Introduction
Introduction Statistics Contact Development Disclaimer Help
DTIC ADA472608: Seismic and Gravitational Studies of Melting in the...
by Defense Technical Information Center
Thumbnail
Download
Web page
This thesis presents three studies which apply
geophysical tools to the task of better understanding
mantle melting phenomena at the upper and lower
boundaries of the mantle. The first study uses seafloor
bathymetry and small variations in the gravitational
acceleration over the Hawaii-Emperor seamount chain to
constrain the changes in the igneous production of the
hot spot melting in the mantle which has created these
structures over the past 80 My. The second study uses
multichannel seismic reflection data to constrain the
location and depth of axial magma chambers at the
Endeavour Segment of the Juan de Fuca spreading ridge,
and then correlates these magma chamber locations with
features of the hydrothermal heat extraction system in
the upper crust such as microseismicity caused by thermal
cracking and high temperature hydrothermal vent systems
observed on the seafloor. The third study uses two-
dimensional global pseudospectral seismic wave
propagation modeling to characterize the sensitivity of
the SPdKS seismic phase to two-dimensional, finite-width
ultra-low velocity zones (ULVZs) at the core-mantle
boundary. Together these three studies highlight the
dynamic complexities of melting in the mantle while
offering new tools to understand that complexity.
Date Published: 2018-06-14 04:52:31
Identifier: DTIC_ADA472608
Item Size: 222000126
Language: english
Media Type: texts
# Topics
DTIC Archive; Van Ark, Emily M ; WOOD...
# Collections
dticarchive
additional_collections
# Uploaded by
@chris85
# Similar Items
View similar items
PHAROS
You are viewing proxied material from tilde.pink. The copyright of proxied material belongs to its original authors. Any comments or complaints in relation to proxied material should be directed to the original authors of the content concerned. Please see the disclaimer for more details.