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  • 1
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    In:  J. Geophys. Res., Bonn, Pergamon, vol. 92, no. 1, pp. 10485-10510, pp. 2050, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1987
    Keywords: Source ; Fault zone ; Tectonics ; Plate tectonics ; Fault plane solution, focal mechanism ; JGR
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  • 2
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    In:  J. Geophys. Res., Bonn, Pergamon, vol. 93, no. 1, pp. 13589-13608, pp. 2050, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1988
    Keywords: Seismic stratigraphy ; JGR
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  • 3
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    In:  Journal of Geophysical Research, Bonn, Pergamon, vol. 104, no. B6, pp. 13169-13182, pp. 2050, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1999
    Keywords: Physical properties of rocks ; Borehole geophys. ; Borehole Compensated Sonic log ; cracks and fractures (.NE. fracturing) ; Fluids ; JGR
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  • 4
    Publication Date: 2019
    Description: Abstract We present a new synthesis of oceanic crustal structure from two‐dimensional seismic profiles to explore differences related to spreading rate and age. Primary results are as follows: (1) Layer 2 has an average thickness of 1.84 km but is thicker for young slow‐spreading crust and thinner for young superfast‐spreading crust. At faster‐spreading rates the layer 2/3 boundary likely corresponds to the lithologic boundary between dikes and gabbros. At slow‐spreading centers, the layer 2/3 boundary is interpreted to mark a change in porosity with depth within the dikes. (2) Total crustal thickness averages 6.15 km and is similar across all spreading rates. (3) Velocities at the top of layer 2 increase rapidly from 3.0 km/s at 0 Ma to 4.6 km/s at 10.5 Ma, with a slower increase to 5.0 km/s at 170 Ma. The rapid increase in velocity at young ages is attributed to crack closure by precipitation of hydrothermal alteration products; the increase at older ages suggests that this process persists as the oceanic crust evolves. (4) There is a correlation between velocities at the top of layer 2 and sediment thickness, with velocities of 5.8–5.9 km/s associated with a sediment thickness of 4.0–4.3 km. The thick sediment may collapse large‐scale features such as lava tubes and fractures. (5) Average velocities at the top of layer 3 are lower for young slow‐spreading and intermediate‐spreading oceanic crust (6.1–6.2 km/s) than for older or faster‐spreading oceanic crust (6.5–6.7 km/s). These low velocities are likely associated with faults penetrating into the sheeted dikes.
    Print ISSN: 8755-1209
    Electronic ISSN: 1944-9208
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Publication Date: 2011-09-23
    Description: The rate of generation of internal gravity waves in the lee of small length scale topography by geostrophic flow in the World Ocean was estimated using linear theory with corrections for finite amplitude topography. Several global data sets were combined for the calculation including an ocean circulation model for the near-bottom geostrophic flow statistics, over 500 abyssal current meter records, historical climatological data for the buoyancy frequency, and two independent estimates of the small scale topographic statistical properties. The first topography estimate was based on an empirically-derived relationship between paleo-spreading rates and abyssal hill roughness, with corrections for sedimentation. The second estimate was based on small-scale (
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
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    American Association for the Advancement of Science (AAAS)
    Publication Date: 2015-09-05
    Description: Crowley et al. (Reports, 13 March 2015, p. 1237) propose that abyssal hill topography can be generated by variations in volcanism at mid-ocean ridges modulated by Milankovitch cycle-driven changes in sea level. Published values for abyssal hill characteristic widths versus spreading rate do not generally support this hypothesis. I argue that abyssal hills are primarily fault-generated rather than volcanically generated features.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Goff, John A -- New York, N.Y. -- Science. 2015 Sep 4;349(6252):1065. doi: 10.1126/science.aab2350.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26339022" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The dependence of acoustic backscatter variations on sediment grain-size distribution is examined using a combined analysis of 95 kHz side-scan data and approx. 300 grab samples from the New Jersey margin. We show that, under well-controlled circumstances, an unprecedented degree of correlation can be obtained between backscatter intensity and mean grain size. However, backscatter is disproportionately affected by larger grain sizes. Addition of just a few extra weight percentage of the larger grain sizes (〉4 mm), which in our study is typically represented by more abundant shell hash among the older sediments at greater water depths, can completely degrade this correlation.