Repetitive mixing events and holocene pyroclastic activity at Pico de Orizaba and Popocatepetl (Mexico)     

J. M. Cantagrel  A. Gourgaud  C. Robin 《Bulletin of Volcanology》1984,47(4):735-748

The Holocene volcanic activity which built up the present terminal cones of Pico de Orizaba and Popocatepetl in eastern Mexico, was characterized by repeated pyroclastic Saint-Vincent type eruptions. Radiocarbon data show that these paroxysmal events occurred at more or less regular intervals, and were followed by moderate activity producing ash and pumice falls and andesitic lava flows from the summit craters.Typical ash and scoria pyroclastic flows exhibit a heterogeneous composition given by the interaction of a dacitic component with a more basic andesitic one. Scoria bombs are characterized by banded to emulsified textures, mineralogical desequilibrium assemblages and linear chemical variations on element-element plots as exemplified by the Loma Grande flow at Pico.Periodic replenishments of the magmatic reservoir could be the major phenomenon that started mixing and consequently triggered the pyroclastic eruptions.  相似文献   

Hydrodynamic dispersion during absorption of water by soil: 2. Immobile water model     

M.J.L. Robin  K.B. Laryea  D.E. Elrick 《Journal of Hydrology》1983,65(4):333-348

The assumptions and analysis of Part 1 are extended to the three model soil-water profiles having different immobile-water contents up to 0.08 m³ m^?3. Concentration profiles in the mobile zone obtained with a constant dispersion coefficient are compared with those calculated with the same dispersion coefficient and no immobile water. The average concentration profiles were calculated from the concentration of the solution in both the mobile and immobile phases. Increasing the immobile-water content decreased and shifted the average concentration profiles further into the soil. The values of the dispersion coefficient calculated with the immobile-water fraction ignored, were found to be water content dependent and many times greater than that of the input dispersion coefficient.  相似文献   

Polar ice sheets: Developments since Wegener     

Dr. G. de Q. Robin 《International Journal of Earth Sciences》1981,70(2):648-663

Wegener's expeditions pioneered many measurements that are now essential for computer modelling of ice sheets. Advances in knowledge of accumulation, thickness, temperature, crystal fabric and surface mapping of ice sheets and of impurities, gas content and isotopic ratios of ice cores from these ice sheets are outlined before computer modelling work is discussed. The value of such studies in providing large scale tests of geophysical concepts is emphasized. The paper concludes by suggesting that the drag of continental ice sheets on the top of continental blocks might be of comparable magnitude and tend to balance forces on the base of these blocks by motion of the asthenosphere. Apart from providing a possible reason for the aseismic nature of the Antarctic and Greenland land masses, the hypothesis provides a suitable link for this volume between Wegener's interest in continental ice sheets and continental drift.

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Zusammenfassung Wegeners Expeditionen haben viele Messungen angeregt, die zu Ergebnissen geführt haben, die nunmehr reif sind für Computer-Modelle von Eisdecken. Es werden die Fortschritte in der Kenntnis von Akkumulationsraten, Mächtigkeit, Temperatur, Kristallstruktur, Oberflächenkartierung von Eisdecken und Verunreinigungen umrissen. Danach wird die Arbeit mit dem Computer-Modell diskutiert. Der Wert solcher Untersuchungen für großmaßstäbliche Tests geophysikalischer Konzepte wird betont. Die Ergebnisse lassen erwarten, daß die Schubkräfte der kontinentalen Eisdecken auf dem Top der kontinentalen Blöcke in derselben Größenordnung liegen könnten wie die aus der Bewegung der Asthenosphäre an der Basis dieser Blöcke. Letztere könnten damit kompensiert werden.Unabhängig davon, daß die aufgestellte Hypothese mögliche Argumente für die aseismische Natur der Antarktischen und Grönland-Massen aufzeigt, verbindet sie im Rahmen dieses Bandes Wegeners Interesse an kontinentalen Eisdecken mit der Kontinentaldrift.

