Seismic structure along transitions from flat to normal subduction: central Mexico, southern Peru, and southwest Japan

The fine-scale seismic structure of the central Mexico, southern Peru, and southwest Japan subduction zones is studied using intraslab earthquakes recorded by temporary and permanent regional seismic arrays. The morphology of the transition from flat to normal subduction is explored in central Mexico and southern Peru, while in southwest Japan the spatial coincidence of a thin ultra-slow velocity layer (USL) atop the flat slab with locations of slow slip events (SSEs) is explored. This USL is also observed in central Mexico and southern Peru, where its lateral extent is used as one constraint on the nature of the flat-to-normal transitions.

In western central Mexico, I find an edge to this USL which is coincident with the western boundary of the projected Orozco Fracture Zone (OFZ) region. Forward modeling of the 2D structure of the subducted Cocos plate using a finite-difference algorithm provides constraints on the velocity and geometry of the slab’s seismic structure in this region and confirms the location of the USL edge. I propose that the Cocos slab is currently fragmenting into a North Cocos plate and a South Cocos plate along the projection of the OFZ, by a process analogous to that which occurred when the Rivera plate separated from the proto-Cocos plate 10 Ma.

In eastern central Mexico, observations of a sharp transition in slab dip near the abrupt end of the Trans Mexican Volcanic Belt (TMVB) suggest a possible slab tear located within the subducted South Cocos plate. The eastern lateral extent of the USL is found to be coincident with these features and with the western boundary of a zone of decreased seismicity, indicating a change in structure which I interpret as evidence of a possible tear. Analysis of intraslab seismicity patterns and focal mechanism orientations and faulting types provides further support for a possible tear in the South Cocos slab. This potential tear, together with the tear along the projection of the OFZ to the northwest, indicates a slab rollback mechanism in which separate slab segments move independently, allowing for mantle flow between the segments.

In southern Peru, observations of a gradual increase in slab dip coupled with a lack of any gaps or vertical offsets in the intraslab seismicity suggest a smooth contortion of the slab. Concentrations of focal mechanisms at orientations which are indicative of slab bending are also observed along the change in slab geometry. The lateral extent of the USL atop the horizontal Nazca slab is found to be coincident with the margin of the projected linear continuation of the subducting Nazca Ridge, implying a causal relationship, but not a slab tear. Waveform modeling of the 2D structure in southern Peru provides constraints on the velocity and geometry of the slab’s seismic structure and confirms the absence of any tears in the slab.

In southwest Japan, I estimate the location of a possible USL along the Philippine Sea slab surface and find this region of low velocity to be coincident with locations of SSEs that have occurred in this region. I interpret the source of the possible USL in this region as fluids dehydrated from the subducting plate, forming a high pore-fluid pressure layer, which would be expected to decrease the coupling on the plate interface and promote SSEs.

Investigations of group IVA transition metal mediated carbon-carbon bond forming reactions

Zirconocene aldehyde and ketone complexes were synthesized in high yield by treatment of zirconocene acyl complexes with trimethylaluminum or diisobutylaluminum hydride. These complexes, which are activated by dialkylaluminum chloride ligands, inserted unsaturated substrates such as alkynes, allenes, ethylene, nitriles, ketenes, aldehydes, ketones, lactones, and acid chlorides with moderate to high conversion. Insertion of aldehyde substrates yielded zirconocene diolate complexes with up to 20:1 (anti:syn) diastereoselectivity. The zirconocene diolates were hydrolyzed to afford unsymmetrical 1,2-diols in 40-80% isolated yield. Unsymmetrical ketones gave similar insertion yields with little or no diastereoselectivity. A high yielding one-pot method was developed that coupled carbonyl substrates with zirconocene aldehyde complexes that were derived from olefins by hydrozirconation and carbonylation. The zirconocene aldehyde complexes also inserted carbon monoxide and gave acyloins in 50% yield after hydrolysis.

The insertion reaction of aryl epoxides with the trimethylphoshine adduct of titanocene methylidene was examined. The resulting oxytitanacyclopentanes were carbonylated and oxidatively cleaved with dioxygen to afford y-lactones in moderate yields. Due to the instability and difficult isolation of titanocene methylidene trimethylphoshine adducts, a one-pot method involving the addition of catalytic amounts of trimethylphosphine to β,β-dimethyltitanacyclobutane was developed. A series of disubstituted aryl epoxides were examined which gave mixtures of diastereomeric insertion products. Based on these results, as well as earlier Hammett studies and labeling experiments, a biradical transition state intermediate is proposed. The method is limited to aryl substituted epoxide substrates with aliphatic examples showing no insertion reactivity.

