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Massachusetts Institute of Technology

Evolution of upper mantle beneath East Asia and the Tibetan Plateau from P-wave tomography

Abstract

dc:description.abstract

The main objective of the research presented in this thesis is to improve our understanding for the evolution of the upper mantle beneath East Asia and the Tibetan Plateau through high resolution P-wave tomography. The approach to high resolution tomography is based on (i) the combined use of a large range of different types of seismic data, (ii) the use of approximate finite frequency sensitivity kernels to account for difference in measurement technique and frequency content of the data, (iii) the use of an irregular grid with cell-size adapted to sampling density, and (iv) the use of a priori information, e.g., on crustal structure from receiver function analysis. I construct a multi-scale and high resolution seismic tomography model of the upper mantle structure beneath East Asia and the Tibetan Plateau. The new model reveals that the mantle structure associated with the Indian subduction varies considerably along the strike of the collision zone. From west to east, the dip angle of Indian subduction increases and the distance over which the plate underthrusts the Tibetan Plateau decreases. Oblique subduction and changes of dip angle in the central part of the collision zone may cause and determine the location of the north-south trending normal faults in central Tibet. The eastward retreating slabs of western Pacific and Philippine plates are deflected in the transition zone beneath the Korea, Japan Sea, and East China. Some of Mesozoic subducted slabs have reached as far west as 1100E longitude under the Yangtze Craton, which might have resulted from the Eocene subduction at the South China and Japan trenches.

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
2007

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Li, Chang, Ph.D.
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.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/40964
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/40964

Chain of custody

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

Li, Chang, Ph.D.. Evolution of upper mantle beneath East Asia and the Tibetan Plateau from P-wave tomography. Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1721.1/40964