New insights into Crustal Contributions to Large-volume Rhyolite Generation in the Mid-Tertiary Sierra Madre Occidental Province, Mexico, revealed by U Pb Geochronology

Voluminous (≥3·9 × 105 km3), prolonged (∼18 Myr) explosive silicic volcanism makes the mid-Tertiary Sierra Madre Occidental province of Mexico one of the largest intact silicic volcanic provinces known. Previous models have proposed an assimilation–fractional crystallization origin for the rhyolites involving closed-system fractional crystallization from crustally contaminated andesitic parental magmas, with <20% crustal contributions. The lack of isotopic variation among the lower crustal xenoliths inferred to represent the crustal contaminants and coeval Sierra Madre Occidental rhyolite and basaltic andesite to andesite volcanic rocks has constrained interpretations for larger crustal contributions. Here, we use zircon age populations as probes to assess crustal involvement in Sierra Madre Occidental silicic magmatism. Laser ablation-inductively coupled plasma-mass spectrometry analyses of zircons from rhyolitic ignimbrites from the northeastern and southwestern sectors of the province yield U–Pb ages that show significant age discrepancies of 1–4 Myr compared with previously determined K/Ar and 40Ar/39Ar ages from the same ignimbrites; the age differences are greater than the errors attributable to analytical uncertainty. Zircon xenocrysts with new overgrowths in the Late Eocene to earliest Oligocene rhyolite ignimbrites from the northeastern sector provide direct evidence for some involvement of Proterozoic crustal materials, and, potentially more importantly, the derivation of zircon from Mesozoic and Eocene age, isotopically primitive, subduction-related igneous basement. The youngest rhyolitic ignimbrites from the southwestern sector show even stronger evidence for inheritance in the age spectra, but lack old inherited zircon (i.e. Eocene or older). Instead, these Early Miocene ignimbrites are dominated by antecrystic zircons, representing >33 to ∼100% of the dated population; most antecrysts range in age between ∼20 and 32 Ma. A sub-population of the antecrystic zircons is chemically distinct in terms of their high U (>1000 ppm to 1·3 wt %) and heavy REE contents; these are not present in the Oligocene ignimbrites in the northeastern sector of the Sierra Madre Occidental. The combination of antecryst zircon U–Pb ages and chemistry suggests that much of the zircon in the youngest rhyolites was derived by remelting of partially molten to solidified igneous rocks formed during preceding phases of Sierra Madre Occidental volcanism. Strong Zr undersaturation, and estimations for very rapid dissolution rates of entrained zircons, preclude coeval mafic magmas being parental to the rhyolite magmas by a process of lower crustal assimilation followed by closed-system crystal fractionation as interpreted in previous studies of the Sierra Madre Occidental rhyolites. Mafic magmas were more probably important in providing a long-lived heat and material flux into the crust, resulting in the remelting and recycling of older crust and newly formed igneous materials related to Sierra Madre Occidental magmatism.

Late Oligocene to middle Miocene rifting and syn-extensional magmatism in the southwestern Sierra Madre occidental, Mexico: the beginning of the Gulf of California rift

Although Basin and Range style extension affected several areas of western Mexico since the Late Eocene, extension in the Gulf of California region (the Gulf Extensional Province GEP) is thought to have started as subduction waned and ended at ~14 12.5 Ma. A general consensus also exists in considering the mid Miocene Comondú group as a suprasubduction volcanic arc. Our new integration of the geology of the south east Gulf region, backed by 43 new Ar Ar and U Pb mineral ages and geochemical studies, document a widespread phase of extension in the southern GEP between latest Oligocene and Early Miocene that subsequently focused in the region of the future Gulf in the Middle Miocene. Upper Oligocene to Lower Miocene rocks across the southern Sierra Madre Occidental (SMO)(northern Nayarit and southern Sinaloa) were affected by major ~N S to NNW striking normal faults prior to ~21 Ma. Then, between ~21 and 11 Ma, a system of NNW-SSE high angle extensional faults continued extending the southwestern side of the SMO. Rhyolitic domes, shallow intrusive bodies, and lesser basalts were emplaced along this extensional belt at 20-17 Ma. In northern Sinaloa, large grabens were floored by huge dome complexes at ~21-17 Ma and filled by continental sediments with interlayered basalts dated at 15-14 Ma, a setting and timing very similar to Sonora. Early to Middle Miocene volcanism, including the largely volcaniclastic Comondú strata in Baja California Sur, was thus emplaced in rift basins and was likely associated to decompression melting of upper mantle (inducing crustal partial melting) rather than to fluxing by fluids from the young subducting plate. Along the Nayarit and Sinaloa coast, flatlying basaltic lava flows dated at 11-10 Ma are exposed just above the present sea level. Here, crustal thickness is almost half that in the unextended core of the SMO, implying significant lithosphere stretching before ~11 Ma. Our study shows that rifting began much earlier than Late Miocene and provided a fundamental control on the style and composition of volcanism from at least 30 Ma. We envision a sustained period of lithospheric stretching and magmatism during which the pace and breadth of extension changed at ~20-18 Ma to be narrower and likely more rapid, and again at ~12.5 Ma, when the kinematics of rifting became more oblique.

