Complex anisotropy beneath the Peruvian flat slab from frequency-dependent, multiple-phase shear wave splitting analysis

Flat or shallow subduction is a relatively widespread global occurrence, but the dynamics remain poorly understood. In particular, the interaction between flat slabs and the surrounding mantle flow has yet to be studied in detail. Here we present measurements of seismic anisotropy to investigate mantle flow beneath the Peruvian flat-slab segment, the largest present-day region of flat subduction. We conduct a detailed shear wave splitting analysis at a long-running seismic station (NNA) located near Lima, Peru. We present measurements of apparent splitting parameters (fast direction ? and delay time ?t) for SKS, ScS, and local S phases from 80 events. We observe well-defined frequency dependence and backazimuthal variability, indicating the likely presence of complex anisotropy. Forward modeling the observations with two or three layers of anisotropy reveals a likely layer with a trench-normal fast direction underlying a layer with a more trench-oblique (to trench-subparallel) fast direction. In order to further constrain the anisotropic geometry, we analyzed the source-side splitting from events originating within the slab measured at distant stations. Beneath the flat-slab segment, we found trench-normal fast splitting directions in the subslab mantle, while within the dipping portion of the slab further to the east, likely trench-subparallel anisotropy within the slab itself. This subslab pattern contradicts observations from elsewhere in South America for “normal” (i.e., more steeply dipping) slab conditions. It is similar, however, to inferences from other shallowly dipping subduction zones around the world. While there is an apparent link between slab dip and the surrounding mantle flow, at least beneath Peru, the precise nature of the relationship remains to be clarified

Rethinking the “Best Interests” of the Child: Voices from Aboriginal Child and Family Welfare Practitioners

n Victoria, recent reforms to the child and family welfare system, through the introduction of the Children Youth and Families Act (2005), have significantly strengthened the principle of the ‘‘best interests’’ of the child. Giving substance to the principle, this legislation defines a set of standards and a practice framework to guide its application. How this is to be applied is of particular interest to the Aboriginal child and family welfare sector, given that the principle of best interests has historically underpinned the removal of thousands of Aboriginal and Torres Strait Islander children from their families on the basis of their race (Bamblett, 2006). This paper presents the findings of a qualitative research study that aimed to identify an Aboriginal perspective on the best interests principle as it applies to Victorian Aboriginal children. In-depth interviews were conducted with six experienced Aboriginal child and family welfare practitioners. The outcomes of this study highlight the distinct cultural perspectives that inform Aboriginal child and family welfare practice and raise a number of concerns in regard to an ongoing ethnocentric application of the principle by mainstream service providers. Key findings of the study are discussed, including the importance of increasing understanding of Aboriginal child-rearing practices, recognising that there is a distinct Aboriginal understanding of what constitutes a best interests framework, and the implications of this for both Aboriginal and mainstream child and family welfare practice. The paper discusses these findings within the context of recent Victorian legislative reform, which promotes Aboriginal self-determination, and argues that more work is needed to ensure Aboriginal perspectives are incorporated into service provision to Aboriginal children and families if we are truly to meet the best interests of Aboriginal children

Cost effectiveness analysis of Year 2 of an elementary school-located influenza vaccination program-Results from a randomized controlled trial.

BackgroundSchool-located vaccination against influenza (SLV-I) has the potential to improve current suboptimal influenza immunization coverage for U.S. school-aged children. However, little is known about SLV-I's cost-effectiveness. The objective of this study is to establish the cost-effectiveness of SLV-I based on a two-year community-based randomized controlled trial (Year 1: 2009-2010 vaccination season, an unusual H1N1 pandemic influenza season, and Year 2: 2010-2011, a more typical influenza season).MethodsWe performed a cost-effectiveness analysis on a two-year randomized controlled trial of a Western New York SLV-I program. SLV-I clinics were offered in 21 intervention elementary schools (Year 1 n = 9,027; Year 2 n = 9,145 children) with standard-of-care (no SLV-I) in control schools (Year 1 n = 4,534 (10 schools); Year 2 n = 4,796 children (11 schools)). We estimated the cost-per-vaccinated child, by dividing the incremental cost of the intervention by the incremental effectiveness (i.e., the number of additionally vaccinated students in intervention schools compared to control schools).ResultsIn Years 1 and 2, respectively, the effectiveness measure (proportion of children vaccinated) was 11.2 and 12.0 percentage points higher in intervention (40.7 % and 40.4 %) than control schools. In year 2, the cost-per-vaccinated child excluding vaccine purchase ($59.88 in 2010 US$) consisted of three component costs: (A) the school costs ($8.25); (B) the project coordination costs ($32.33); and (C) the vendor costs excluding vaccine purchase ($16.68), summed through Monte Carlo simulation. Compared to Year 1, the two component costs (A) and (C) decreased, while the component cost (B) increased in Year 2. The cost-per-vaccinated child, excluding vaccine purchase, was$59.73 (Year 1) and $59.88 (Year 2, statistically indistinguishable from Year 1), higher than the published cost of providing influenza vaccination in medical practices ($39.54). However, taking indirect costs (e.g., averted parental costs to visit medical practices) into account, vaccination was less costly in SLV-I ($23.96 in Year 1,$24.07 in Year 2) than in medical practices.ConclusionsOur two-year trial's findings reinforced the evidence to support SLV-I as a potentially favorable system to increase childhood influenza vaccination rates in a cost-efficient way. Increased efficiencies in SLV-I are needed for a sustainable and scalable SLV-I program