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Résumé Les expéditions de Wegener ont suscité de nombreuses mesures qui ont fourni des données aujourd'hui mûres pour établir des modèles de couvertures glaciaires par la voie de calculatrices. Mais avant de discuter ce procédé, mention est faite des progrès accomplis dans la connaissance de l'accumulation, de l'épaisseur, de la température, de la structure cristalline et de la cartographie des couvertures glaciaires ainsi que de leurs impuretés, leur teneur en gas et les rapports d'isotopes dans les carottes qui y ont été prélevées, études dont il convient de souligner la valeur par les données à grande échelles qu'elles ont fourni à l'appui de concepts géophysiques. Le mémoire conclut sur la suggestion que les forces d'entrainement des couvertures glaciaires continentales sur la surface des blocs continentaux doit être d'un ordre comparable aux forces agissant à la base de ces blocs dans leur mouvement sur l'asthénosphère et qu'ils tendent à égaler. Outre qu'elle donne une raison possible de la nature asismique du continent antactique et du Groenland, cette hypothèse, dans ce volume, forme un trait d'union dans les intérêts que Wegener a portés aux couvertures glaciaires continentales et à la dérive des continents.

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Réponse au commentaire de Maurice Mattauer à l'article Was the Trevaresse Thrust the source of the 1909 Lambesc (Provence) earthquake? Historical and geomorphic evidence     

Robin Lacassin  Paul Tapponnier  Bertrand Meyer  Rolando Armijo 《Comptes Rendus Geoscience》2002,334(7):515-517

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Reply to comment of Drs U. Radtke and G. Schellmann on the paper by Aguirre, M.L. and Whatley, R.C. (1995). Late quaternary marginal marine deposits and palaeoenvironments from Northeastern Buenos Aires Province, Argentina: A review. Quaternary science reviews, 14, 223–254     

Marina L. Aguirre  Robin C. Whatley 《Quaternary Science Reviews》1996,15(10):1063-1064

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Phytoplankton and particulate matter in Carlingford Lough, Ireland: An assessment of food availability and the impact of bivalve culture     

Brendan Ball  Robin Raine  Dermot Douglas 《Estuaries and Coasts》1997,20(2):430-440

In an attempt to assess the impact of bivalve culture in Carlingford Lough, Ireland, the seasonal cycles of nutrients, particulate matter, chlorophylla, and phytoplankton in the lough was investigated in 1992. Chlorophyll levels showed an increase in April, corresponding to the annual spring bloom, and levels remained relatively high (2–12 mg m^?3) throughout the summer before dropping to a winter minimum by December. Throughout the summer the phytoplankton community was dominated by diatoms, with microflagellates becoming an increasingly larger fraction of the biomass in autumn and winter. Dinoflagellates were only present on occasion in low numbers during the summer months. Seasonal variations in nitrate, phosphate, and silicate concentrations at all stations showed characteristic winter maxima and summer minima. Nitrate concentrations had reached a minimum undetectable level by June, at a time when the main freshwater input from the Clanrye River had dropped to <0.3 m³ s^?1. Particulate organic carbon (POC) composed approximately 5% of the suspended matter, with highest values in winter due to resuspension. Levels of biologically available POC, as determined by a modified BOD technique, were greatest in summer, and an inverse relationship was observed between total POC and its fraction that was biologically available. Most of the labile fraction was considered to be phytoplankton, and remineralization during the summer is suggested as a mechanism for maintaining high productivity during the summer months. Although the phytoplankton biology was uncoupled with that outside the lough, it is concluded that there is scope for expansion of the local bivalve mariculture industry without altering the ecosystem of the lough. The upper limit on such expansion would be set by practical considerations such as availability of space and site suitability due to water quality.  相似文献   

An intensified C.C.D. camera for telescope guidance     

G. Herpe  M. Chevreton  J. C. Robin  P. Prat  B. Servan  F. Gex 《Experimental Astronomy》1991,2(3):163-177

This paper deals with the study and the fabrication of an intensified C.C.D. camera for guiding telescopes or for searching fields containing faint stars. It describes the sensor of the camera (by connecting the Thomson C.C.D. and the RTC image intensifier) and its three working modes. The first is the direct exploitation of the video signal sent to the TV monitor, in conformity with the C.C.I.R. standard (the N.T.S.C. standard is also available). However, the study of stability and sensitivity of the intensifier lead us to create a second working mode necessary for the correct detection of faint objects (by an averaging filter improving the signal to noise ratio). The last mode is the integration by the C.C.D. itself: it allows a maximum of three-seconds integration time (therefore the detection of fainter objects), with the help of a thermoelectric cooling system. Moreover, the tests made on the 1.52 meter telescope of the O.A.N. (Calar-Alto, Spain) have been successful and confirm the capabilities of this camera to replace the intensified TV tube cameras, like the super-isocon camera.  相似文献   