Consequences of extensional tectonics on volcanic eruption style, compositions and source regions : new insights from the southern Sierra Madre Occidental and Gulf of California regions, western Mexico

Understanding the link between tectonic-driven extensional faulting and volcanism is crucial from a hazard perspective in active volcanic environments, while ancient volcanic successions provide records on how volcanic eruption styles, compositions, magnitudes and frequencies can change in response to extension timing, distribution and intensity. This study draws on intimate relationships of volcanism and extension preserved in the Sierra Madre Occidental (SMO) and Gulf of California (GoC) regions of western Mexico. Here, a major Oligocene rhyolitic ignimbrite “flare-up” (>300,000 km3) switched to a dominantly bimodal and mixed effusive-explosive volcanic phase in the Early Miocene (~100,000 km3), associated with distributed extension and opening of numerous grabens. Rhyolitic dome fields were emplaced along graben edges and at intersections of cross-graben and graben-parallel structures during early stages of graben development. Concomitant with this change in rhyolite eruption style was a change in crustal source as revealed by zircon chronochemistry with rapid rates of rhyolite magma generation due to remelting of mid- to upper crustal, highly differentiated igneous rocks emplaced during earlier SMO magmatism. Extension became more focused ~18 Ma resulting in volcanic activity being localised along the site of GoC opening. This localised volcanism (known as the Comondú “arc”) was dominantly effusive and andesite-dacite in composition. This compositional change resulted from increased mixing of basaltic and rhyolitic magmas rather than fluid flux melting of the mantle wedge above the subducting Guadalupe Plate. A poor understanding of space-time relationships of volcanism and extension has thus led to incorrect past tectonic interpretations of Comondú-age volcanism.

Late Oligocene to Middle Miocene rifting and synextensional magmatism in the southwestern Sierra Madre Occidental, Mexico : the beginning of the Gulf of California rift

Although Basin and Range–style extension affected large areas of western Mexico after the Late Eocene, most consider that extension in the Gulf of California region began as subduction waned and ended ca. 14–12.5 Ma. A general consensus also exists in considering Early and Middle Miocene volcanism of the Sierra Madre Occidental and Comondú Group as subduction related, whereas volcanism after ca. 12.5 Ma is extension related. Here we present a new regional geologic study of the eastern Gulf of California margin in the states of Nayarit and Sinaloa, Mexico, backed by 43 new Ar-Ar and U-Pb mineral ages, and geochemical data that document an earlier widespread phase of extension. This extension across the southern and central Gulf Extensional Province began between Late Oligocene and Early Miocene time, but was focused in the region of the future Gulf of California in the Middle Miocene. Late Oligocene to Early Miocene rocks across northern Nayarit and southern Sinaloa were affected by major approximately north-south– to north-northwest– striking normal faults prior to ca. 21 Ma. Between ca. 21 and 11 Ma, a system of north-northwest–south-southeast high angle extensional faults continued extending the southwestern side of the Sierra Madre Occidental. Rhyolitic domes, shallow intrusive bodies, and lesser basalts were emplaced along this extensional belt at 20–17 Ma. Rhyolitic rocks, in particular the domes and lavas, often show strong antecrystic inheritance but only a few Mesozoic or older xenocrysts, suggesting silicic magma generation in the mid-upper crust triggered by an extension induced basaltic infl ux. In northern Sinaloa, large grabens were occupied by huge volcanic dome complexes ca. 21–17 Ma and filled by continental sediments with interlayered basalts dated as 15–14 Ma, a stratigraphy and timing very similar to those found in central Sonora (northeastern Gulf of California margin). Early to Middle Miocene volcanism occurred thus in rift basins, and was likely associated with decompression melting of upper mantle (inducing crustal partial melting) rather than with fluxing by fluids from the young and slow subducting microplates. Along the eastern side of the Gulf of California coast, from Farallón de San Ignacio island offshore Los Mochis, Sinaloa, to San Blas, Nayarit, a strike distance of >700 km, flat lying basaltic lavas dated as ca. 11.5–10 Ma are exposed just above the present sea level. Here crustal thickness is almost half that in the unextended core of the adjacent Sierra Madre Occidental, implying signifi cant lithosphere stretching before ca. 11 Ma. This mafic pulse, with subdued Nb-Ta negative spikes, may be related to the detachment of the lower part of the subducted slab, allowing an upward asthenospheric flow into an upper mantle previously modified by fluid fluxes related to past subduction. Widespread eruption of very uniform oceanic island basalt–like lavas occurred by the late Pliocene and Pleistocene, only 20 m.y. after the onset of rifting and ~9 m.y. after the end of subduction, implying that preexisting subduction-modified mantle had now become isolated from melt source regions. Our study shows that rifting across the southern-central Gulf Extensional Province began much earlier than the Late Miocene and provided a fundamental control on the style and composition of volcanism from at least 30 Ma. We envision a sustained period of lithospheric stretching and magmatism during which the pace and breadth of extension changed ca. 20–18 Ma to be narrower, and again after ca. 12.5 Ma, when the kinematics of rifting became more oblique.

