Coupled 186 Os and 187 Os Evidence for Core-Mantle Interaction

Author:

Brandon Alan D.1234,Walker Richard J.1234,Morgan John W.1234,Norman Marc D.1234,Prichard Hazel M.1234

Affiliation:

1. A. D. Brandon, R. J. Walker, J. W. Morgan, Isotope Geochemistry Laboratory, Department of Geology, University of Maryland, College Park, MD 20742, USA.

2. J. W. Morgan, Department of Earth Resources, Colorado State University, Fort Collins, CO 80523, USA.

3. M. D. Norman, GEMOC, School of Earth Sciences, Macquarie University, NSW 2109, Australia.

4. H. M. Prichard, Department of Earth Sciences, University of Wales, Cardiff, CF1 3YE, United Kingdom.

Abstract

Osmium isotopic analyses of picritic lavas from Hawaii show enrichments in the osmium-186/osmium-188 ratio ( 186 Os/ 188 Os) of 0.008 to 0.018%, relative to a chondritic upper mantle, that are positively correlated with enrichments in 187 Os/ 188 Os of 5.4 to 9.0%. The most viable mechanism to produce these coupled 186 Os and 187 Os enrichments is by addition of 0.5 to 1 weight percent of outer core metal to a portion of the D" layer and subsequent upwelling of the mixture. These data suggest that some plumes originate at the core-mantle boundary and that Os isotopes may be used to distinguish plumes derived from shallow versus deep mantle sources.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3