Doctoral Dissertations
Keywords and Phrases
Complex anisotropy; Mantle Dynamics; Seismic Anisotropy; Shear wave splitting; Splitting parameters; Tien Shan Orogenic Belt
Abstract
"In spite of numerous studies, the mechanisms for the crustal shortening, mountain formation and associated tectonism leading to complex or simply seismic anisotropy formation beneath the Tien Shan Orogenic Belt is still debated. The most popular hypotheses suggested for the existence of seismic anisotropy are small-scale mantle convection, regional scale resistive basal shear and APM induced asthenospheric flow. Here, we used shear-wave splitting (SWS) measurements with good azimuthal coverage to provide additional constraints on the various models proposed by previous studies. One of the most effective approaches utilized to constrain convective mantle flow patterns is the splitting of P-to-S converted phases at the core-mantle boundary on the receiver side (XKS including PKS, SKKS, and SKS). Consequently, a robust procedure involving automatic and manual batch processing to reliably assess and objectively rank shear-wave splitting parameters were used. The resulting 2089 pairs of well-defined XKS splitting parameters obtained from 25 stations located in the study area were broad enough to make a reliable determination about the existence or absence of complex anisotropy. Out of the 25 stations, measurements from 10 stations show insignificant azimuthal variations, the majority of stations demonstrating strike parallel E-W fast orientation. A remarkable feature of the fast orientations observed at the 15 stations is a clear azimuthal variation with a 900 periodicity, indicating the existence of two-layer anisotropy. Thus, the strike-parallel upper layer anisotropy is caused by lithospheric shortening, and anisotropy in the lower layer is associated with WNW-ward flow of asthenospheric material sandwiched between the subducting Tarim lithosphere and the thick Kazakh lithospheric root"--Abstract, page iv.
Advisor(s)
Gao, Stephen S.
Committee Member(s)
Liu, Kelly H.
Rogers, David J.
Anderson, Neil L. (Neil Lennart), 1954-
Mickus, Kevin L.
Department(s)
Geosciences and Geological and Petroleum Engineering
Degree Name
Ph. D. in Geology and Geophysics
Publisher
Missouri University of Science and Technology
Publication Date
Spring 2015
Pagination
xii, 112 pages
Note about bibliography
Includes bibliographic references (pages 107-111).
Geographic Coverage
Tien Shan
Rights
© 2015 Solomon Gerra Cherie, All rights reserved.
Document Type
Dissertation - Open Access
File Type
text
Language
English
Subject Headings
Shear waves -- MeasurementAnisotropyEarth (Planet) -- MantleOrogenic belts -- Tien Shan
Thesis Number
T 10710
Electronic OCLC #
913389914
Recommended Citation
Cherie, Solomon Gerra, "Shear wave splitting analysis beneath Tien Shan: Geodynamic implications of complex anisotropy" (2015). Doctoral Dissertations. 2379.
https://scholarsmine.mst.edu/doctoral_dissertations/2379