Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848
http://ufdc.ufl.edu/UF00029229/00001

Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848

Éditeur(s) : Farming Systems Support Project, International Programs, Institute of Food and Agricultural Sciences, University of Florida Farming Systems Support Project, International Programs, Institute of Food and Agricultural Sciences, University of Florida ( Gainesville Fla )
Résumé : (Statement of Responsibility) préparé par: Farming Systems Support Project ... rédaction technique: John Caldwell, TIm Frankenberger; rédaction coordination: Lisette Walecka.
"Octobre 1987."
Spiral bound.
(Funding) Electronic resources created as part of a prototype UF Institutional Repository and Faculty Papers project by the University of Florida.
Haiti
Developing countries
Developing countries

71042283

Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848

Éditeur(s) : National Shellfisheries Association
Résumé : The subcellular fractionation of the digestive gland cells of the common cuttlefish Sepia officinalis was performed to investigate the distribution of metals between organelles and cytosol and the different cytosolic fractions separated by gel-filtration chromatography. Total metal concentrations vary over 3 orders of magnitude, ranging from dwt for Pb to dwt for Zn. With the exception of Cd, Co, and Cu, metals were mostly bound to the organelles. Whereas no specific organelle compartment was found for Mn, Ph, and Zn, Fe was mainly associated with nucleus, brown body, and "boule" fraction (i.e., 52%) and 44% of the total Ag was contained in the lysosomal and mitochondria enriched fraction. The link of metals with hydrosoluble proteins in the cytosolic fraction was investigated at 254 and 280 not. Direct relationship between cytosolic metal and metallothioneins could only be established for Ag and Cu, whereas Cd and Zn seem to mainly bind high (> 70 kDa) and low (< 4 kDa) molecular weight proteins.
The Journal of Shellfish Research (0730-8000) (National Shellfisheries Association), 2006-12 , Vol. 25 , N. 3 , P. 987-993

Droits : 2006 NSA
http://archimer.ifremer.fr/doc/2006/publication-2532.pdf
http://archimer.ifremer.fr/doc/00000/2532/

Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848

Éditeur(s) : Editorial Cultura Editorial Cultura ( México )
Résumé : (Bibliography) "Bibliografía": p. 56.
(Statement of Responsibility) conferencia pronunciada por su autor, coronel Adrián Cravioto ... en el salón de conferencias de la Unión racionalista de París (rama mexicana), durante la noche del 28 de mayo de 1943.
Belize
Guatemala
Guatemala
Belize

002814093
07451185
ANU2597
44012017

Éditeur(s) : Yale University
Résumé : Sea-surface temperature images of the coastal upwelling regions off Northwest Africa show that the core of upwelling is sometimes located far from the coast. This has been documented in three regions that share a common feature, namely a wide and shallow continental shelf. This upwelling feature plays a key role in the ecology of the Canary Current System. It creates an innerfront which provides retention for biological material, e.g. fish eggs and larvae, in the highly productive nearshore environment. An analytical model has been developed based on a two dimensional extension of Ekman's solution. The linear and steady response of a homogeneous ocean forced by an upwelling-favorable wind provides a mechanism for the upwelling separation from the coast. The merging of the surface and bottom Ekman layers induces a very weak cross-shore circulation and a "kinematic barrier" for the Ekman transport divergence. In the case of an alongshore wind, the barrier is located near the isobath h ≈ 0.4D, where D is the thickness of Ekman layers. This yields an upwelling cell which is essentially concentrated in the region 0.5D < h < 1.25D, with upwelling occurring preferentially near the isobath h ≈ 0.6D. It turns out that the cross-shore width of upwelling scales with D/S, the ratio of Ekman depth to bottom topographic slope. The application of this solution to real bathymetric profiles rationalizes, not only the offshore upwelling observations in Northwest Africa, but also the influence of topography on the cross-shelf structure of a wind-driven coastal upwelling. The model also quantifies the effect of the cross-shore wind component showing how it drives the nearshore pressure gradient adjustment and how it affects the upwelling. A linear numerical experiment reproduces the theoretical steady solution, thereby allowing investigation of the transient regime. Relaxation of the hypothesis in the numerical model validates the linear assumption of the theory and then allows investigation of the sensitivity to friction parameterizations and the influence of stratification. The latter leads to an "oscillation" of the upwelling cell with seaward migration driven by outcropping and homogeneization of the water column, and, coastal incursion driven by a "boundary layers splitting" process caused by shoreward advection of the isopycnal dome and stratification of the inner shelf.
Journal of Marine Research (Yale University), 2008-09 , Vol. 66 , N. 5 , P. 589-616