Trends in age-at-recruitment and juvenile growth of cuttlefish, Sepia officinalis, from the English Channel     

Challier  Laurence; Dunn  Matthew R.; Robin  Jean-Paul 《ICES Journal of Marine Science》2005,62(8):1671-1682

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Hypotaurine and thiotaurine as indicators of sulfide exposure in bivalves and vestimentiferans from hydrothermal vents and cold seeps     

Garth L. Brand  Robin V. Horak  Nadine Le Bris  Shana K. Goffredi  Susan L. Carney  Breea Govenar  & Paul H. Yancey 《Marine Ecology》2007,28(1):208-218

Vesicomyid clams, vestimentiferans, and some bathymodiolin mussels from hydrothermal vents and cold seeps possess thiotrophic endosymbionts, high levels of hypotaurine and, in tissues with symbionts, thiotaurine. The latter, a product of hypotaurine and sulfide, may store and/or transport sulfide non‐toxically, and the ratio to hypotaurine plus thiotaurine (Th/[H + Th]) may reflect an animal's sulfide exposure. To test this, we analyzed seep and vent animals with in situ sulfide measurements. Calyptogena kilmeri clams occur at high‐sulfide seeps in Monterey Canyon, while C. (Vesicomya) pacifica clams occur at seeps with lower levels but take up and metabolize sulfide more effectively. From one seep where they co‐occur, both had gill thiotaurine contents at 22–25 mmol kg⁻¹ wet mass, and while C. (V.) pacifica had a higher blood sulfide level, it had a lower Th/[H + Th] (0.39) than C. kilmeri (0.63). However, these same species from different seeps with lower sulfide exposures had lower ratios. Bathymodiolus thermophilus [East Pacific Rise (EPR 9°50′ N)] from high‐(84 μm ) and a low‐(7 μm ) sulfide vents had gill ratios of 0.40 and 0.12, respectively. Trophosomes of Riftia pachyptila (EPR 9°50′ N) from medium‐(33 μm ) and low‐(4 μm ) sulfide vents had ratios of 0.23 and 0.20, respectively (not significantly different). Ridgeia piscesae vestimentiferans (Juan de Fuca Ridge) have very different phenotypes at high‐ and low‐sulfide sites, and their trophosomes had the greatest differences: 0.81 and 0.04 ratios from high‐ and low‐sulfide sites, respectively. Thus Th/[H + Th] may indicate sulfide exposure levels within species, but not in interspecies comparisons, possibly due to phylogenetic and metabolic differences. Total H + Th was constant within each species (except in R. piscesae); the sum may indicate the maximum potential sulfide load that a species faces.  相似文献   

Spatial and temporal variations in spectra of storm waves across a barred nearshore     

Robin G.D. Davidson-Arnott  David C. Randall 《Marine Geology》1984,60(1-4):15-30

Wave staffs and electromagnetic current meters were deployed on a profile across a two-bar system at Wendake Beach, southern Georgian Bay. This paper examines spatial and temporal changes in the characteristics of wave form, and the spectra of surface elevation and on-offshore current motion, during one storm. Non-linear effects of wave shoaling and breaking across the bars result in the appearance of secondary waves and both the wave and on-offshore current spectra have significant harmonic peaks during most of the storm. Significant low-frequency energy occurs only during the peak of the storm. While the peak frequency remains constant across the bar system, the proportion of energy in the primary peak is greatest in the troughs and lowest over the bar crests and there are similar changes in the proportion of energy in the first harmonic. However, in both surface elevation spectra and on-offshore current spectra, the greatest proportion of energy is found in frequencies related to the incident wind waves.  相似文献