{"id":{"repo_id":"baylor","oai_identifier":"oai:baylor-ir.tdl.org:2104/9814"},"canonical_url":"https://search.dev.ndltd.org/etd/baylor/oai:baylor-ir.tdl.org:2104/9814","repository":{"repo_id":"baylor","name":"Baylor University","base_url":"https://baylor-ir.tdl.org/server/oai/request"},"display":{"title":"Ps receiver function imaging of crustal structure and Moho topography beneath the Northeast Caribbean.","abstract":"The Caribbean plate consists of accreted different geologic terrains bounded by a system of complex plate boundaries. We conduct P-to-S receiver function studies of the Northeast Caribbean in order to image the plate boundary and study the major forces driving tectonics and strain distribution in the region. To calculate a velocity model for migration, we implement a technique analogous to "velocity analysis" in reflection seismology. We image a strong positive amplitude feature that shallows from ~40 km in the west to ~30 km in the east, which we interpret as the Moho. We also image a feature at ~80 km, which we conclude to be a subducting North America (NA) slab pushing against the Caribbean lithosphere. The next step in seismological studies of the Northeast Caribbean region is seismic tomography using teleseismic and local arrivals. This will allow us to gain insight into the volume and location of features.","abstract_html":"The Caribbean plate consists of accreted different geologic terrains bounded by a system of complex plate boundaries. We conduct P-to-S receiver function studies of the Northeast Caribbean in order to image the plate boundary and study the major forces driving tectonics and strain distribution in the region. To calculate a velocity model for migration, we implement a technique analogous to "velocity analysis" in reflection seismology. We image a strong positive amplitude feature that shallows from ~40 km in the west to ~30 km in the east, which we interpret as the Moho. We also image a feature at ~80 km, which we conclude to be a subducting North America (NA) slab pushing against the Caribbean lithosphere. The next step in seismological studies of the Northeast Caribbean region is seismic tomography using teleseismic and local arrivals. This will allow us to gain insight into the volume and location of features.","abstract_has_math":false,"creators":["Ntuli, Gift."],"institution":"Baylor University.","degree_name":"M.S.","degree_level":"Masters","degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":["Pulliam, Jay."],"committee_chairs":[],"committee_members":[],"year":2016,"date_issued":"2016-08","date_published":"2016-08","updated_at":"2026-07-24T01:08:04Z","subjects":["Northeast Caribbean.","Receiver functions."],"languages":["en"],"rights":["Baylor University works 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. Contact libraryquestions@baylor.edu for inquiries about permission."],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://hdl.handle.net/2104/9814","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.advisor","label":"Advisor","values":["Pulliam, Jay."]},{"key":"dc:creator","label":"Author","values":["Ntuli, Gift."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2016-09-01T13:36:02Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2016-09-01T13:36:02Z"]},{"key":"dc:date.issued","label":"Date","values":["2016-08"]},{"key":"dc:type","label":"Dc Type","values":["Thesis"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Masters"]},{"key":"thesis:degree_name","label":"Degree Name","values":["M.S."]},{"key":"thesis:institution_name","label":"Thesis Institution Name","values":["Baylor University."]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Northeast Caribbean.","Receiver functions."]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language.iso","label":"Language (ISO)","values":["en"]},{"key":"dc:rights","label":"Dc Rights","values":["Baylor University works 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. Contact libraryquestions@baylor.edu for inquiries about permission."]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.uri","label":"Identifier URI","values":["https://hdl.handle.net/2104/9814"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["The Caribbean plate consists of accreted different geologic terrains bounded by a system of complex plate boundaries. We conduct P-to-S receiver function studies of the Northeast Caribbean in order to image the plate boundary and study the major forces driving tectonics and strain distribution in the region. To calculate a velocity model for migration, we implement a technique analogous to "velocity analysis" in reflection seismology. We image a strong positive amplitude feature that shallows from ~40 km in the west to ~30 km in the east, which we interpret as the Moho. We also image a feature at ~80 km, which we conclude to be a subducting North America (NA) slab pushing against the Caribbean lithosphere. The next step in seismological studies of the Northeast Caribbean region is seismic tomography using teleseismic and local arrivals. This will allow us to gain insight into the volume and location of features."]},{"key":"dc:format.mimetype","label":"Dc Format Mimetype","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["Ps receiver function imaging of crustal structure and Moho topography beneath the Northeast Caribbean."]}]}],"canonical_facts":{"dc:contributor.advisor":["Pulliam, Jay."],"dc:creator":["Ntuli, Gift."],"dc:date.accessioned":["2016-09-01T13:36:02Z"],"dc:date.available":["2016-09-01T13:36:02Z"],"dc:date.issued":["2016-08"],"dc:description.abstract":["The Caribbean plate consists of accreted different geologic terrains bounded by a system of complex plate boundaries. We conduct P-to-S receiver function studies of the Northeast Caribbean in order to image the plate boundary and study the major forces driving tectonics and strain distribution in the region. To calculate a velocity model for migration, we implement a technique analogous to "velocity analysis" in reflection seismology. We image a strong positive amplitude feature that shallows from ~40 km in the west to ~30 km in the east, which we interpret as the Moho. We also image a feature at ~80 km, which we conclude to be a subducting North America (NA) slab pushing against the Caribbean lithosphere. The next step in seismological studies of the Northeast Caribbean region is seismic tomography using teleseismic and local arrivals. This will allow us to gain insight into the volume and location of features."],"dc:format.mimetype":["application/pdf"],"dc:identifier.uri":["https://hdl.handle.net/2104/9814"],"dc:language.iso":["en"],"dc:rights":["Baylor University works 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. Contact libraryquestions@baylor.edu for inquiries about permission."],"dc:subject":["Northeast Caribbean.","Receiver functions."],"dc:title":["Ps receiver function imaging of crustal structure and Moho topography beneath the Northeast Caribbean."],"dc:type":["Thesis"],"thesis:degree_level":["Masters"],"thesis:degree_name":["M.S."],"thesis:institution_name":["Baylor University."]},"updated_at":"2026-07-24T01:08:04Z"}