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  • 1
    Series available for loan
    Series available for loan
    A reconnaissance study of the beach sands of Puerto Rico (1957)
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Details Availability
    Call number: SR 90.0001(1042-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 273-305 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1042-I
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
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    A measuring scheme for determining in-situ stresses and moduli at large scale (1997)
    In:  International Journal of Rock Mechanics and Mining Sciences, Warszawa, Inst. Electrical & Electronics Engineers, vol. 34, no. 1, pp. 157-162, pp. L11614, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1997
    Keywords: Stress measurements ; Stress ; Physical properties of rocks
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    BIBLIOGRAPHY SEISMOLOGY
  • 3
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    Prion strain mutation determined by prion protein conformational compatibility and primary structure (2010)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2010-05-15
    Description: Prions are infectious proteins composed of the abnormal disease-causing isoform PrPSc, which induces conformational conversion of the host-encoded normal cellular prion protein PrPC to additional PrPSc. The mechanism underlying prion strain mutation in the absence of nucleic acids remains unresolved. Additionally, the frequency of strains causing chronic wasting disease (CWD), a burgeoning prion epidemic of cervids, is unknown. Using susceptible transgenic mice, we identified two prevalent CWD strains with divergent biological properties but composed of PrPSc with indistinguishable biochemical characteristics. Although CWD transmissions indicated stable, independent strain propagation by elk PrPC, strain coexistence in the brains of deer and transgenic mice demonstrated unstable strain propagation by deer PrPC. The primary structures of deer and elk prion proteins differ at residue 226, which, in concert with PrPSc conformational compatibility, determines prion strain mutation in these cervids.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4097672/" target="_blank"〉〈img src="https://static.pubmed.gov/portal/portal3rc.fcgi/4089621/img/3977009" border="0"〉〈/a〉   〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4097672/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Angers, Rachel C -- Kang, Hae-Eun -- Napier, Dana -- Browning, Shawn -- Seward, Tanya -- Mathiason, Candace -- Balachandran, Aru -- McKenzie, Debbie -- Castilla, Joaquin -- Soto, Claudio -- Jewell, Jean -- Graham, Catherine -- Hoover, Edward A -- Telling, Glenn C -- 1P01AI077774-01/AI/NIAID NIH HHS/ -- 2R01 NS040334-04/NS/NINDS NIH HHS/ -- N01-AI-25491/AI/NIAID NIH HHS/ -- P01 AI077774/AI/NIAID NIH HHS/ -- R01 NS049173/NS/NINDS NIH HHS/ -- T32 AI49795/AI/NIAID NIH HHS/ -- T32 DA022738/DA/NIDA NIH HHS/ -- New York, N.Y. -- Science. 2010 May 28;328(5982):1154-8. doi: 10.1126/science.1187107. Epub 2010 May 13.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Microbiology, Immunology and Molecular Genetics, University of Kentucky Medical Center, Lexington, KY 40536, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20466881" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acid Sequence ; Animals ; Brain/pathology ; Brain Chemistry ; *Deer ; Disease Susceptibility ; Mice ; Mice, Transgenic ; Mutation ; PrPC Proteins/*chemistry/genetics ; PrPSc Proteins/analysis/*chemistry/genetics/pathogenicity ; Protein Conformation ; Protein Folding ; Selection, Genetic ; Serial Passage ; Species Specificity ; *Wasting Disease, Chronic/pathology/transmission
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
    Published by American Association for the Advancement of Science (AAAS)
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  • 4
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    Modest Change In Fluvial Style With Varying Accommodation In Regressive Alluvial-To-Coastal-Plain Wedge: Upper Cretaceous Blackhawk Formation, Wasatch Plateau, Central Utah, U.S.A (2013)
    Society for Sedimentary Geology (SEPM)
    Details
    Publication Date: 2013-03-07
