The Sottunga-Jurmo shear zone : structure and deformation history of a crustal-scale ductile shear zone in SW Finland

The aim of this study is to gain a better understanding of the structure and the deformation history of a NW-SE trending regional, crustal-scale shear structure in the Åland archipelago, SW Finland, called the Sottunga-Jurmo shear zone (SJSZ). Approaches involving e.g. structural geology, geochronology, geochemistry and metamorphic petrology were utilised in order to reconstruct the overall deformation history of the study area. The study therefore describes several features of the shear zone including structures, kinematics and lithologies within the study area, the ages of the different deformation phases (ductile to brittle) within the shear zone, as well as some geothermobarometric results. The results indicate that the SJSZ outlines a major crustal discontinuity between the extensively migmatized rocks NE of the shear zone and the unmigmatised, amphibolite facies rocks SW of the zone. The main SJSZ shows overall dextral lateral kinematics with a SW-side up vertical component and deformation partitioning into pure shear and simple shear dominated deformation styles that was intensified toward later stages of the deformation history. The deformation partitioning resulted in complex folding and refolding against the SW margin of the SJSZ, including conical and sheath folds, and in a formation of several minor strike-slip shear zones both parallel and conjugate to the main SJSZ in order to accommodate the regional transpressive stresses. Different deformation phases within the study area were dated by SIMS (zircon U-Pb), ID-TIMS (titanite U-Pb) and 40Ar/39Ar (pseudotachylyte wholerock) methods. The first deformation phase within the ca. 1.88 Ga rocks of the study area is dated at ca. 1.85 Ga, and the shear zone was reactivated twice within the ductile regime (at ca. 1.83 Ga and 1.79 Ga), during which the strain was successively increasingly partitioned into the main SJSZ and the minor shear zones. The age determinations suggest that the orogenic processes within the study area did not occur in a temporal continuum; instead, the metamorphic zircon rims and titanites show distinct, 10-20 Ma long breaks in deformation between phases of active deformation. The results of this study further imply slow cooling of the rocks through 600-700ºC so that at 1.79 Ga, 2 the temperature was still at least 600ºC. The highest recorded metamorphic pressures are 6.4-7.1 kbar. At the late stages or soon after the last ductile phase (ca. 1.79 Ga), relatively high-T mylonites and ultramylonites were formed, witnessing extreme deformation partitioning and high strain rates. After the rocks reached lower amphibolite facies to amphibolite-greenschist facies transitional conditions (ca. 500-550ºC), they cooled rapidly, probably due to crustal uplift and exhumation. The shear zone was reactivated at least once within the semi-brittle to brittle regime between ca. 1.79 Ga and 1.58 Ga, as evidenced by cataclasites and pseudotachylytes. In summary, the results of this study suggest that the Sottunga-Jurmo shear zone (and the South Finland shear zone) defines a major crustal discontinuity, and played a central role in accommodating the regional stresses during and after the Svecofennian orogeny.

High-Speed Solid-Rotor Induction Machine – Electromagnetic Calculation and Design

Within the latest decade high-speed motor technology has been increasingly commonly applied within the range of medium and large power. More particularly, applications like such involved with gas movement and compression seem to be the most important area in which high-speed machines are used. In manufacturing the induction motor rotor core of one single piece of steel it is possible to achieve an extremely rigid rotor construction for the high-speed motor. In a mechanical sense, the solid rotor may be the best possible rotor construction. Unfortunately, the electromagnetic properties of a solid rotor are poorer than the properties of the traditional laminated rotor of an induction motor. This thesis analyses methods for improving the electromagnetic properties of a solid-rotor induction machine. The slip of the solid rotor is reduced notably if the solid rotor is axially slitted. The slitting patterns of the solid rotor are examined. It is shown how the slitting parameters affect the produced torque. Methods for decreasing the harmonic eddy currents on the surface of the rotor are also examined. The motivation for this is to improve the efficiency of the motor to reach the efficiency standard of a laminated rotor induction motor. To carry out these research tasks the finite element analysis is used. An analytical calculation of solid rotors based on the multi-layer transfer-matrix method is developed especially for the calculation of axially slitted solid rotors equipped with wellconducting end rings. The calculation results are verified by using the finite element analysis and laboratory measurements. The prototype motors of 250 – 300 kW and 140 Hz were tested to verify the results. Utilization factor data are given for several other prototypes the largest of which delivers 1000 kW at 12000 min-1.