Anisotropy and deformation in the Earth's mantle : seismological observations, geodynamical models, and laboratory experiments

Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2006.This electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections."June 2006."Includes bibliographical references (p. 289-316).In this thesis I report the results of several studies of elastic anisotropy and deformation in the Earth's mantle, using shear wave splitting measurements, numerical models of geodynamical processes, and laboratory experiments on mantle minerals. I evaluate the performance of several methods for measuring shear wave splitting at broadband stations, and discuss how different measurements can inform our interpretation of mantle anisotropy. I describe a set of shear wave splitting measurements from both teleseismic and local earthquakes at 65 stations of the F-net array in Japan. I find considerable evidence from the measured splitting patterns for complex and heterogeneous anisotropy beneath Japan associated with the subduction of the Pacific and Philippine Sea plates beneath Eurasia. The comparison of teleseismic and local splitting at stations in southwestern Japan provides strong evidence for trench-parallel anisotropy in the mantle wedge above the subducting slab. I consider several scenarios that would produce the observed anisotropy and conclude that the most likely model for deformation beneath the Ryukyu arc is corner flow in the mantle wedge, with a region extending ~ 150 kilometers from the trench dominated by B-type olivine fabric.(cont.) To characterize further the detailed pattern of flow and anisotropy, I evaluate a series of two-dimensional finite element models that describe the subduction of the Philippine Sea plate beneath southwestern Japan, and compare the resulting flow field, strain, and anisotropy in the mantle wedge to F-net shear wave splitting observations. To complement this forward modeling approach, I develop and implement a method for the 2.5-D inversion of shear wave splitting intensity measurements for anisotropic structure in the upper mantle. I present preliminary anisotropic models for southwestern Japan and discuss strategies for explicitly integrating the tomographic inversion of splitting intensity data with numerical models that describe geodynamic processes in the wedge. Finally, I describe a series of laboratory experiments characterizing deformation and the resulting lattice preferred orientation in magnesiowüstite, a lower mantle mineral, and discuss the implications for the interpretation of seismic anisotropy at the base of the mantle.by Maureen Devaney Long.Ph.D

Seismic anisotropy in Eastern Tibet from shear wave splitting reveals changes in lithospheric deformation

Knowledge about seismic anisotropy can provide important insight into the deformation of the crust and upper mantle beneath tectonically active regions. Here we focus on the southeastern part of the Tibetan plateau, in Sichuan and Yunnan provinces, SW China. We measured shear wave splitting of core-refracted phases (SKS and SKKS) at a temporary array of 25 IRIS-PASSCAL stations. We calculated splitting parameters using a multi-channel and a single-record cross-correlation method. Multiple layers of anisotropy cannot be ruled out but are not required by the data. A Fresnel zone analysis suggests that the shallow mantle (between 60 and 160 km depth) is the most likely source of anisotropy. The polarization directions reveal a pronounced transition from primarily north–south in the north (Sichuan) to mostly east–west orientations in the south (Yunnan). In the southern part of the study region, that is, south of ~26°N, the fast polarization directions do not correlate well with known surface features and geodetic estimates of the crustal displacement fields. Whereas GPS campaigns provide evidence suggesting north–south crustal flow across the Red River Fault, the pattern of anisotropy argues against such flow in the upper mantle. These observations support models that allow differential movement of upper crust relative to lithospheric mantle. In the northern part of the study region the relationships are more ambiguous and coherent deformation of the crust and mantle lithosphere cannot be excluded. The interpretation of the shear wave splitting results is non-unique, but we suggest that the observed N–S transition reflects a fundamental change in deformation regime across our study region. It may be related to lateral variations in lithospheric rheology, or may mark a transition from the direct impact of the continental collision to dominance of the far-field strain field associated with regional subduction processes. Understanding the nature of the lateral change in deformation regime may prove critical for our understanding the geotectonic evolution of (eastern) Tibet

