pinecone/core-2020-05-10-deduplication huggingface dataset:
The Glarus thrust : excursion guide and report of a field trip of the Swiss Tectonic Studies Group (Swiss Geological Society, 14.16. 09. 2006)

This excursion guide results form a field trip to the Glarus nappe complex organized by the Swiss Tectonic Studies Group in 2006. The aim of the excursion was to discuss old and recent concepts related to the evolution of the Glarus thrust. The major aspects were (i) the interplay between deformation, fluid flow and geochemical alteration, (ii) episodic versus continuous deformation and fluid flow, and (iii) the link between large-scale structures, microstructures, and geochemical aspects. Despite 150 years of research in the Glarus nappe complex and the new results discussed during the excursion, there exist controversies that still are unsolved
A map-view restoration of the Alpine-Carpathian-Dinaridic system for early miocene

A map-view palinspastic restoration of tectonic units in the Alps, Carpathians and Dinarides reveals the plate tectonic configuration before the onset of Miocene to recent deformations. Estimates of shortening and extension from the entire orogenic system allow for a semi-quantitative restoration of translations and rotations of tectonic units during the last 20 Ma. Our restoration yielded the following results: (1) The Balaton Fault and its eastern extension along the northern margin of the Mid-Hungarian Fault Zone align with the Periadriatic Fault, a geometry that allows for the eastward lateral extrusion of the Alpine-Carpathian-Pannonian (ALCAPA) Mega-Unit. The Mid-Hungarian Fault Zone accommodated simultaneous strike-perpendicular shortening and strike-slip movements, concomitant with strike-parallel extension. (2) The Mid-Hungarian Fault Zone is also the locus of a former plate boundary transforming opposed subduction polarities between Alps (including Western Carpathians) and Dinarides. (3) The ALCAPA Mega-Unit was affected by 290 km extension and fits into an area W of present-day Budapest in its restored position, while the Tisza-Dacia Mega-Unit was affected by up to 180 km extension during its emplacement into the Carpathian embayment. (4) The external Dinarides experienced Neogene shortening of over 200 km in the south, contemporaneous with dextral wrench movements in the internal Dinarides and the easterly adjacent Carpatho-Balkan orogen. (5) NS convergence between the European and Adriatic plates amounts to some 200 km at a longitude of 14° E, in line with post-20 Ma subduction of Adriatic lithosphere underneath the Eastern Alps, corroborating the discussion of results based on high-resolution teleseismic tomography. The displacement of the Adriatic Plate indenter led to a change in subduction polarity along a transect through the easternmost Alps and to substantial Neogene shortening in the eastern Southern Alps and external Dinarides. While we confirm that slab-pull and rollback of oceanic lithosphere subducted beneath the Carpathians triggered back-arc extension in the Pannonian Basin and much of the concomitant folding and thrusting in the Carpathians, we propose that the rotational displacement of this indenter provided a second important driving force for the severe Neogene modifications of the Alpine-Carpathian-Dinaridic orogenic system
From subduction to collision : thermal overprint of HP/LT meta-sediments in the north-eastern Leopontine Dome (Swiss Alps) and consequences regarding the tectono-metamorphic evolution of the Alpine orogenic wedge

The Cenozoic-age metamorphic structure of the Alps consists of a throughgoing pressure-dominated belt (blueschists and eclogites) that strikes parallel to the orogen and was later truncated by two thermal domes characterised by Barrow-type metamorphism (Lepontine dome and Tauern window). This study documents for the first time that relics of Fe-Mg carpholite occur also within meta-sedimentary units that are part of the north-eastern Lepontine structural and metamorphic dome, where so far exclusively Barrovian assemblages were found. They occur in meta-sediments of both Valais Oceanderived Lower Penninic Bündnerschiefer and structurally lower Europe-derived Sub-Penninic cover nappes and slices. These high-pressure units were subsequently overprinted by a thermal event, as is documented by the growth of new minerals typical for Barrovian metamorphism. We present evidence for a two-stage metamorphic evolution in the northern part of the Lepontine dome: (1) Early subduction-related syn-D1 (Safienphase) HP/LT metamorphism under blueschist facies conditions (350–400 °C and 1.2–1.4 GPa) was immediately followed by “cold” isothermal (or cooling) decompression during D2 nappe-stacking (Ferrera phase). (2) Collisionrelated Barrovian overprint (500–570 °C and 0.5–0.8 GPa) postdates the D3 nappe-refolding event (Domleschg phase) and represents a late heating pulse, separated by D2 and D3 from the D1 high-pressure event. It occurred before and/or during the initial stages of D4 (Chièra phase) representing a second nappe-refolding event. In discussing possible heat sources for the late Barrow-type heating pulse it is argued that heat release from radioactive decay of accreted material may play an important role in contributing much to heat production. Based on the field evidence, we conclude that heat transfer was essentially conductive during these latest stages of the thermal evolution
Seismic source characterization of the Alpine foreland in the context of a probabilistic seismic hazard analysis by PEGSOS Expert Group 1 (EG1a)

