54 research outputs found

    Emplacement of the Foy, Hess and Pele Offset Dykes at the Sudbury impact structure, Canada

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    The 1.85 Ga Sudbury impact structure is the remnant of what is generally considered to have been an ~150–200 km diameter impact basin in central Ontario, Canada. The so-called Offset Dykes are impact melt dykes that are found concentrically around – and extending radially outward from – the Sudbury Igneous Complex (SIC), a ~3 km thick differentiated impact melt sheet. The dykes are typically composed of two main phases of granodiorite: an inclusion- and sulfide-rich granodiorite in the centre of the dyke, and an inclusion- and sulfide-poor granodiorite along the margins of the dyke. This study uses a combination of field mapping, petrography, electron microprobe analyses and geochemical data to address two outstanding questions regarding the temporal relationships of the Offset Dykes: (1) When were the Offset Dykes emplaced relative to the impact cratering process and differentiation of the SIC and; (2) What is the relationship between the internal phases of the Offset Dykes (i.e., inclusion-rich and inclusion-poor granodiorite). New exposures of the Foy and Hess Offset dykes, along with the recent discovery of the Pele Offset Dyke, provide an excellent opportunity to understand the relationship between the Offset Dykes in the North Range of the SIC. From this research, a number of conclusions can be drawn: (1) The Foy and Hess were intruded after the SIC had undergone some degree of differentiation; (2) The Hess is slightly less evolved than the Foy with respect to the SIC, but the two dykes co-existed as melts and mixed at the intersection; (3) The Foy was likely emplaced during a single prolonged event, which carried the clasts and sulfides, and subsequent flow differentiation moved the clasts and sulfides towards the centre of the dyke, forming the inclusion-poor and inclusion-rich phases and; (4) The Pele is composed of only the inclusion-poor phase, is chemically more evolved than the other North Range Offset Dykes, and may have been one of the last Offset Dykes to have been emplaced. These results suggest that emplacement of the Offset Dykes took place over an extended period of time and not as a single early injection event

    Monitoring the excited state dynamics of thymine by time-resolved IR spectroscopy

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    Die Parabel vom klugen / betrĂŒgerischen Verwalter Lk 16,1-8a(8b-13)

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    Der Text Lk 16,1-8a(8b-13) wird zunĂ€chst synchron gelesen und anhand des exegetischen Methodenkanons erschlossen. Dabei fließen schrittweise diachrone Fragestellungen ein. Das frĂŒhe Ringen um das VerstĂ€ndnis des Textes kommt in den Blick sowie die darin sich widerspiegelnden Probleme und Auseinandersetzungen der urchristlichen Gemeinde. Zentrale Fragen in diesem Zusammenhang sind: Wer ist der kyrios in Vers 8a, und wo ist das Ende der ursprĂŒnglichen Parabel anzusetzen? Die Positionen verschiedener Forscher zu diesen Fragestellungen werden diskutiert und mit eigenen InterpretationsansĂ€tzen ergĂ€nzt. Das Lob des Herrn fĂŒr den „Verwalter der Ungerechtigkeit“ in Vers 8a ist eine Provokation, die sich nicht auflösen lĂ€sst, unabhĂ€ngig davon, welcher Interpretation man folgt. Der aufmerksame Leser / die aufmerksame Leserin wird im Zuge der ParabellektĂŒre „herausgerufen“ (vgl. provocare), vor allem aber herausgefordert, die eigenen Deutungsmuster kritisch zu hinterfragen. Obwohl die Verwalterparabel zum SLk gehört, steht sie doch nicht isoliert im Text des NT, sondern weist BezĂŒge und Querverbindungen innerhalb des NT auf. Einige dieser Querverbindungen (semantisch, motivlich) werden diskutiert und dargestellt. Dabei werden unterschiedliche Beziehungsmuster zwischen Vorgesetzten und Untergebenen im NT analysiert sowie RĂŒckschlĂŒsse in Bezug auf die Verwalterparabel thematisiert. Die Anregung von J. Ernst, hinter to alethinĂłn (Vers 11) eine mögliche Anspielung auf das „Wort der Wahrheit“ in der Briefliteratur (2 Tim 2,15; Jak 1,18) zu sehen, wird aufgegriffen und analysiert. Die erwĂ€hnten Stellen werden durch weitere, im Zuge der Recherchen entdeckte, ergĂ€nzt. Eine ZusammenfĂŒhrung unterschiedlicher bibeltheologischer Aussagen in den jeweiligen Zeitkontexten soll im Sinne einer zeitgenössischen Hermeneutik verstanden werden. Es geht um die Frage: Wie zeitliche Fragestellungen auf die Leseweise und Interpretation des Textes einwirken? Die unterschiedlichen Positionen, vor allem neuere ZugĂ€nge zu diesem durchaus sperrigen Text, werden dargestellt. Abschließend wird der Versuch unternommen, einige FĂ€den des exegetischen Polylogs zusammenzufĂŒhren

