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The Global ETD Search service is a free service for researchers
to find electronic theses and dissertations. This service is
provided by the
Networked Digital Library of Theses and Dissertations.
Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
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Showing 1 to 10 of 47 (0.038 seconds)Spelling suggestions: "subject:"mind ocean bridges""
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Ecology of deep-sea hydrothermal ventsCopley, Jonathan Timothy Peter January 1998 (has links)
No description available.
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Interactions between mantle plumes and mid-ocean ridges : constraints from geophysics, geochemistry, and geodynamical modeling /Georgen, Jennifer E. January 1900 (has links)
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2001. / "September 2001." Vita. Page 223 blank. Includes bibliographical references.
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Examining the effects of mid ocean ridge topography on 3D marine magnetometric resistivity model responses /Lassner, Lisa A. January 1900 (has links)
Thesis (M.S.)--Joint Program in Oceanography/ Applied Ocean Science and Engineering, Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution, 2003. / Includes bibliographical references (p. 768-69).
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Seismic and hydroacoustic investigations near Ascension Island /Hanson, Jeffrey Acton, January 1998 (has links)
Thesis (Ph. D.)--University of California, San Diego, 1998. / Vita. Includes bibliographical references.
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Magmatic processes at mid-ocean ridges evidence from lavas and melt inclusions from the southeast Indian ridge, the Endeavor Segment of the Juan de Fuca Ridge, and the Northern East Pacific Rise /Sours-Page, Rachel E. January 2000 (has links)
Thesis (Ph. D.)--Oregon State University, 2000. / Includes bibliographical references (leaves 141-151).
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Magmatic processes at mid-ocean ridges : evidence from lavas and melt inclusions from the Southeast Indian Ridge, the Endeavour Segment of the Juan de Fuca Ridge, and the northern East Pacific Rise /Sours-Page, Rachel E. January 1900 (has links)
Thesis (Ph. D.)--Oregon State University, 2001. / Typescript (photocopy). Includes bibliographical references (leaves 141-151). Also available on the World Wide Web.
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Melt and deformation in the mantle beneath mid-ocean ridges a textural and lattice-preferred orientation study of abyssal peridotites /Achenbach, Kay L. January 2008 (has links)
Thesis (Ph.D.)--University of Wyoming, 2008. / Title from PDF title page (viewed on Mar. 22, 2010). Appendices are available as supplemental PDF files. Includes bibliographical references (p. 249-263).
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Convection and melting processes in a mantle plume under a spreading ridge, with application to the Iceland plumeRuedas, Thomas. January 1900 (has links)
Thesis (doctoral)--Johann Wolfgang Goethe Universität, 2004. / Includes bibliographical references (p. [270]-299).
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Mantle melting and heterogeneity along mid-ocean ridges : insight from basalt geochemistry along axial depth and morphologic gradients for intermediate spreading rate systems /Russo, Christopher J. January 1900 (has links)
Thesis (Ph. D.)--Oregon State University, 2008. / Printout. Includes bibliographical references (leaves 171-186). Also available on the World Wide Web.
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Earthquake and volcanic processes at mid-ocean ridgesTan, Yen Joe January 2019 (has links)
In this thesis, I present results that broadly fall into two themes. The first involves understanding active tectonic and magmatic processes at mid-ocean ridges. The second involves using small stress changes due to the tides to probe earthquake processes at mid-ocean ridges. The four main results of my thesis are as follow: (1) The spatiotemporal evolution of an eruption at a fast-spreading mid-ocean ridge, the East Pacific Rise, is now characterized and understood to be mainly controlled by the buildup of tectonic stress to a critical level rather than magma overpressure. (2) Microearthquakes at the East Pacific Rise are found to be strongly modulated by tides in the years before an eruption but not immediately after the eruption, suggesting the potential utility of tidal triggering strength for eruption forecasting. (3) Earthquake size-frequency distribution, often quantified using the b value, is shown to vary systematically with tidal stresses which lends support to the use of earthquake b value as an in-situ stressmeter. (4) The 2015 Axial Seamount eruption is revealed to be preceded by variable rates of melt influx into the shallow reservoir, highlighting the short-timescale variability of magmatic systems as they are primed for an eruption.
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