Polymorphic Nature of Iron and Degree of Lattice Preferred Orientation Beneath the Earth's Inner Core Boundary-Reference-Cited by-同舟云学术

Polymorphic Nature of Iron and Degree of Lattice Preferred Orientation Beneath the Earth's Inner Core Boundary

Author:

Mattesini Maurizio¹²^ORCID,Belonoshko Anatoly B.³^ORCID,Tkalčić Hrvoje⁴^ORCID

Affiliation:

1. Department of Earth's Physics and Astrophysics; Complutense University of Madrid; Madrid Spain

2. Instituto de Geociencias (UCM-CSIC); Facultad de Ciencias Físicas; Madrid Spain

3. Condensed Matter Theory, Department of Physics, KTH Royal Institute of Technology; AlbaNova University Center; Stockholm Sweden

4. Research School of Earth Sciences; The Australian National University; Canberra ACT Australia

Funder

Spanish Ministry of Economy and Competitiveness

Banco Bilbao Vizcaya Argentaria

“I convocatoria de Ayudas Fundación BBVA a Investigadores, Innovadores y Creadores Culturales”

Swedish Scientific Council

Physics of the Earth's Core

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference62 articles.

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