Seismic source characterization is performed as part of the PEGASOS project for the assessment of the seismic hazard at the 4 sites of the Swiss Nuclear Power Plants. The analysis is performed according to the Level 4 procedures for expert elicitation defined in the guidelines of the US Nuclear Regulatory Committee whereby the quantification of uncertainties plays a crucial role. According to our analysis, which is one amongst four that were performed in the frame of PEGASOS, the most important epistemic uncertainty is related to the question as to weather basement-rooted faults at the margins of pre-existing Permo-Carboniferous troughs are prone for compressive or transpressive reactivation under the present-day stress field or not. The question after the present-day style of deformation in the Alpine foreland (thick-skinned versus thin-skinned) is closely related to this key question. Together with the consideration of uncertainties regarding the mapping of seismogenic zones and/or line sources alternative zonations are presented in form of a logic tree with 21 branches. Area sources play a predominant role in the working area located at the margin of a diffuse plate boundary. Earthquake recurrence relationships are discussed by taking into account a series of uncertainties. These concern the evaluation of b-values and the evaluation of a-values once the b-values were fixed. Both parameters in the Gutenberg-Richter law are based on non-perfect and incomplete catalogue data that were carefully analysed beforehand. Since PEGASOS demanded an analysis of annual probabilities down to one event in 107 years, the question after the value of the maximum possible earthquake magnitude Mmax and related error in Mmax estimates plays a crucial role. We estimate Mmax by using geological as well as statistical methods. Mmax = 6.9 cannot be excluded in most areas, in the Basel area Mmax = 7.3 is possible. Uncertainties in a, b and Mmax are again discussed in form of a logic tree, this time with 18 branches. Hence the final logic tree has 378 branches and represents the seismic source characterization input into PSHA that takes account of all uncertainties we are aware of. Betr. u.a. Erdbebengefährdung in der Region Base
Preparing a seismic hazard model for Switzerland : the view from PEGASOS expert group 3 (EG1c)

The seismic hazard model used in the PEGASOS project for assessing earth-quake hazard at four NPP sites was a composite of four sub-models, each produced by a team of three experts. In this paper, one of these models is described in detail by the authors. A criticism sometimes levelled at probabilistic seismic hazard studies is that the process by which seismic source zones are arrived at is obscure, subjective and inconsistent. Here, we attempt to recount the stages by which the model evolved, and the decisions made along the way. In particular, a macro-to-micro approach was used, in which three main stages can be described. The first was the characterisation of the overall kinematic model, the “big picture” of regional seismogenesis. Secondly, this was refined to a more detailed seismotectonic model. Lastly, this was used as the basis of individual sources, for which parameters can be assessed. Some basic questions had also to be answered about aspects of the approach to modelling to be used: for instance, is spatial smoothing an appropriate tool to apply? Should individual fault sources be modelled in an intraplate environment? Also, the extent to which alternative modelling decisions should be expressed in a logic tree structure has to be considered. \u
Formal proposal for the Bathonian GSSP (Middle Jurassic) in the\ud
Ravin du Bès Section (Bas-Auran, SE France)

