294 research outputs found
Surface Rupture of the November 2002 M7.9 Denali Fault Earthquake, Alaska, and Comparison to Other Strike-Slip Ruptures
On November 3, 2002, a moment-magnitude (Mw) 7.9 earthquake produced
340 km of surface rupture on the Denali fault and two related faults in central
Alaska. The rupture, which proceeded from west to east, began with a 40-km-long
break on a previously unknown thrust fault. Estimates of surface slip on this thrust
were 3-6 m. Next came the principal surface break, along 220 km of the Denali
fault. There, right-lateral offset averaged almost 5 m and increased eastward to a
maximum of nearly 9 m. Finally, slip turned southeastward onto the Totschunda
fault, where dextral offsets up to 3 m continued for another 70 km. This three-part
rupture ranks among the longest documented strike-slip events of the past two
centuries. The surface-slip distribution supports and clarifies models of
seismological and geodetic data that indicated initial thrusting followed by rightlateral
strike slip, with the largest moment release near the east end of the Denali
fault. The Denali fault ruptured beneath the Trans-Alaska oil pipeline. The
pipeline withstood almost 6 m of lateral offset, because engineers designed it to
survive such offsets based on pre-construction geological studies. The Denali
fault earthquake was typical of large-magnitude earthquakes on major
intracontinental strike-slip faults, in the length of the rupture, the multiple fault
strands that ruptured, and the variable slip along strike
Surface Rupture and Slip Distribution of the Denali and Totschunda Faults
The 3 November 2002 Denali fault, Alaska, earthquake resulted in
341 km of surface rupture on the Susitna Glacier, Denali, and Totschunda faults. The
rupture proceeded from west to east and began with a 48-km-long break on the
previously unknown Susitna Glacier thrust fault. Slip on this thrust averaged about
4 m (Crone et al., 2004). Next came the principal surface break, along 226 km of
the Denali fault, with average right-lateral offsets of 4.5–5.1 m and a maximum offset
of 8.8 m near its eastern end. The Denali fault trace is commonly left stepping and
north side up. About 99 km of the fault ruptured through glacier ice, where the trace
orientation was commonly influenced by local ice fabric. Finally, slip transferred
southeastward onto the Totschunda fault and continued for another 66 km where
dextral offsets average 1.6–1.8 m. The transition from the Denali fault to the Totschunda
fault occurs over a complex 25-km-long transfer zone of right-slip and
normal fault traces. Three methods of calculating average surface slip all yield a
moment magnitude of Mw 7.8, in very good agreement with the seismologically
determined magnitude of M 7.9. A comparison of strong-motion inversions for moment
release with our slip distribution shows they have a similar pattern. The locations
of the two largest pulses of moment release correlate with the locations of
increasing steps in the average values of observed slip. This suggests that slipdistribution
data can be used to infer moment release along other active fault traces.PublishedS23–S52reserve
Argumentation in school science : Breaking the tradition of authoritative exposition through a pedagogy that promotes discussion and reasoning
The value of argumentation in science education has become internationally recognised and has been the subject of many research studies in recent years. Successful introduction of argumentation activities in learning contexts involves extending teaching goals beyond the understanding of facts and concepts, to include an emphasis on cognitive and metacognitive processes, epistemic criteria and reasoning. The authors focus on the difficulties inherent in shifting a tradition of teaching from one dominated by authoritative exposition to one that is more dialogic, involving small-group discussion based on tasks that stimulate argumentation. The paper builds on previous research on enhancing the quality of argument in school science, to focus on how argumentation activities have been designed, with appropriate strategies, resources and modelling, for pedagogical purposes. The paper analyses design frameworks, their contexts and lesson plans, to evaluate their potential for enhancing reasoning through foregrounding the processes of argumentation. Examples of classroom dialogue where teachers adopt the frameworks/plans are analysed to show how argumentation processes are scaffolded. The analysis shows that several layers of interpretation are needed and these layers need to be aligned for successful implementation. The analysis serves to highlight the potential and limitations of the design frameworks
Screening of DUB activity and specificity by MALDI-TOF mass spectrometry
Deubiquitylases (DUBs) are key regulators of the ubiquitin system which cleave ubiquitin moieties from proteins and polyubiquitin chains. Several DUBs have been implicated in various diseases and are attractive drug targets. We have developed a sensitive and fast assay to quantify in vitro DUB enzyme activity using matrix-assisted laser desorption/ionization time-of-flight (MALDI-TOF) mass spectrometry. Unlike other current assays, this method uses unmodified substrates, such as diubiquitin topoisomers. By analyzing 42 human DUBs against all diubiquitin topoisomers we provide an extensive characterization of DUB activity and specificity. Our results confirm the high specificity of many members of the OTU and JAMM DUB families and highlight that all USPs tested display low linkage selectivity. We also demonstrate that this assay can be deployed to assess the potency and specificity of DUB inhibitors by profiling 11 compounds against a panel of 32 DUBs
Stress Field Interactions Between Overlapping Shield Volcanoes : Borehole Breakout Evidence From the Island of Hawai'i, USA