The third study involved the use of magnesium chloride supported titanium catalysts for the Lewis acid catalyzed silyl group transfer condensation of enol silanes with aldehydes. The reaction resulted in silylated aldol products with as many as 140 catalytic turnovers before catalyst inactivation. Low diastereoselectivities favoring the anti-isomer were consistent with an open transition state involving a titanium atom bound to the catalyst surface. The catalysts were also used for the aldol group transfer polymerization of t-butyldimethylsilyloxy-1-ethene resulting in polymers with molecular weights of 5000-31,000 and molar mass dispersities of 1.5-2.8. Attempts to polymerize methylmethacrylate using GTP proved unsuccessful with these catalysts.

Collective dynamics of glass-forming polymers at intermediate length scales: a synergetic combination of neutron scattering, atomistic simulations and theoretical modelling

Qens/wins 2014 - 11th International Conference on Quasielastic Neutron Scattering and 6th International Workshop on Inelastic Neutron Spectrometers / editado por:Frick, B; Koza, MM; Boehm, M; Mutka, H

Desenvolvimento do sistema reprodutivo de Echinostoma paraensei (Trematoda: Digenea) de hamsters (Mesocricetus auratus) experimentalmente infectados, analisado por microscopia de luz de campo e microscopia laser confocal

O conhecimento da morfologia e ultraestrutura dos helmintos permite a correta classificação destes organismos, bem como fornece subsídios que poderão ser utilizados para diagnóstico e controle. A microscopia laser confocal é uma ferramenta para estudar a organização estrutural de várias espécies de helmintos, possibilitando acesso a detalhes morfológicos não evidenciados pela microscopia óptica. Echinostoma paraensei é um trematódeo, digenético, hermafrodita parasito de numerosos hospedeiros vertebrados. Neste trabalho foi investigado o desenvolvimento dos órgãos reprodutivo e a morfometria de E. paraensei, desde a fase jovem até a adulta, como contribuição ao conhecimento do desenvolvimento reprodutivo desta espécie. Os trematódeos foram recuperados aos 3, 4, 5, 6, 7, 10, 14 e 21 dias posterior à infecção (dpi) experimental em hamsters. Estes foram corados em carmim clorídrico, desidratados em série alcoólica e montados em lâmina permanente em bálsamo do Canadá, fotografados e medidos usando microscopia de luz de campo claro (MCC) e microscopia de varredura laser confocal (MVLC). Entre 3 e 4 dpi, os primórdios genitais estavam presentes e nenhuma organização do sistema reprodutivo foi visualizada por MCC e MVLC. Os primórdio do ovário, dos testículos e da bolsa do cirro foram visualizados por MCC aos 5 e 6 dpi, no entanto, MVLC dos helmintos aos 5dpi mostra que estes primórdios, o ootipo e o útero estavam presentes, como estruturas individualizadas. A bolsa do cirro apresenta metratermo e o ovário com primórdio do oótipo adjacente aos 7dpi por MVLC. A vesícula seminal, receptáculo seminal, células diferenciadas nos testículos, ducto e reservatório vitelínico e oviducto foram visualizados após 10 dias, enquanto os espermatozóides na vesícula seminal, ovos e oócitos, células vitelínicas, poro e canal de Laurer aos 14 dias. A morfometria evidencia um acelerado crescimento dos órgãos reprodutores a partir do 7 dia. Os testículos apresentam aumento significativo no comprimento do 7 ao 21 dia e o ovário durante o período de 7 à 10 dpi. Aos 21 dpi, todos os helmintos apresentaram glândulas vitelínicas, útero contendo ovos e espermatozóides no oviducto enquanto outros ovos estão sendo formados. As mudanças morfológicas acentuadas durante a gametogênese consistem no aumento do comprimento do helminto, maturação das gônadas, desenvolvimento e maturação das glândulas vitelínicas. O desenvolvimento do helminto como um todo está relacionado à maturação dos órgãos reprodutivo masculino e feminino indicando o investimento deste trematódeo em garantir a produção e eliminação dos ovos ao meio exterior.