Title Information
Title
Upper Mantle Processes and Structures Imaged with Shear-wave Splitting and Ps and Sp Receiver Functions
Name: Personal
Name Part
Abt, David L.
Role
Role Term: Text
creator
Origin Information
Copyright Date (keyDate="yes", encoding="w3cdtf")
2009
Physical Description
Extent
xiv, 265 p.
digitalOrigin
born digital
Note
Thesis (Ph.D.) -- Brown University (2010)
Name: Personal
Name Part
Fischer, Karen
Role
Role Term: Text
director
Name: Personal
Name Part
Forsyth, Donald
Role
Role Term: Text
reader
Name: Personal
Name Part
Parmentier, Edgar
Role
Role Term: Text
reader
Name: Personal
Name Part
Saal, Alberto
Role
Role Term: Text
reader
Name: Personal
Name Part
Abers, Geoffrey
Role
Role Term: Text
reader
Name: Corporate
Name Part
Brown University. Geological Sciences
Role
Role Term: Text
sponsor
Genre (aat)
theses
Abstract
The interaction between Earth's relatively rigid tectonic plates and relatively viscous convecting upper mantle fundamentally influences myriad processes ranging from arc and intraplate volcanism to orogenesis and rifting. The work presented here addresses two of the most basic concepts of plate tectonics regarding this interaction: (1) the pattern of upper mantle flow in subduction zones, and (2) the thickness and internal structure of continental lithosphere. Chapters 1-3 are devoted to the observation, modeling, and interpretation of local-S and teleseismic SK(K)S splitting measured by the TUCAN seismic array in the Central American subduction zone. Both the splitting measurements themselves and the tomographic model derived from them demonstrate the need for significant arc-parallel anisotropic fabric, inferred to indicate arc-parallel mantle wedge flow; trends in arc lava radiogenic isotopes (Appendix A) provide independent evidence for the existence of arc-parallel flow. The primary implications of these results are that (1) two-dimensional corner flow models and any predictions derived from them are unlikely to be accurate in southeastern Central America, (2) the three-dimensional and finite lateral extent of subduction probably plays a significant role in determining the pattern of wedge and sub-slab flow, and (3) the degree of coupling between the subducting plate and surrounding mantle may be lower than expected. Chapter 4 presents a receiver function study across North America that uses both Ps and Sp data to estimate the depth of the lithosphere-asthenosphere boundary (LAB), as well as other lithospheric discontinuities. Along with other geophysical data (e.g., heat flow, xenoliths, reflection profiles), the differences in inferred LAB depth between the receiver functions and surface waves and the variation in negative Sp energy indicate that (1) the velocity contrast between lithosphere and asthenosphere in the western U.S. is larger, perhaps due to both elevated temperatures and the presence of asthenospheric partial melt, (2) the velocity gradient at the LAB in cratonic North America likely occurs over more than 30 km and can be explained purely thermally, and (3) significant lithospheric layering likely exists in the central and eastern U.S.
Subject (Local)
Topic
shear-wave splitting
Subject (Local)
Topic
mantle wedge
Subject (Local)
Topic
seismic anisotropy
Subject (Local)
Topic
receiver functions
Subject (Local)
Topic
lithosphere-asthenosphere boundary
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1152453")
Topic
Tomography
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1244535")
Geographic
Central America
Subject (FAST) (authorityURI="http://id.worldcat.org/fast", valueURI="http://id.worldcat.org/fast/1242475")
Geographic
North America
Record Information
Record Content Source (marcorg)
RPB
Record Creation Date (encoding="iso8601")
20091218
Language
Language Term: Code (ISO639-2B)
eng
Language Term: Text
English
Identifier: DOI
10.7301/Z0SQ8XPM
Access Condition: rights statement (href="http://rightsstatements.org/vocab/InC/1.0/")
In Copyright
Access Condition: restriction on access
Collection is open for research.
Type of Resource (primo)
dissertations