Seismology of the Dynamic Deep Earth

A special issue of Geosciences (ISSN 2076-3263).

Deadline for manuscript submissions: 31 December 2024 | Viewed by 875

Special Issue Editors


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Guest Editor
1. Department of Earth and Planetary Sciences, Yale University, New Haven, CT, USA
2. Department of Earth and Planetary Sciences, University of California, Berkeley, CA, USA
Interests: geophysics; global seismology; mantle dynamics; deep Earth

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Guest Editor
School of Earth and Space Exploration, Arizona State University, Tempe, AZ, USA
Interests: geophysics; global seismology; Earth and planetary interiors; deep Earth geophysics

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Guest Editor
Department of Geological Sciences, The University of Alabama, Tuscaloosa, AL 35487, USA
Interests: geophysics; global seismology; Earth’s interior; deep Earth

Special Issue Information

Dear Colleagues,

We are pleased to invite contributions to this Special Issue of Geosciences, entitled “Seismology of the Dynamic Deep Earth”. Seismic analyses play a central role in elucidating the fundamental structure, dynamics, and evolution of the mantle and core, and investigations over the past few decades have characterized a number of phenomena that are not represented in standard, globally average models of Earth’s radial properties. Examples include upper mantle heterogeneities and anisotropy; fine-scale structures at, above, and below the core–mantle boundary; anisotropy and layering in the lowermost mantle as well as in the inner core; and massive low-velocity provinces in the lower mantle. Such phenomena directly relate to the temperature, chemistry, flow properties, and evolution of the mantle and core, thus motivating seismologists to continue to bring the interior into sharper focus. 

This Special Issue of Geosciences aims to attract seismology-based contributions that elucidate the Earth’s interior, from the deep lithosphere to the center of the planet. Both original research articles and reviews are welcome. Research areas may include (but are not limited to) seismic imaging of the deep lithosphere; subducting slabs; upper and/or lower mantle heterogeneity and anisotropy; D” phenomena; ultra-low-velocity zones; plumes; large low-velocity provinces; the core–mantle boundary region’s fine-scale structure; the outer core’s structure; and the inner core’s structure, heterogeneity, and anisotropy. While we are focused on seismic imaging, multidisciplinary approaches that aid in the interpretation of seismic findings are also welcomed. We anticipate a one-of-a-kind volume that highlights the current state of the seismic imaging of the deep Earth, spanning a wide breadth of methods and data, as well as their implications for the structure, mineralogy, convection, heat flow, and evolution of the Earth.

Prior to submitting a manuscript, we request that interested authors initially submit a proposed title and an abstract of 150–300 words summarizing their intended contribution. Please send these items to the Guest Editors Jonathan Wolf ([email protected]), Ed Garnero ([email protected]), and Sam  Hansen ([email protected]), or to the Geosciences editorial office ([email protected]). Abstracts will be reviewed by the Guest Editors for the purpose of ensuring a proper fit within the scope of this Special Issue. Full manuscripts will undergo single-blind peer-review. We look forward to receiving your contributions.

Abstract submission deadline:

July 20, 2024.

Notification of abstract acceptance:

August 10, 2024.

Dr. Jonathan Wolf
Prof. Dr. Edward Garnero
Prof. Dr. Samantha E. Hansen
Guest Editors

Manuscript Submission Information

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Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Geosciences is an international peer-reviewed open access monthly journal published by MDPI.

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Keywords

  • deep Earth
  • core
  • sublithospheric mantle
  • Earth structure
  • Earth dynamics
  • Earth history
  • core–mantle boundary
  • outer core
  • seismic imaging

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Published Papers (1 paper)

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Research

10 pages, 3373 KiB  
Article
Antipodal Seismic Observation and Sensitivity Kernel for the Liquid Region on the Earth’s Inner Core
by Seiji Tsuboi and Rhett Butler
Geosciences 2024, 14(12), 333; https://doi.org/10.3390/geosciences14120333 - 6 Dec 2024
Viewed by 367
Abstract
It is considered that a part of the inner core surface where iron in the fluid outer core is precipitated may have melted and formed a mushy region, but its position is not well understood seismologically. We recently analyzed seismic waveforms observed at [...] Read more.
It is considered that a part of the inner core surface where iron in the fluid outer core is precipitated may have melted and formed a mushy region, but its position is not well understood seismologically. We recently analyzed seismic waveforms observed at the antipodal station of the seismic source and showed that there are precursors to the PKIIKP phase reflected beneath the inner core boundary. It has been found that this precursory wave can be modeled as a reflection under the liquid/solid interface at a depth of 100 km below the inner core boundary. Here, we use these precursor waves observed at the antipodal station (>179°). The sensitivity kernel of the amplitude of these precursor waves for the shear wave velocity structure on the inner core surface was calculated by the adjoint method, using theoretical seismic waveforms. Our results might be used to locate regions of the inner core surface where the shear wave velocity may be close to zero. Full article
(This article belongs to the Special Issue Seismology of the Dynamic Deep Earth)
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