Aspectos antropológicos de las terapias con células madre

Resumen: Las células madre tienen dos características naturales únicas, que son su capacidad de división celular indefinida, y de regeneración y reparación de tejidos. Esto genera un gran interés en las áreas de investigación y tratamiento de enfermedades que aún no tienen cura y son motivadoras de una importante fuente de esperanza para los pacientes. Surge, entonces, el dilema ético de definir cuáles serán los recursos para obtenerlas, procesarlas y determinar la seguridad y eficacia de su uso en la aplicación clínica. Un enfoque personalista ontológico considerará la protección de todos los participantes en los procesos de investigación: los donantes de células, los participantes de la investigación y los pacientes que serán beneficiarios de estos tratamientos, de manera de proteger a todos los involucrados sin exponer a riesgos a unos para salvar a otros.

¿Libertad de elección de la madre o derecho a la vida del niño por nacer? : una disyuntiva que no es tal

Introducción: El aborto es un tema que genera diferentes opiniones en nuestro país y en todo el mundo. Es una problemática que no se reduce a lo jurídico, sino que implica connotaciones políticas, sociales, culturales, económicas y religiosas1. En el presente artículo nos proponemos aclarar la aparente disyuntiva que se presenta entre el derecho a la vida del niño por nacer y los derechos de la madre, como su libertad de elección, su privacidad y su salud, circunscribiendo el análisis al derecho argentino, aunque se hará especial referencia al precedente norteamericano, Roe v. Wade. En este sentido, en un primer momento haremos mención de la protección legislativa y jurisprudencial de cada uno de los derechos mencionados, para luego tratar de dar respuesta a la disyuntiva propuesta en el título del presente artículo: ¿existe el derecho a abortar? ¿Puede ser restringida la vida en el comienzo de su desarrollo? ¿Qué ocurre en caso de riesgo en la salud de la madre?

Algunos significados originarios y enseñanzas actuales : hermeneútica de la historia de las apariciones de Nuestra Madre de Guadalupe

Deseamos colaborar a una mejor profundización y aprovechamiento de los tesoros del acontecimiento guadalupano, auténtica posibilidad y modelo para nuestro presente. Al especificar, titular y jerarquizar algunos aspectos de una interpretación inicial sobre el mismo, partiendo de lo anterior, y conversando con su contenido desde nuestros intereses de hoy, completamos esta propuesta hermenéutica. Concretamos, en suma, un recorrido que proporciona criterios para apropiarse de la relevante, vigente y siempre actual dinámica de diálogo, que revela la historia de las apariciones de la Virgen Morena. Busca incentivar, de esta manera, a redescubrir y recrear sagazmente dicha dinámica, con todas sus importantes consecuencias, y con la pedagogía que la subyace y hace posible; para movernos a decisiones prudenciales que, al comenzar el tercer milenio, en cada cultura y situación, nos lleven a vivir más lúcidamente nuestra identidad, acontecer y servicio como Pueblo de Dios. Deseamos favorecer la llegada a existenciales conclusiones que nos guíen, en el contexto de un mundo con muchos y cercanos diferentes unos al lado del otro, hacia la construcción de un mundo auténticamente plural, viviendo una evangelización inculturante e inculturada.