The Bathonian Global Stratotype Section and Point (GSSP) is proposed at\ud
the base of limestone bed RB071 (bed 23 in Sturani 1967) in the Ravin du\ud
Bès Section (43º 57' 38" N, 6º 18' 55" E), Bas-Auran area, “Alpes de Haute\ud
Provence” French department. The Ravin du Bès Section, as formal candidate\ud
GSSP for the base of the Bathonian Stage, satisfies most of the requirements\ud
recommended by the International Commission on Stratigraphy: 1) The exposure\ud
extends over 13 m in thickness. At the Bajocian-Bathonian transition,\ud
no vertical (bio-, ichno- or tapho-) facies changes, condensation, stratigraphic\ud
gaps or hiatuses have been recorded. Structural complexity, synsedimentary\ud
and tectonic disturbances, or important alterations by metamorphism are not\ud
relevant constraints. 2) There is a well-preserved, abundant and diverse fossil\ud
record across the boundary interval, with key markers (ammonites and\ud
nannofossils) for worldwide correlation. The base of the Bathonian Stage\ud
and Zigzag Zone in Bas-Auran corresponds to the first occurrence level of\ud
Gonolkites convergens Buckman, which coincides with the first occurrence of\ud
Morphoceras parvum Wetzel. Calcareous nannofossils, as secondary global\ud
marker, are present in all beds and allow characterizing the Bajocian-Bathonian\ud
transition. 3) Regional analyses of sequence stratigraphy and manganese\ud
chemostratigraphy are available. Spectral gamma-ray data corroborate an\ud
Early Bathonian deepening half-cycle of second order. 4) The criteria of accessibility,\ud
conservation and protection are assured by the “Réserve Naturelle\ud
Géologique de Haute Provence”. The Cabo Mondego Section (Portugal) is\ud
suggested as the Bathonian auxiliary section and point (ASSP) within this\ud
GSSP proposal
Microtextural investigation (SEM and TEM study) of phyllosilicates in a major thrust fault zone (Monte Perdido, southern Pyrenees): impact on fault reactivation

Thrusting fault zone in foreland basins are characterized by highly foliated zones generally enriched in phyllosilicates which can play a major role on the mechanical behaviour of the fault. In this context, investigations of synkinematic clay minerals permit to determine the origin of the fluid from which they precipitated as well as the mechanisms of deformation. Our study is focused on clay mineral assemblages (illite and chlorite) in a major thrust fault located in the Monte Perdido massif (southern Pyrenees), a shallow thrust that affects upper cretaceouspaleocene platform carbonates and lower Eocene marls and turbidites
Platform-basin transitions and their role in Alpine-style collision systems : a comparative approach

CB acknowledges financial support from Optimus (Aberdeen) ltd. Petroceltic International plc are thanked for providing access to the subsurface data used in this study and for permission to publish images used here. Schlumberger are thanked for providing use of Petrel software under their academic agreement with the University of Aberdeen. RWHB thanks the organisers of the 12th Emile Argand Conference on Alpine Geological Studies for the invitation and financial support to participate in the Montgenevre workshop. Reviewers Enrico Tavarnelli, Thierry Dumont and editors Christian Sue and Stefan Schmid are all thanked for their comments that have significantly improved this contribution.Peer reviewedPublisher PD
Structural and geochronological constraints from the Drina-Ivanjica thrust sheet (Western Serbia): implications for the Cretaceous–Paleogene tectonics of the Internal Dinarides

We have investigated successive episodes of ocean-continent and continent–continent convergence in Western Serbia\ud
(Drina-Ivanjica thrust sheet). The coupled application of structural and petrological analyses with Illite Crystallinity measurements and K/Ar dating has revealed the timing and structural characteristics of multiple regional deformation phases, and allowed us to revise the origin of the different Triassic units outcropping in the study area. D1 tectonic burial was characterized by anchizonal metamorphism, dominantly WNW-verging isoclinal folding (F1), and related axial planar cleavage (S1) formation in the Paleozoic basement and the stratigraphic cover of the Drina-Ivanjica thrust sheet exposed along the northern rim of this thrust sheet. The timing of D1 deformation is constrained by K/Ar ages suggesting 135–150 Ma tectonic burial for the Drina-Ivanjica thrust sheet. D1 deformation and metamorphism is correlated with the closure of the Vardar ocean by top-W to NW ophiolite obduction and the underthrusting of the Adriatic distal passive margin below the oceanic upper plate. Since D1 structures are lacking in the southern occurrences of Triassic rocks within the study area it is proposed that this Triassic is may not be the original sedimentary cover of the Drina-Ivanjica Paleozoic\ud
basement. We propose that this southern Triassic originated from a more external Dinaridic thrust sheet and was transported to its present-day position by a top-NE backthrust presumably during late Early Cretaceous–Paleogene times. Mapscale, NW–SE striking D2 thrust faults and abundant NW–SE trending F2 folds observed in all units correspond to the general trend of the Dinaridic orogen and are attributed to the latest Cretaceous–Paleogene collision between Adria and Europe. Regional Latest Cretaceous–Paleogene shortening was followed by strike-slip tectonics (N–S shortening and perpendicular extension) and subsequent Miocene normal faulting in both orogen-parallel and orogen-perpendicular directions driven by slab rollback processes of the Carpathian-Dinaridic realm
Julian Schwinger: Nuclear Physics, the Radiation Laboratory,
  Renormalized QED, Source Theory, and Beyond