Tunkeuman hallinta MIG/MAG-hitsauksessa

MIG/MAG-hitsaukselle tyypillinen ominaispiirre, valokaaren itsesäätyvyys, saavutetaan vakiojännitelähdettä käyttämällä. Valokaaren sisäisen säätömekanismin ansiosta kaarenpituus pysyy vakiona, vaikka hitsauspolttimen ja työkappaleen välinen etäisyys vaihtelisi hitsauksen aikana. Vakiojännitelähteen käyttäminen aiheuttaa kuitenkin kaaritehon vaihtelua vapaalankapituuden muuttuessa. Vapaalangan kasvaessa liian pitkäksi kaariteho laskee niin alas, ettei se enää riitä sulattamaan tarpeeksi perusainetta railon kyljissä. Tämän seurauksena hitsausliitokseen syntyy erilaisia liittymävirheitä. Käsinhitsauksessa vapaalangan pituus saattaa polttimen epävakaasta kuljetuksesta johtuen vaihdella erityisesti kokemattomilla hitsaajilla. Mekanisoidussa ja automatisoidussa hitsauksessa railojen mitta- ja muotopoikkeamat aiheuttavat vapaalankapituuden vaihtelua. Poikkeamia syntyy kaikissa hitsausrailojen esivalmistusvaiheissa. Lisäksi lämmöntuonnin aiheuttamat muodonmuutokset kappaleissa lisäävät poikkeamia railonsovituksessa hitsauksen aikana. Ongelma on useimmiten ratkaistavissa railonseurantaa käyttämällä. Railonseurantajärjestelmät ovat kuitenkin kalliita, eivätkä ne toimi luotettavasti kaikissa olosuhteissa. Diplomityössä tutkittiin uutta MIG/MAG-hitsauksen reaaliaikaiseen tunkeuman hallintaan kehitettyä säätöjärjestelmää. Työn tavoitteina olivat säätöjärjestelmän luotettavan toiminnan takaavien reunaehtojen ja kosketussuutinetäisyyden suositusrajojen määrittäminen. Tavoitteiden täyttämiseksi työn kokeellisessa osiossa suoritettiin laaja hitsauskokeiden sarja, jossa hitsattavina materiaaleina käytettiin seostamatonta ja runsasseosteista terästä.

Dans le labyrinthe de la pensée. Approches croisées du Qu'est-ce que la philosophie de Gilles Deleuze et Félix Guattari

Ce cahier regroupe une série d'études portant, principalement, sur le Qu'est-ce que la philosophie? de G. Deleuze et F. Guattari. Il réunit des contributions de chercheurs confirmés - A. Sauvagnargues, A. Villani - et de jeunes chercheurs de l'Université de Lausanne sous la direction et la supervision de Hugues Poltier, membre de la section de philosophie de l'université.

L'immanence - ou l'opinion à la question. Autour de Qu'est-ce que la philosophie?

Nous nous attachons, dans une lecture centrée sur Qu'est-ce que la philosophie? de Deleuze et Guattari, à cerner la compréhension des auteurs du propre de la philosophie. Nous montrons la centralité de la nécessité de se distinguer d'avec l'opinion dans l'élaboration du concept de concept et l'importance du plan d'immanence en tant qu'il n'est pas un concept mais le tracé, toujours se faisant, des rapports de composition entre les concepts.

Tectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain)

Two small, alluvial-lacustrine subbasins developed during the early restraining overstep stages of the Oligocene-Miocene As Pontes strike-slip Basin (NW Spain). Later, the basin evolved into a restraining bend stage and an alluvial-swamp-dominated depositional framework developed. The palaeobiological record demonstrates that the Oligocene-Miocene palaeoclimate in NW Spain was subtropical, warm and humid to subhumid.