Explicação do salmo cincoenta feita a rogo da madre Dona Isabel de Sancto Antonio, ou de Lima, pello P. Fr. Pedro de S. Francisco frade menor da Provincia de Portugal : Dico ego opera mea

Pedro de S. Francisco nasceu em Marzagào, na África, em data desconhecida, e morreu em 1638. O religioso franciscano foi mestre em Teologia e Provincial da sua Ordem. Segundo Inocêncio, na ‘Explicação do salmo cincoenta’, o autor analisa e comenta extensamente cada um dos versos do salmo Miserere mei Dei e afirma, ainda, que "são raros os exemplares deste livro, em que (corno diz o censor Jorge Cabral, que o reviu por ordem do Santo Ofício) resplandece a erudição, doutrina, piedade e sabedoria do autor". O impressor da obra, Pedro Craesbeeck, nasceu em Antuérpia, onde aprendeu a arte da impressão na famosa Oficina de Cristóvão Plantino. Mudou-se para Portugal por volta de 1592, onde fundou uma verdadeira dinastia de impressores célebres que ali trabalharam nos séculos XV e XVI. Responsável pela impressão de obras de grande beleza tipográfica. Pedro Craesbeeck tornou-se impressor régio, conforme consta em alvará de 28 de maio de r620. Seus trabalhos foram editados no período de 1597 a 1632.

Memorias para a historia da capitania de S. Vicente, hoje chamada de S. Paulo, do Estado do Brazil / publicada de ordem da Academia R. das Sciencias por Fr. Gaspar da Madre de Deos

Segundo Richard R. Ramer, "Primeira edição. O autor, natural de Santos, SP, escreveu esta obra depois de ter feito um estudo cuidadoso em documentos contemporâneos...".

Influencia de las células madre mesenquimales en la recuperación de oligodendrocitos sometidos a estrés oxidativo

179 p.

Interacciones entre las células madre pluripotentes del carcinoma embrionario y las células mioides peritubulares del testículo

112 p.+ anexos

Evaluación de la aplicación del Método Madre Canguro en la madre y en el neonato

Resumen: El Método de la Madre Canguro (MMC) es un sistema de cuidado neonatal que consiste en el contacto piel con piel de la madre y su hijo de forma precoz, continuada y mantenida en el tiempo. Objetivo: Describir los efectos del uso del Método de la Madre Canguro en la madre y en el neonato. Metodología: Se ha realizado una búsqueda bibliográfica en diferentes bases de datos para recopilar revisiones sistemáticas, ensayos clínicos y estudios cualitativos acerca del MMC. La búsqueda se realizó entre Noviembre de 2014 y Febrero de 2015. Finalmente fueron seleccionados 17 artículos para la realización de este trabajo. Conclusión: Parece probado que la práctica del Método de la Madre Canguro resulta beneficiosa tanto para la madre como para el neonato. Es necesario avanzar más en la protocolización del método y en la investigación científica de sus efectos, para poder aumentar su fiabilidad y convertirlo en un método más eficaz y seguro.

Community Vulnerability to Malaria in Madre de Dios, Peru

Construction of a highway and artisanal gold mining have contributed to population and land use changes within the department of Madre de Dios, Peru. Such changes are expected to alter malaria rates due to impacts on vector habitat and human exposure. Vulnerability, as defined by the possibility of bereavement of a physical good or abstract state, is useful for understanding which communities are most likely to be adversely impacted by hazards such as malaria. A model defining susceptibility (SUS) and lack of resilience (LOR) was used to create an index of vulnerability to malaria for 40 communities in Madre de Dios. Indicators of SUS and LOR were developed from household and community data and combined into a final vulnerability index score. Vulnerability scores ranged between 0.13 and 0.31 with a mean of 0.21. Communities were grouped according to standard deviations from the mean. The most vulnerable communities (>1.5 standard deviations from mean) were located in the southern portion of the study area. When the dimension scores were compared for all communities, scores were generally higher in the susceptibility dimension than in the lack of resilience dimension. Examination of the indicator scores of individual communities revealed that drivers of vulnerability vary across the department. Therefore, targeted interventions addressing specific aspects of vulnerability may be useful. Finally, a predicted vulnerability surface was created for a 10 km buffer surrounding the Interoceanic Highway in Madre de Dios.

Air pollution, Fuel Usage and Health Outcomes in Madre de Dios, Peru: a Comparative Cross Sectional Study

Air pollution is a common problem. Particulate matter generated from air pollution has been tied to adverse health outcomes associated with cardiovascular disease. Biomass fuels are a specific contributor to increased particulate matter and arise as a result of indoor heating, cook stoves and indoor food preparation. This is a two part cross sectional study looking at communities in the Madre de Dios region. Survey data was collected from 9 communities along the Madre de Dios River. Individual level household PM2.5 was also collected as a means to generate average PM data stratified by fuel use. Data collection was affected by a number of outside factors, which resulted in a loss of data. Results from the cross-sectional study indicate that hypertension is not a significant source of morbidity. Obesity is prevalent and significantly associated with kitchen venting method indicating a potential relationship.

Napoli dal Casino della Regina Madre : [vue générale de la baie de Naples] : [peinture]

Collectionneur : Lesouëf, Auguste (1829-1906)