    Description: . Concept-driven sequence stratigraphic models of alluvial-to-coastal-plain successions suggest that fluvial architecture and style should transition from isolated, single-story, channelized sandbodies deposited by single-thread (typically meandering) rivers in mudstone-prone, high-accommodation intervals into densely stacked, amalgamated sandbodies deposited by multiple-thread (typically braided) rivers in low-accommodation intervals. Model predictions of changing fluvial style are tested by comparing the facies character, internal architecture, dimensions, and formative paleohydraulic conditions of representative, major fluvial sandbodies developed at different stratigraphic levels of an alluvial-to-coastal-plain succession developed under a progressively decreasing rate of accommodation creation (Late Cretaceous Blackhawk Formation, Wasatch Plateau, central Utah, USA). The major fluvial sandbodies have a similar facies composition, and consist mainly of cross-bedded, medium-grained sandstone with subordinate mudclast conglomerate, folded sandstone, and inclined sandstones and intercalated siltstones. Facies are arranged within a hierarchy of architectural components. Channel stories (mean width and depth of 90 m and 7.2 m, respectively) represent the migration of a paleochannel segment and adjacent bar, and they are amalgamated laterally into channel belts (mean width and depth of 400 m and 9.2 m, respectively) that in turn are stacked vertically into channel-belt complexes (mean width and depth of 400 m and 20 m, respectively). Channel stories and belts were deposited by a combination of three paleochannel types that occur together in most major sandbodies: (1) single-thread "cut-and-fill" channels; (2) single-thread, laterally accreting channels of low-to-moderate sinuosity; and (3) multiple-thread, wandering-to-braided channels. Estimated paleochannel slopes are uniformly low (〈 0.04°), most sandbodies contain sparse, potential marine indicators (e.g., Teredolites -bored logs and tidally modulated? carbonaceous drapes along cross-bed foresets), and paleodischarge estimates imply that multiple-thread channels may have narrowed and branched downstream to form distributary networks. All of these features are consistent with a delta-plain setting. Channel story and belt stacking patterns within each major sandbody (channel-belt complex) are highly non-uniform, such that (1) there are no systematic trends shared by the sandbodies, (2) sandbodies do not result from systematic, short-term changes in accommodation, such as those associated with the incision and fill of coastal incised valleys, and (3) variability within each sandbody is more pronounced than variability between sandbodies. These results suggest that local variations in sediment flux and transport capacity, combined with local avulsion history, were the principal controls on the architecture and dimensions of the major sandbodies. The similarities in architecture between major fluvial sandbodies imply that these controls were not predominantly governed by proximity to the coeval shoreline (c. 40–100 km) or by long-term tectonic subsidence rate (c. 80–700 m/Myr), which controlled creation of accommodation.
    Print ISSN: 1527-1404
    Topics: Geosciences
    Published by Society for Sedimentary Geology (SEPM)
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  • 5
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    Energy policy: Renewables targeted before Fukushima (2016)
    Nature Publishing Group (NPG)
    Details
    Publication Date: 2016-05-07
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Cherp, Aleh -- Jewell, Jessica -- England -- Nature. 2016 May 5;533(7601):36. doi: 10.1038/533036b.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Central European University, Budapest, Hungary. ; International Institute for Applied Systems Analysis, Laxenburg, Austria.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27147023" target="_blank"〉PubMed〈/a〉
    Keywords: *Fukushima Nuclear Accident ; Humans ; Research/*trends
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Published by Nature Publishing Group (NPG)
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  • 6
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    Late Pleistocene Record of Off‐Fault Deformation and Vertical Slip Rates from the Wasatch Fault Zone, Utah: Implications for Fault Segmentation from Lake Bonneville Shorelines (2019)
    Seismological Society of America (SSA)
    Details
    Publication Date: 2019
    Description: 〈span〉〈div〉Abstract〈/div〉In an effort to better understand the Pleistocene history of the Wasatch fault zone, we evaluate the deformation and displacement of the Bonneville and Provo high‐stand shorelines of Lake Bonneville along the Wasatch Front. We apply an automated shoreline elevation measurement application developed as part of this study to measure Lake Bonneville shoreline elevations along the Weber and Brigham City segments of the fault, adding to a previously published dataset of shoreline elevations on the Salt Lake City segment. Tectonically deformed shorelines on the footwall of the fault demonstrate elevation patterns that are inconsistent with the idea that the Pleasant View salient, a bedrock salient marking the segment boundary between the Weber and Brigham City