    Triplet‐Induced Lesion Formation at CpT and TpC Sites in DNA

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    UV irradiation induces DNA lesions particularly at dipyrimidine sites. Using time‐resolved UV pump (250 nm) and mid‐IR probe spectroscopy the triplet pathway of cyclobutane pyrimidine dimer (CPD) formation within TpC and CpT sequences was studied. The triplet state is initially localized at the thymine base but decays with 30 ns under formation of a biradical state extending over both bases of the dipyrimidine. Subsequently this state either decays back to the electronic ground state on the 100 ns time scale or forms a cyclobutane pyrimidine dimer lesion (CPD). Stationary IR spectroscopy and triplet sensitization via 2â€Č‐methoxyacetophenone (2‐M) in the UVA range shows that the lesions are formed with an efficiency of approximately 1.5 %. Deamination converts the cytosine moiety of the CPD lesions on the time scale of 10 hours into uracil which gives CPD(UpT) and CPD(TpU) lesions in which the coding potential of the initial cytosine base is vanished

    Identification of charge separated states in thymine single strands

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    UV excitation of the DNA single strand (dT)(18) leads to electronically excited states that are potential gateways to DNA photolesions. Using time-resolved infrared spectroscopy we characterized a species with a lifetime of similar to 100 ps and identified it as a charge separated excited state between two thymine bases

    Identification of charge separated states in thymine single strands

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    UV excitation of the DNA single strand (dT)(18) leads to electronically excited states that are potential gateways to DNA photolesions. Using time-resolved infrared spectroscopy we characterized a species with a lifetime of similar to 100 ps and identified it as a charge separated excited state between two thymine bases

    Field and laboratory validation of remote rover operations Science Team findings: The CanMars Mars Sample Return analogue mission

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    The CanMars Mars Sample Return Analogue Deployment (MSRAD) was a closely simulated, end-to-end Mars Sample Return (MSR) mission scenario, with instrumentation, goals, and constraints modeled on the upcoming NASA Mars 2020 rover mission; this paper reports on the post-mission validation of the exercise. The exercise utilized the CSA Mars Exploration Science Rover (MESR) rover, deployed to Utah, USA, at a Mars-analogue field site. The principal features of the field site located near Green River, Utah are Late Jurassic inverted, fluvial paleochannels, analogous to features on Mars in sites being considered for the ESA ExoMars rover mission and present within the chosen landing site for the Mars 2020 rover mission. The in-simulation (“in-sim”) mission operations team worked remotely from The University of Western Ontario, Canada. A suite of MESR-integrated and hand-held spectrometers was selected to mimic those of the Mars 2020 payload, and a Utah-based, on-site team was tasked with field operations to carry out the data collection and sampling as commanded by the in-sim team. As a validation of the in-sim mission science findings, the field team performed an independent geological assessment. This paper documents the field team's on-site geological assessment and subsequent laboratory and analytical results, then offers a comparison of mission (in-sim) and post-mission (laboratory) science results. The laboratory-based findings were largely consistent with the in-sim rover-derived data and geological interpretations, though some notable exceptions highlight the inherent difficulties in remote science. In some cases, available data was insufficient for lithologic identification given the absence of other important contextual information (e.g., textural information). This study suggests that the in-sim instruments were largely adequate for the Science Team to characterize samples; however, rover-based field work is necessarily hampered by mobility and time constraints with an obvious effect on efficiency but also precision, and to some extent, accuracy of the findings. The data show a dearth of preserved total organic carbon (TOC) – used as a proxy for ancient biosignature preservation potential – in the fluvial-lacustrine system of this field site, suggesting serious consideration with respect to the capabilities and opportunities for addressing the Mars exploration goals. We therefore suggest a thorough characterization of terrestrial sites analogous to those of Mars rover landing sites, and in-depth field studies like CanMars as important, pre-mission strategic exercises
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