Acknowledgments: This PTA2 borehole investigation was funded by the International Continental Scientific Drilling Program (ICDP) and by VMAPP (Volcanic Margin Petroleum Prospectivity) project (VBPR/DougalEARTH/TGS) in collaboration with the Humu'ula Groundwater Research Project. D. A. J. and S. P. are partly funded through a Norwegian Research Council Centres of Excellence project (project number 223272, CEED). We thank Marco Groh for the logging operations. We thank two anonymous reviewers for the comments and suggestions. We are particularly grateful to the Associate Editor Mike Poland for his valuable comments and his critical review that greatly improved the manuscript.Peer reviewedPublisher PD
The Searsville Lake Site (California, USA) as a candidate Global Boundary Stratotype Section and Point for the Anthropocene Series
Cores from Searsville Lake within Stanford University’s Jasper Ridge Biological Preserve, California, USA, are examined to identify a potential GSSP for the Anthropocene: core JRBP2018-VC01B (944.5 cm-long) and tightly correlated JRBP2018-VC01A (852.5 cm-long). Spanning from 1900 CE ± 3 years to 2018 CE, a secure chronology resolved to the sub-annual level allows detailed exploration of the Holocene-Anthropocene transition. We identify the primary GSSP marker as first appearance of 239,240Pu (372–374 cm) in JRBP2018-VC01B and designate the GSSP depth as the distinct boundary between wet and dry season at 366 cm (6 cm above the first sample containing 239,240Pu) and corresponding to October-December 1948 CE. This is consistent with a lag of 1–2 years between ejection of 239,240Pu into the atmosphere and deposition. Auxiliary markers include: first appearance of 137Cs in 1958; late 20th-century decreases in δ15N; late 20th-century elevation in SCPs, Hg, Pb, and other heavy metals; and changes in abundance and presence of ostracod, algae, rotifer, and protozoan microfossils. Fossil pollen document anthropogenic landscape changes related to logging and agriculture. As part of a major university, the Searsville site has long been used for research and education, serves users locally to internationally, and is protected yet accessible for future studies and communication about the Anthropocene.
PLAIN WORD SUMMARY:
The Global Boundary Stratotype Section and Point (GSSP) for the proposed Anthropocene Series/Epoch is suggested to lie in sediments accumulated over the last ~120 years in Searsville Lake, Woodside, California, USA. The site fulfills all of the ideal criteria for defining and placing a GSSP. In addition, the Searsville site is particularly appropriate to mark the onset of the Anthropocene, because it was anthropogenic activities–the damming of a watershed–that created a geologic record that now preserves the very signals that can be used to recognize the Anthropocene worldwide
1957: Abilene Christian College Bible Lectures - Full Text
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Metabolic consequences of interleukin-6 challenge in developing neurons and astroglia
Abstract Background: Maternal immune activation and subsequent interleukin-6 (IL-6) induction disrupt normal brain development and predispose the offspring to developing autism and schizophrenia. While several proteins have been identified as having some link to these developmental disorders, their prevalence is still small and their causative role, if any, is not well understood. However, understanding the metabolic consequences of environmental predisposing factors could shed light on disorders such as autism and schizophrenia. Methods: To gain a better understanding of the metabolic consequences of IL-6 exposure on developing central nervous system (CNS) cells, we separately exposed developing neuron and astroglia cultures to IL-6 for 2 hours while collecting effluent from our gravity-fed microfluidic chambers. By coupling microfluidic technologies to ultra-performance liquid chromatography-ion mobility-mass spectrometry (UPLC-IM-MS), we were able to characterize the metabolic response of these CNS cells to a narrow window of IL-6 exposure. Results: Our results revealed that 1) the use of this technology, due to its superb media volume:cell volume ratio, is ideally suited for analysis of cell-type-specific exometabolome signatures; 2) developing neurons have low secretory activity at baseline, while astroglia show strong metabolic activity; 3) both neurons and astroglia respond to IL-6 exposure in a cell type-specific fashion; 4) the astroglial response to IL-6 stimulation is predominantly characterized by increased levels of metabolites, while neurons mostly depress their metabolic activity; and 5) disturbances in glycerophospholipid metabolism and tryptophan/kynurenine metabolite secretion are two putative mechanisms by which IL-6 affects the developing nervous system. Conclusions: Our findings are potentially critical for understanding the mechanism by which IL-6 disrupts brain function, and they provide information about the molecular cascade that links maternal immune activation to developmental brain disorders
Teaching Tolerance in a Globalized World: Final Remarks
Each of the five empirical studies presented in this report aimed to identify factors and conditions that help schools and teachers to promote tolerance in a globalized world. Each study acknowledged the complex, hierarchical layers of explanatory mechanisms, while focusing on what could be learned from in-depth analysis of data collected by the International Association for the Evaluation ofEducational Achievement’s International Civic and Citizenship Education Study 2009. In this chapter, key findings are summarized, while acknowledging limitations and caveats, and avenues for further research are identified. The report findings also flag some potential implications for policymakers
KIMA: Noise: A visual sound installation on urban noise
KIMA: Noise is a participatory art piece inviting audiences to explore impact of urban noises interactively. Using specific urban sound sources, the audience experiences noise as spatial soundscapes, responding to it, physically engaging and interacting with it. KIMA: Noise creates awareness for the phenomenon of noise pollution. The paper looks at preeminent research in the field, and draws conclusions of how sound affects us as individuals. The art project KIMA: Noise is introduced technically and conceptually
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