An active zone characterized by slow normal faults, the northwestern margin of the València trough (NE Iberia): a review

The northwestern margin of the Valencia trough is an area of low strain characterized by slow normal faults and low to moderate seismicity. Since the mid 1990s this area has been the subject of a number of studies on active tectonic which have proposed different approaches to the location of active faults and to the calculation of the parameters that describe their seismic cycle. Fifty-six active faults have been found and a classification has been made in accordance with their characteristics: a) faults with clear evidence of large paleo-, historic or instrumental earthquakes (2/56); b) faults with evidence of accumulated activity during the Plio-Quaternary and with associated instrumental seismicity (7/56); c) faults with evidence of accumulated activity during the Plio-Quaternary and without associated instrumental seismicity (17/56); d) faults with associated instrumental seismicity and without evidence of accumulated activity during the Plio-Quaternary (30/56), and e) faults without evidence of activity or inactive faults. The parameters that describe the seismic cycle of these faults have been evaluated by different methods that use the geological data obtained for each fault except when paleoseismological studies were available. This classification can be applied to other areas with low slip faults because of the simplicity of the approaches adopted. This study reviews the different approaches proposed and describes the active faults located, highlighting the need a) to better understand active faults in slow strain zones through paleoseismological studies, and b) to include them in seismic hazard studies.

Managing the crises : how did local governments react to the financial crisis in 2008 and what explains the differences ? The case of Swiss municipalities

Swiss municipalities are, to a large extent, responsible for their financial resources. Since these resources primarily depend on income and property taxes from individuals and enterprises, municipality budgets are likely to be directly affected by the current crisis in the financial sector and the economy. This article investigates how municipalities perceived this threat and how they reacted to it. In a nationwide survey conducted at the end of 2009 in all 2596 Swiss municipalities, we asked local secretaries which measures had been launched in order to cope with expected losses in tax income and a possible increase in welfare spending. Did the municipalities rely on Keynesian measures increasing public spending and accepting greater deficits, or did they try to avoid further deficits by using austerity measures and a withdrawal of planned investments? Our results show that only a few municipalities - mainly the bigger ones - expected to be greatly affected by the crisis. Their reactions, however, did not reveal any clear patterns that theory would lead one to expect. Preferences for austerity measures and deficit spending become visible but many municipalities took measures from both theories. The strongest explanatory factors for determining how/why municipalities react are: the municipality's level of affectedness followed by whether or not the municipality belongs to the French-speaking part of the country. Size also has an impact, whereas the strength of the Social Democrat party is negligible. Explaining what kind of measures municipalities are likely to take is more difficult. However, the more a municipality is affected, the more likely it is to stick to austerity measures.

A Social Network Analysis of Twitter: Mapping the Digital Humanities Community

Defining digital humanities might be an endless debate if we stick to the discussion about the boundaries of this concept as an academic "discipline". In an attempt to concretely identify this field and its actors, this paper shows that it is possible to analyse them through Twitter, a social media widely used by this "community of practice". Based on a network analysis of 2,500 users identified as members of this movement, the visualisation of the "who's following who?" graph allows us to highlight the structure of the network's relationships, and identify users whose position is particular. Specifically, we show that linguistic groups are key factors to explain clustering within a network whose characteristics look similar to a small world.