segments of the fault, is a persistent barrier to fault rupture since the late Pleistocene. Shoreline features are elevated ∼20  m across the segment boundary as compared to shoreline features on the northern part of the Brigham City segment. We suggest the possibility that fault rupture through the Pleasant View salient has been common since the late Pleistocene and speculate that a similar relationship could exist between the Provo and Salt Lake City segments, based on similarities between the shoreline elevation patterns on the Brigham City and Salt Lake City segments of the fault. Vertical slip rates measured from displaced shorelines at the Pleasant View salient (Brigham City–Weber segment boundary) are generally higher compared to those at the Honeyville spur (Collinston–Brigham City segment boundary). Statistically significant vertical slip rates calculated from the Provo shoreline at the Pleasant View salient (0.8±0.5 to 0.9±0.6  mm/yr and 0.7±0.5 to 0.9±0.6  mm/yr) suggest that late Pleistocene vertical slip rates are slightly lower than Holocene rates; however, large uncertainties in the shoreline elevation measurements exist.〈/span〉
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Published by Seismological Society of America (SSA)
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  • 7
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    Late Pleistocene Record of Off‐Fault Deformation and Vertical Slip Rates from the Wasatch Fault Zone, Utah: Implications for Fault Segmentation from Lake Bonneville Shorelines (2019)
    Seismological Society of America (SSA)
    Details
    Publication Date: 2019
    Description: 〈span〉〈div〉Abstract〈/div〉In an effort to better understand the Pleistocene history of the Wasatch fault zone, we evaluate the deformation and displacement of the Bonneville and Provo high‐stand shorelines of Lake Bonneville along the Wasatch Front. We apply an automated shoreline elevation measurement application developed as part of this study to measure Lake Bonneville shoreline elevations along the Weber and Brigham City segments of the fault, adding to a previously published dataset of shoreline elevations on the Salt Lake City segment. Tectonically deformed shorelines on the footwall of the fault demonstrate elevation patterns that are inconsistent with the idea that the Pleasant View salient, a bedrock salient marking the segment boundary between the Weber and Brigham City segments of the fault, is a persistent barrier to fault rupture since the late Pleistocene. Shoreline features are elevated ∼20  m across the segment boundary as compared to shoreline features on the northern part of the Brigham City segment. We suggest the possibility that fault rupture through the Pleasant View salient has been common since the late Pleistocene and speculate that a similar relationship could exist between the Provo and Salt Lake City segments, based on similarities between the shoreline elevation patterns on the Brigham City and Salt Lake City segments of the fault. Vertical slip rates measured from displaced shorelines at the Pleasant View salient (Brigham City–Weber segment boundary) are generally higher compared to those at the Honeyville spur (Collinston–Brigham City segment boundary). Statistically significant vertical slip rates calculated from the Provo shoreline at the Pleasant View salient (0.8±0.5 to 0.9±0.6  mm/yr and 0.7±0.5 to 0.9±0.6  mm/yr) suggest that late Pleistocene vertical slip rates are slightly lower than Holocene rates; however, large uncertainties in the shoreline elevation measurements exist.〈/span〉
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Published by Seismological Society of America (SSA)
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  • 8
    Electronic Resource
    Electronic Resource
    The Inductive Effect and Chemical Reactivity. V. Theoretical Dipole Moments of α,ι-Dichloroalkanes and α,ι-Dibromoalkanes1 (1961)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 83 (1961), S. 3785-3788 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja01479a014
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  • 9
    Electronic Resource
    Electronic Resource
    A colorimetric qualitative test for glycine (1960)
    s.l. : American Chemical Society
    Analytical chemistry 32 (1960), S. 1841-1842 
    Details
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ac50153a039
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  • 10
    Electronic Resource
    Electronic Resource
    Colorimetric Quantitative Method for Determining Glycine in Presence of Other Amino Acids. (1965)
    s.l. : American Chemical Society
    Analytical chemistry 37 (1965), S. 1034-1035 
    Details
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ac60227a023
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