Chikungunya outbreak in Karachi Pakistan 2016-2017: An analysis of viral isolates

In December 2016 physicians in Karachi, Pakistan,witnessed an increase in patients presenting with febrile illness and severe polyarthralgia. Subsequently, chikungunya virus (CHIKV)) was isolated from three patients. This virus was sequenced and compared with other isolates of CHIKV obtained in India and Pakistan during recent outbreaks. Phylogenetic analysis indicated that the Karachi isolates were most similar to the East Central South African CHIKV lineage and showed sequence homology to isolates obtained in other parts of Pakistan and India. More importantly, two of the CHIKV isolates had a nucleotide substitution in the E1 gene corresponding to an amino acid change at chain F portion of the E1 protein

Wavefield Migration Imaging of Moho Geometry and Upper Mantle Structure Beneath Southern New England

The crust and upper mantle beneath the New England Appalachians exhibit a large offset of the Moho across the boundary between Laurentia and accreted terranes and several dipping discontinuities, which reflect Paleozoic or younger tectonic movements. We apply scattered wavefield migration to the SEISConn array deployed across northern Connecticut and obtain insights not previously available from receiver function studies. We resolve a doubled Moho at a previously imaged Moho offset, which may reflect westward thrusting of rifted Grenville crust. The migration image suggests laterally variable velocity contrasts across the Moho, perhaps reflecting mafic underplating during continental rifting. A west-dipping feature in the lithospheric mantle is further constrained to have a slab-like geometry, representing a relict slab subducted during an Appalachian orogenic event. Localized low seismic velocities in the upper mantle beneath the eastern portion of the array may indicate that the Northern Appalachian Anomaly extends relatively far to the south.publishedVersio

Response of the mantle to flat slab evolution: Insights from local S splitting beneath Peru

The dynamics of flat subduction, particularly the interaction between a flat slab and the overriding plate, are poorly understood. Here we study the (seismically) anisotropic properties and deformational regime of the mantle directly above the Peruvian flat slab. We analyze shear wave splitting from 370 local S events at 49 stations across southern Peru. We find that the mantle above the flat slab appears to be anisotropic, with modest average delay times (~0.28 s) that are consistent with ~4% anisotropy in a ~30 km thick mantle layer. The most likely mechanism is the lattice-preferred orientation of olivine, which suggests that the observed splitting pattern preserves information about the mantle deformation. We observe a pronounced change in anisotropy along strike, with predominately trench-parallel fast directions in the north and more variable orientations in the south, which we attribute to the ongoing migration of the Nazca Ridge through the flat slab system

Response of the mantle to flat slab evolution: Insights from local splitting beneath Peru

The dynamics of flat subduction, particularly the interaction between a flat slab and the overriding plate, are poorly understood. Here we study the (seismically) anisotropic properties and deformational regime of the mantle directly above the Peruvian flat slab. We analyze shear wave splitting from 370 local S events at 49 stations across southern Peru. We find that the mantle above the flat slab appears to be anisotropic, with modest average delay times (~0.28?s) that are consistent with ~4% anisotropy in a ~30?km thick mantle layer. The most likely mechanism is the lattice-preferred orientation of olivine, which suggests that the observed splitting pattern preserves information about the mantle deformation. We observe a pronounced change in anisotropy along strike, with predominately trench-parallel fast directions in the north and more variable orientations in the south, which we attribute to the ongoing migration of the Nazca Ridge through the flat slab system

Doctors' and nurses' views and experience of transferring patients from critical care home to die: a qualitative exploratory study.

BACKGROUND: Dying patients would prefer to die at home, and therefore a goal of end-of-life care is to offer choice regarding where patients die. However, whether it is feasible to offer this option to patients within critical care units and whether teams are willing to consider this option has gained limited exploration internationally. AIM: To examine current experiences of, practices in and views towards transferring patients in critical care settings home to die. DESIGN: Exploratory two-stage qualitative study SETTING/PARTICIPANTS: Six focus groups were held with doctors and nurses from four intensive care units across two large hospital sites in England, general practitioners and community nurses from one community service in the south of England and members of a Patient and Public Forum. A further 15 nurses and 6 consultants from critical care units across the United Kingdom participated in follow-on telephone interviews. FINDINGS: The practice of transferring critically ill patients home to die is a rare event in the United Kingdom, despite the positive view of health care professionals. Challenges to service provision include patient care needs, uncertain time to death and the view that transfer to community services is a complex, highly time-dependent undertaking. CONCLUSION: There are evidenced individual and policy drivers promoting high-quality care for all adults approaching the end of life encompassing preferred place of death. While there is evidence of this choice being honoured and delivered for some of the critical care population, it remains debatable whether this will become a conventional practice in end of life in this setting