Evidence for coseismic events of recurrent prehistoric deformation along the Alhama de Murcia fault, southeastern Spain

The Alhama de Murcia fault is a 85 km long oblique-slip fault, and is related to historical and instrumental seismic activity. A paleoseismic analysis of the Lorca-Totana sector of the fault containing MSK I=VIII historical earthquakes was made in order to identify and quantify its seismic potential. We present 1) the results of the neotectonic, structural and geomorphological analyses and, 2) the results of trenching. In the study area, the Alhama de Murcia fault forms a depressed corridor between two strands, the northwestern fault with morphological and structural features of a reverse component of slip, bounding the La Tercia range to the South, and the southeastern fault strand with evidence of sinistral oblique strike-slip movement. The offset along this latter fault trapped the sediments in transit from the La Tercia range towards the Guadalentín depression. The most recent of these sediments are arranged in three generations of alluvial fans and terraces. The first two trenches were dug in the most recent sediments across the southeastern fault strand. The results indicate a coseismic reverse fault deformation that involved the sedimentary sequence up to the intermediate alluvial fan and the Holocene terrace deposits. The sedimentary evolution observed in the trenches suggests an event of temporary damming of the Colmenar creek drainage to the South due to uplifting of the hanging wall during coseismic activation of the fault. Trench, structural and sedimentological features provide evidence of at least three coseismic events, which occurred after 125,000 yr. The minimum vertical slip rate along the fault is 0.06 mm/yr and the average recurrence period should not exceed 40,000 yr in accordance with the results obtained by fan topographic profiling. Further absolute dating is ongoing to constrain these estimates.

American Indians of the Southwest

Recorded in Indian communities by Willard Rhodes, with the cooperation of the United States Office of Indian Affairs.

Phase behavior and rheological analysis of reverse liquid crystals and W/I2, W/H2 gel emulsions using an amphiphilic block copolymer.

This article reports the phase behavior determi- nation of a system forming reverse liquid crystals and the formation of novel disperse systems in the two-phase region. The studied system is formed by water, cyclohexane, and Pluronic L-121, an amphiphilic block copolymer considered of special interest due to its aggregation and structural proper- ties. This system forms reverse cubic (I2) and reverse hexagonal (H2) phases at high polymer concentrations. These reverse phases are of particular interest since in the two-phase region, stable high internal phase reverse emulsions can be formed. The characterization of the I2 and H2 phases and of the derived gel emulsions was performed with small-angle X-ray scattering (SAXS) and rheometry, and the influence of temperature and water content was studied. TheH2 phase experimented a thermal transition to an I2 phase when temperature was increased, which presented an Fd3m structure. All samples showed a strong shear thinning behavior from low shear rates. The elasticmodulus (G0) in the I2 phase was around 1 order of magnitude higher than in theH2 phase. G0 was predominantly higher than the viscousmodulus (G00). In the gel emulsions,G0 was nearly frequency-independent, indicating their gel type nature. Contrarily to water-in-oil (W/O) normal emulsions, in W/I2 and W/H2 gel emulsions, G0, the complex viscosity (|η*|), and the yield stress (τ0) decreased with increasing water content, since the highly viscous microstructure of the con- tinuous phase was responsible for the high viscosity and elastic behavior of the emulsions, instead of the volumefraction of dispersed phase and droplet size. A rheological analysis, in which the cooperative flow theory, the soft glass rheology model, and the slip plane model were analyzed and compared, was performed to obtain one single model that could describe the non-Maxwellian behavior of both reverse phases and highly concentrated emulsions and to characterize their microstructure with the rheological properties.