Julian Schwinger's influence on twentieth century science is profound and
pervasive. Of course, he is most famous for his renormalization theory of
quantum electrodynamics, for which he shared the Nobel Prize with Richard
Feynman and Sin-itiro Tomonaga. But although this triumph was undoubtedly his
most heroic work, his legacy lives on chiefly through subtle and elegant work
in classical electrodynamics, quantum variational principles, proper-time
methods, quantum anomalies, dynamical mass generation, partial symmetry, and
more. Starting as just a boy, he rapidly became the pre-eminent nuclear
physicist in the late 1930s, led the theoretical development of radar
technology at MIT during World War II, and then, soon after the war, conquered
quantum electrodynamics, and became the leading quantum field theorist for two
decades, before taking a more iconoclastic route during his last quarter
century.Comment: 54 pages, no figure
Boltzmann and the art of flying

One of the less known facets of Ludwig Boltzmann was that of an advocate of
Aviation, one of the most challenging technological problems of his times.
Boltzmann followed closely the studies of pioneers like Otto Lilienthal in
Berlin, and during a lecture on a prestigious conference he vehemently defended
further investments in the area. In this article I discuss his involvement with
Aviation, his role in its development and his correspondence with two flight
pioneers, Otto Lilienthal e Wilhelm Kress.Comment: 15 pages, no figure
Physical Science in Barcelona

We provide a tour of Barcelona, Catalonia, Spain, following four routes through the city and one elsewhere in the city and beyond, focusing on sites of importance in physics. Route 1 covers the Old Town, its Gothic Quarter, Plaça del Rei, Plaça de Sant Jaume, and Jewish Quarter. Route 2 identifies sites on and close to La Rambla, the main promenade in the city. Route 3 goes from the medieval shipyards to the Board of Commerce to Citadel Park. Route 4 concentrates on the Extension (Eixample) and covers the restored University, the Industrial University, and the new campus of the University of Barcelona. Elsewhere in the city and beyond are the Fabra Observatory; the Plaça de les Glòries with its large steel sculpture depicting the meridian arc from Dunkirk to Barcelona; Montjuïc, the site of the National Art Museum of Catalonia; and the National Museum of Science and Technology in Terrassa
History of "Anomalous" Atmospheric Neutrino Events: A First Person
  Account

The modern picture of the neutrino as a multiple mass highly mixed neutral
particle has emerged over 40 years of study. Best known of the issues leading
to this picture was the apparent loss of neutrinos coming from the sun. This
article describes another piece of evidence that supports the picture; the
substantial reduction of high energy muon type neutrinos observed in nature.
For much of the 40 year period, before the modern picture emerged this
observation was known as the "atmospheric neutrino anomaly", since as will be
seen, these neutrinos originate in the Earth's atmosphere.
  This paper describes the discovery of the atmospheric neutrino anomaly. We
explore the scientific context and motivations in the late 1970's from which
this work emerged. The gradual awareness that the observations of atmospheric
neutrinos were not as expected took place in the 1983-1986 period.Comment: 46 pages, 24 figures. To be published in Physics in Perspective
  Version 2 has a table of contents, a table of figures and the DOI added The
  final publication is available at Springer via
  http://dx.doi.org/10.1007/s00016-016-0185-
The Early Scientific Contributions of J. Robert Oppenheimer: Why Did the
  Scientific Community Miss the Black Hole Opportunity?

