| 书目名称 | Plate Deformation from Cradle to Grave |
| 副标题 | Seismic Anisotropy a |
| 编辑 | Andy Nowacki |
| 视频video | http://file.papertrans.cn/750/749288/749288.mp4 |
| 概述 | Outstanding doctoral thesis nominated for a Springer Theses Prize by the University of Bristol, United Kingdom.A comprehensive explanation of seismic anisotropy in the lowermost mantle gives the reade |
| 丛书名称 | Springer Theses |
| 图书封面 |  |
| 描述 | The Earth‘s rocky mantle convects to lose heat, which comes from the liquid iron core below. The mantle‘s interfaces - the core-mantle boundary, and the lithosphere - may hold the key to understanding mantle motion because of the seismic anisotropy present in these parts of the Earth. .In this thesis, Andy Nowacki presents a precise but comprehensive review of the current state of the art in studying flow with anisotropy, mineral physics and geodynamics. New measurements of shear wave anisotropy in the lowermost mantle and at mid-ocean ridges are used to constrain mechanisms of creep and melt extraction in the mantle. A model of global flow is used to predict anisotropy in the deep Earth, and novel methods to forward model shear wave splitting are described. Future studies of mantle flow must incorporate the understanding gained in this thesis. .The thesis contains a substantive introduction to the structure of the Earth, seismic anisotropy in general and in the core-mantle boundary region, and mid-ocean ridge processes. It also describes novel methods for forward modelling and interpreting shear wave splitting data. Three chapters present timely research into dynamics at div |
| 出版日期 | Book 2013 |
| 关键词 | Lowermost Mantle; Mantle Dynamics; Mid-ocean Ridges; Seismic Anisotropy; Shear Wave Splitting |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-642-34842-6 |
| isbn_softcover | 978-3-662-51099-5 |
| isbn_ebook | 978-3-642-34842-6Series ISSN 2190-5053 Series E-ISSN 2190-5061 |
| issn_series | 2190-5053 |
| copyright | Springer-Verlag Berlin Heidelberg 2013 |
|Archiver|手机版|小黑屋|
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