Periodontal Diseases in Tanzania

Tutkimuksen tavoitteena oli kuvata hampaiden kiinnityskudossairauksien esiintyvyyttä ja suuhygieniatottumuksia Tansaniassa. Viiden eri tutkimuksen avulla kartoitettiin suuhygieniatottumuksia, kiinnityskudosten tilaa, kiinnityskudossairauksien riskitekijöitä ja hoidon tarvetta (CPITN) sekä ienvetäymiä. Tutkimukset toteutettiin eri paikkakunnilla vuosien 1987 ja 2003 välillä. Tutkittavat valittiin satunnaisesti tai harkitusti; tutkittavien määrä vaihteli 201:stä 1764:ään. Aineistot kerättiin kysymyslomakkeilla ja kliinisten tutkimusten avulla. Kliinisesti mitattiin plakin, hammaskiven ja ienten verenvuodon määrä, ientaskujen syvyys, ienvetäymien laajuus ja puuttuvien hampaiden lukumäärä. Tutkimusvälineinä käytettiin peiliä, Williamsin ja WHO:n ientaskumittareita. Muoviharjaksista hammasharjaa ilmoitti käyttävänsä 51,5-97,8% tutkituista. Ns. harjaustikun käyttö vaihteli paljon: 0,9-32,0 %. Plakkia löydettiin 65-100 %:lla tutkituista. Hammaskiveä oli suurimmalla osalla tutkituista. Myös ienverenvuotoa löytyi valtaosalta (79-100%). Ienverenvuotoa oli enemmän miehillä kuin naisilla sekä alhaisemman koulutustason omaavilla. Neljäkymmentä vuotta täyttäneiltä löydettiin 4–5 mm:n syvyisiä ientaskuja 82,1 %:lta ja ≥ 6 mm:n taskuja 43,8 %:lta. Suun terveystottumusten ohjaamiseen oli tarvetta yli 90 %:lla, hammaskiven poistoon ja juurten pinnan tasoitukseen yli 80%:lla. Yleisimmät riskitekijät kiinnityskudossairauksille olivat ikä (≥ 35 vuotta), miessukupuoli, alhainen koulutustaso, plakin, hammaskiven ja ientulehduksen määrä sekä asuminen maaseudulla. Ienvetäymiä (≥ 4 mm) löytyi noin 54%:lla tutkituista. Ienvetäymiä oli useammin miehillä kuin naisilla ja ne olivat yhteydessä ikään sekä hammaskiven ja ienverenvuodon esiintymiseen. Suuhygieniataso tutkituilla henkilöillä oli huono ja ienvetäymien esiintyvyys korkea. Syviä ientaskuja löytyi kuitenkin harvoilta tutkituilta. Riskitekijät kiinnityskudossairauksille olivat ikä, miessukupuoli, alhainen koulutustaso, plakin, hammaskiven ja ientulehduksen määrä sekä asuminen maaseudulla. Ienvetäymien riskit olivat ikä, miessukupuoli, hammaskivi ja ienverenvuoto

Chaotic dynamics of electric-field domains in periodically driven superlattices

Self-sustained time-dependent current oscillations under dc voltage bias have been observed in recent experiments on n-doped semiconductor superlattices with sequential resonant tunneling. The current oscillations are caused by the motion and recycling of the domain wall separating low- and high-electric-field regions of the superlattice, as the analysis of a discrete drift model shows and experimental evidence supports. Numerical simulation shows that different nonlinear dynamical regimes of the domain wall appear when an external microwave signal is superimposed on the dc bias and its driving frequency and driving amplitude vary. On the frequency-amplitude parameter plane, there are regions of entrainment and quasiperiodicity forming Arnold tongues. Chaos is demonstrated to appear at the boundaries of the tongues and in the regions where they overlap. Coexistence of up to four electric-field domains randomly nucleated in space is detected under ac+dc driving.

Dynamic patterns of flow in the workplace: characterizing within-individual variability using a complexity science approach

As a result of the growing interest in studying employee well-being as a complex process that portrays high levels of within-individual variability and evolves over time, this present study considers the experience of flow in the workplace from a nonlinear dynamical systems approach. Our goal is to offer new ways to move the study of employee well-being beyond linear approaches. With nonlinear dynamical systems theory as the backdrop, we conducted a longitudinal study using the experience sampling method and qualitative semi-structured interviews for data collection; 6981 registers of data were collected from a sample of 60 employees. The obtained time series were analyzed using various techniques derived from the nonlinear dynamical systems theory (i.e., recurrence analysis and surrogate data) and multiple correspondence analyses. The results revealed the following: 1) flow in the workplace presents a high degree of within-individual variability; this variability is characterized as chaotic for most of the cases (75%); 2) high levels of flow are associated with chaos; and 3) different dimensions of the flow experience (e.g., merging of action and awareness) as well as individual (e.g., age) and job characteristics (e.g., job tenure) are associated with the emergence of different dynamic patterns (chaotic, linear and random).