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Massachusetts Institute of Technology

The earth's interior from both a seismological and petrological perspective

Abstract

dc:description.abstract

Shear-wave splitting measurements of teleseismic shear waves, such as SKS, have been used to estimate the amount and direction of upper-mantle anisotropy worldwide. One of the basic assumptions in making these measurements is that the anisotropy is confined to a single, homogeneous layer. In this thesis, I use both numerical and analytical modeling to examine the validity of this assumption. I find that variability in the orientation of anisotropy with depth causes observable effects, such as frequency dependence in the apparent splitting parameters, and that the measured fast-axis direction is consistently different than the average of the medium. A separate focus of this thesis is how spatial associations between minerals in a thin-section can be used to infer the evolutionary pressure-temperature history of a rock. I present a new method for textural analysis that uses digital images obtained with the electron microprobe. This method is used to characterize nine mantle xenoliths erupted from kimberlite pipes in South Africa and to test whether the pyroxenes are spatially correlated with the garnets. The observed associations can be explained by a model in which harzburgitic residues are produced by large extents of partial melting at shallow depths (-60-90 km) and high temperatures (1300-1400ʻ C) and are then subsequently dragged down to greater depths where garnet and clinopyroxene exsolve, perhaps in an Archean subduction zone. The third focus of this thesis is on the seismological evidence for compositional heterogeneity in the lower mantle. Using reprocessed ISC data, I compare P and S wave tomographic models and find systematic differences between regions that have undergone subduction in the last 120 million years and those that have not below -1500 km.

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2002

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Saltzer, Rebecca Lee
Advisor dc:contributor.advisor
  • Robert D. van der Hilst.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/16815

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
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citation

Saltzer, Rebecca Lee. The earth's interior from both a seismological and petrological perspective. Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/16815