's lower mantle

被引：11

作者：

Narygina, O. ^{[1
]}

Dubrovinsky, L. S. ^{[1
]}

Samuel, H. ^{[1
]}

McCammon, C. A. ^{[1
]}

Kantor, I. Yu. ^{[1
]}

Glazyrin, K. ^{[1
]}

Pascarelli, S. ^{[2
]}

Aquilanti, G. ^{[2
]}

Prakapenka, V. B. ^{[3
]}

机构：

[1] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany

[2] European Synchrotron Radiat Facil, F-38043 Grenoble, France

[3] Univ Chicago, CARS, Chicago, IL 60437 USA

来源：

PHYSICS OF THE EARTH AND PLANETARY INTERIORS | 2011年 / 185卷 / 3-4期

基金：

美国国家科学基金会;

关键词：

XANES; Silicate perovskite; Ferropericlase; Fe-Mg partitioning; Diamond anvil cell; In situ laser heating; MAGNESIUM-SILICATE PEROVSKITE; DIAMOND-ANVIL CELL; ABSORPTION-SPECTROSCOPY; SYNCHROTRON MOSSBAUER; FERROUS IRON; MAGNESIOWUSTITE; FERROPERICLASE; GPA;

D O I：

10.1016/j.pepi.2011.02.004

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The effect of spin crossover in lower mantle silicate perovskite (Pv) and ferropericlase (Fp) on the iron partitioning between these two phases remains uncertain, mainly due to the lack of in situ experiments under the relevant pressure and temperature conditions. By combining in situ synchrotron X-ray absorption and diffraction measurements on synthetic ringwoodite and natural (Mg(0.88)Fe(0.12))(2)SiO(4) San Carlos olivine at pressures between 22 GPa and 115 GPa treated at temperatures of 1950-2300 K, we found that temperature promotes iron partitioning into Pv, while pressure acts oppositely. There is only a limited effect of spin crossover in co-existing Pv and Fp on iron partitioning which cannot produce an appreciable chemical inhomogeneity within the Earth's lower mantle spin transition zone. Crown Copyright (C) 2011 Published by Elsevier B.V. All rights reserved.

引用

页码：107 / 111

页数：5

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