AN ABSOLUTE PLATE MOTION MODEL BASED ON HOTSPOT REFERENCE FRAME

ZHANG Qiong, WANG Shi-Min, ZHAO Yong-Hong
{"title":"AN ABSOLUTE PLATE MOTION MODEL BASED ON HOTSPOT REFERENCE FRAME","authors":"ZHANG Qiong,&nbsp;WANG Shi-Min,&nbsp;ZHAO Yong-Hong","doi":"10.1002/cjg2.30060","DOIUrl":null,"url":null,"abstract":"<p>Based on the new generation model of relative plate motions, the MOVEL model, an absolute plate motion model is built by least squares inversion of the observed hotspot trend data. A systematic test for the consistency between the MOVEL model and all the available hotspot data adopted by previous studies of absolute plate motion models shows there are outliers in the data set. Accordingly, two new methods to reject outliers, such as, step-wise rejection and global search rejection, are proposed. Combined with the chi-square test for the total residual and the normal test for the residual frequency distribution, the best model is selected step by step. A T87 model is eventually obtained. This model provides reasonable fitting to 87 globally distributed hotspot trends, but the predicted plate velocities are systematically lower than the observed rates of volcanic migration along hotspot tracks with the deviation up to 4 cm·a<sup>−1</sup>. Such a deviation may be explained as a consequence of systematic errors possibly associated with the observed hotspot rate data, or due to relative motions between hotspots caused by mantle return flow. For either case, however, this study's results demonstrate that the hotspot trend data are capable of defining a global hotspot reference frame independently and effectively, which could be conveniently applied to studies on absolute plate motion, mantle convection and true polar wander.</p>","PeriodicalId":100242,"journal":{"name":"Chinese Journal of Geophysics","volume":"60 5","pages":"456-464"},"PeriodicalIF":0.0000,"publicationDate":"2018-02-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/cjg2.30060","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chinese Journal of Geophysics","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/cjg2.30060","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

Based on the new generation model of relative plate motions, the MOVEL model, an absolute plate motion model is built by least squares inversion of the observed hotspot trend data. A systematic test for the consistency between the MOVEL model and all the available hotspot data adopted by previous studies of absolute plate motion models shows there are outliers in the data set. Accordingly, two new methods to reject outliers, such as, step-wise rejection and global search rejection, are proposed. Combined with the chi-square test for the total residual and the normal test for the residual frequency distribution, the best model is selected step by step. A T87 model is eventually obtained. This model provides reasonable fitting to 87 globally distributed hotspot trends, but the predicted plate velocities are systematically lower than the observed rates of volcanic migration along hotspot tracks with the deviation up to 4 cm·a−1. Such a deviation may be explained as a consequence of systematic errors possibly associated with the observed hotspot rate data, or due to relative motions between hotspots caused by mantle return flow. For either case, however, this study's results demonstrate that the hotspot trend data are capable of defining a global hotspot reference frame independently and effectively, which could be conveniently applied to studies on absolute plate motion, mantle convection and true polar wander.

基于热点参考系的绝对板块运动模型
在新一代板块相对运动模型MOVEL模型的基础上,通过对观测热点趋势数据进行最小二乘反演,建立了板块绝对运动模型。系统检验MOVEL模型与以往研究绝对板块运动模型所采用的所有可用热点数据的一致性,发现数据集中存在异常值。据此,提出了两种新的异常值拒绝方法,即逐步拒绝和全局搜索拒绝。结合总残差的卡方检验和残差频率分布的正态检验,逐步选择最佳模型。最后得到了一个T87模型。该模型对全球分布的87个热点趋势进行了较好的拟合,但预测的板块速度有系统地低于沿热点轨迹观测到的火山迁移速率,偏差达4 cm·a−1。这种偏差可以解释为可能与观测到的热点速率数据有关的系统误差的结果,或者是由于地幔回流引起的热点之间的相对运动。然而,本文的研究结果表明,热点趋势数据能够独立有效地定义一个全球热点参考框架,可以方便地应用于板块绝对运动、地幔对流和真极移的研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信