We aim to carry out an assessment of the scientific value of Oppenheimer's
research on black holes in order to determine and weigh possible factors to
explain its neglect by the scientific community, and even by Oppenheimer
himself. Dealing primarily with the science and looking closely at the
scientific culture and the scientific conceptual belief system of the 1930s,
the present article seeks to supplement the existent literature on the subject
by enriching the explanations and possibly complicating the guiding questions.
We suggest a rereading of Oppenheimer as a more intriguing, ahead-of-his-time
figure.Comment: 19 pages, Phys. Perspect. (2017
Signalling in viral entry.

Viral infections are serious battles between pathogens and hosts. They can result in cell death, elimination of the virus or latent infection keeping both cells and pathogens alive. The outcome of an infection is often determined by cell signalling. Viruses deliver genomes and proteins with signalling potential into target cells and thereby alter the metabolism of the host. Virus interactions with cell surface receptors can elicit two types of signals, conformational changes of viral particles, and intracellular signals triggering specific cellular reactions. Responses by cells include stimulation of innate and adaptive immunity, growth, proliferation, survival and apoptosis. In addition, virus-activated cell signalling boosts viral entry and gene delivery, as recently shon for adenoviruses and adeno-associated viruses. This review illustrates that multiple activation of host cells during viral entry profoundly impacts the elaborate relationship between hosts and viral pathogens
Neuromuscular synaptogenesis: clustering of acetylcholine receptors revisited.

Clustering of neurotransmitter receptors in the postsynaptic membrane is critical for efficient synaptic transmission. During neuromuscular synaptogenesis, clustering of acetylcholine receptors (AChRs) is an early sign of postsynaptic differentiation. Recent studies have revealed that the earliest AChR clusters can form in the muscle independent of motorneurons. Neurally released agrin, acting through the muscle-specific kinase MuSK and rapsyn, then causes further clustering and localization of clusters underneath the nerve terminal. AChRs themselves are required for agrin-induced clustering of several postsynaptic proteins, most notably rapsyn. Once formed, AChR clusters are stabilized by several tyrosine kinases and by components of the dystrophin/utrophin glycoprotein complex, some of which also direct postnatal synaptic maturation such as formation of postjunctional folds. This review summarizes these recent results about AChR clustering, which indicate that early clustering can occur in the absence of nerves, that AChRs play an active role in the clustering process and that partly different mechanisms direct formation versus stabilization of AChR clusters
Vernix caseosa as a multi-component defence system based on polypeptides, lipids and their interactions

To access publisher full text version of this article. Please click on the hyperlink in Additional Links fieldVernix caseosa is a white cream-like substance that covers the skin of the foetus and the newborn baby. Recently, we discovered antimicrobial peptides/proteins such as LL-37 in vernix, suggesting host defence functions of vernix. In a proteomic approach, we have continued to characterize proteins in vernix and have identified 20 proteins, plus additional variant forms. The novel proteins identified, considered to be involved in host defence, are cystatin A, UGRP-1, and calgranulin A, B and C. These proteins add protective functions to vernix such as antifungal activity, opsonizing capacity, protease inhibition and parasite inactivation. The composition of the lipids in vernix has also been characterized and among these compounds the free fatty acids were found to exhibit antimicrobial activity. Interestingly, the vernix lipids enhance the antimicrobial activity of LL-37 in vitro, indicating interactions between lipids and antimicrobial peptides in vernix. In conclusion, vernix is a balanced cream of compounds involved in host defence, protecting the foetus and newborn against infection
DNA methylation of fly genes and transposons

The use of anti-5-methylcytosine antibodies in affinity columns allowed the identification of methylated sequences in the genome of Drosophila melanogaster adults. In view of the presence of transposable elements amongst the identified sequences, it has been suggested that DNA methylation is involved in transposon control in the fly genome. On the contrary, a re-analysis of these data can furnish several intriguing elements that could open new questions about the role that DNA methylation plays in the fly genome. The aim of the present paper is to discuss some features that emerge from the analysis of the identified methylated sequences