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We have developed statistical models of upper and middle crustal seismic velocity heterogeneity based on geologic maps and petrophysical data from the Lewisian gneiss complex, Scotland. the level of heterogeneity we have measured is relevant to seismic exploration of the crystalline crust using conventional reflection and refraction techniques. We digitized two 1:10560 geologic maps of Laxfordian (Archean) age Lewisian rocks on a 26.8m grid. Both maps are believed to be representative of the upper and middle crust in north-western Scotland, and both are believed to provide cross-sectional views of parts of the crust. the digital maps were characterized by the statistics of their lithologic populations and by their 2-D spatial autocorrelation functions. Different lithologies were assigned seismic velocities appropriate for the mid-crust using petrophysical data. Three lithologies are dominant: silicic gneisses (Vp∼6.2 km s−1), mafic amphibolites (Vp— 6.75 kms−1), and intermediate composition schists (Vp—6.5kms−1). Both maps have self-affine spatial fabrics.The first map covers the core of a syncline. Its autocorrelation function defines a medium with a fractal dimension of 2.78, a horizontal characteristic length of about 244m and a vertical correlation of about 133m (aspect ratio is 2:1). It has an essentially trimodal velocity (lithology) population consisting of 37 per cent silicicgneiss, 43 per cent mafic amphibolites, and 20 per cent schists. This map is representative of 30-40 per cent of Laxfordian rocks. the second map is a plan view which can be rotated 90° about an axis perpendicular to strike to give a cross-section. This map is characterized by a fractal dimension of 2.55, with a horizontal correlation length of about 111m and a vertical correlation of about 38m (aspect ratio 3:1). It has a nearly bimodal population consisting of 77 per cent silicic gneisses and 22 per cent mafic amphibotites. It is representative of 60-70 per cent of Laxfordian rocks.Lastly we examine the seismic response of an upper to middle crust based on our statistical models using acoustic and elastic 2-D finite-difference synthetic seismograms. Short-offset shot records demonstrate that a Lewisian upper crust produces scattered waves which significantly disrupt signals reflecting from deeper levels. Measurements of transmission scattering Q, and coda decay rates confirm that seismic scattering in Lewisian-type crust is strong. the migrated CMP response of a Lewisian crustal model shows the characteristic ‘salt and pepper’ pattern often observed in the upper crust, and described, incorrectly, as ‘transparent'. We suggest that ‘translucent’ is a more appropriate descriptor.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-0581
    Keywords: East Pacific Rise ; multibeam sonar surveying ; Mid-Ocean Ridge ; magmatic plumbing system
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Detailed bathymetric data from a Hydrosweep multibeam sonar survey of a 250 km-long portion of the ‘superfast’-spreading southern East Pacific Rise crest and flanks show that the along-axis variation in morphology and axial depth differs significantly from that observed at the fast-spreading northern East Pacific Rise. While the deep mantle upwelling pattern is similar under the northern and southern East Pacific Rise, our observations require that the connectivity of the shallow, subcrestal plumbing system be more efficient beneath the ‘super-fast’ spreading southern East Pacific Rise than beneath the slower spreading northern East Pacific Rise.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2016-03-22
    Description: An ultra-high resolution acoustic reflection survey within Corpus Christi Bay, Texas, reveals numerous oyster reefs that have died off and been buried by subsequent sedimentation. The die-offs occurred in four temporal clusters, as evidenced by nearly coterminous capping horizons across multiple reef heads. These horizons can be correlated to published, calibrated radiocarbon dates (2- uncertainty: ± ~900 years) derived from cored sediments, and placed into the stratigraphic context. The reefs began growing with the initial flooding of the bay at ~9600 ybp. The first die-offs are coincident with the transition from upper bay to open bay environment at ~8140 ybp, with the greatest concentration of die-offs seaward. Subsequent die-offs occurred ~7600, 6870, and 5800 ybp, with a seaward-to-landward progression. These ages appear to either post-date or be concurrent with published periods of accelerated sea level rise of ~1–4 m. However, because bay oysters ( Crassostrea virginica ) are robust with respect to salinity and depth changes, we cannot directly link die-offs with punctuated sea level rise. We hypothesize instead that reef die-offs are associated with extreme salinity changes caused by droughts, based on observations during the 1950s Texas drought. During that event, bay reefs were colonized by open-ocean species ( Crassostrea equestris ), which gradually replaced bay oysters progressing seaward to landward in concentration. Subsequent flooding and rapid freshening of the bay caused massive mortality of the colonizing species. These floods also brought abundant fine-grained sedimentation that could bury reefs before they could be recolonized. Such a sequence of events could explain widespread early Holocene, seaward-to-landward oyster reef die-offs during times of more frequent and severe drought conditions. A plausible climatological link exists between periods of low rainfall in Texas and periods of accelerated melting of the polar ice cap, which could explain the evident correlation between reef die-off and sea level rise.
    Print ISSN: 0959-6836
    Electronic ISSN: 1477-0911
    Topics: Geography , Geosciences
    Published by Sage
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