Droits : 2008 Yale University
http://archimer.ifremer.fr/doc/2008/publication-6334.pdf
DOI:10.1357/002224008787536790
http://archimer.ifremer.fr/doc/00000/6334/

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
Integrated Ocean Drilling Program Expedition 313 continuously cored uppermost Eocene to Miocene sequences on the New Jersey shallow shelf (Sites M27, M28, and M29). Previously, 15 Miocene (ca. 23-13 Ma) seismic sequence boundaries were recognized on several generations of multichannel seismic profi les using criteria of onlap, downlap, erosional truncation, and toplap. We independently recognize sequence boundaries in the cores and logs based on an integrated study of core surfaces, lithostratigraphy and process sedimentology (grain size, mineralogy, facies, and paleoenvironments), facies successions, stacking patterns, benthic foraminiferal water depths, downhole logs, core gamma logs, and chronostratigraphic ages. We use a velocitydepth function to predict the depths of seismic sequence boundaries that were tested by comparison with major core surfaces, downhole and core logs, and synthetic seismograms. Using sonic velocity (core and downhole), core density, and synthetic seismograms, we show that sequence boundaries correspond with acoustic impedance contrasts, although other stratal surfaces (e.g., maximum fl ooding and transgressive surfaces) also produce refl ections. Core data are suffi cient to link seismic sequence boundaries to impedance contrasts in 9 of 12 instances at Site M27, 6 of 11 instances at Site M28, and 8 of 14 instances at Site M29. Oligocene sequences have minimal lithologic and seismic expression due to deep-water locations on clinoform bottomsets. Miocene sequences (ca. 23-13 Ma) were sampled across several unconformity clinothems (prograding units) on topset, foreset, and bottomset locations. Excellent recovery allows core-seismic integration that confi rms the hypothesis that unconformities are a primary source of impedance contrasts. Our core-seismic-log correlations predict that key seismic surfaces observed in other sub surface investigations without core and/or well logs are stratal surfaces with sequence stratigraphic signifi cance.
EISSN: 1553-040X

insu-00946235
https://hal-insu.archives-ouvertes.fr/insu-00946235
DOI : 10.1130/GES00858.1

Éditeur(s) : Talleres tipo-litográficos nacionales Talleres tipo-litográficos nacionales ( Tegucigalpa Honduras )
Résumé : At head of title: Publicaciones de la Secretaría de relaciones exteriores de la república de Honduras.
Mosquitia (Nicaragua and Honduras)
Honduras
Nicaragua
Nicaragua
Honduras

001090392
02184354
AFH5854
39009381

Éditeur(s) : A Lahure A Lahure ( Paris )
Résumé : (Statement of Responsibility) présenté à Rome le 26 septembre 1903 par Joaquim Nabuco, envoyé extraordinaire et ministre plénipotentiaire du Brésil en mission spéciale auprès de Sa Majesté le roi d'Italie.
Brazil
Guyana
Guyana
Brazil

000128035
23886960
AAP4029

Éditeur(s) : National Imagery and Mapping Agency ( Bethesda, Maryland )
Résumé : (Language) In English and Spanish.
Relief shown by contours and spot heights; contour interval 5 meters.
"Map information as of 1999".
"Printed by Instituto Geográfico Nacional de Honduras 01-01".
"NIMA ref. no. E952XPUERTOCORT".
Includes legend, glossary, index to streets, guide to numbered features, hydrographic data, city location map and boundary diagram.
(Statement of Responsibility) prepared by the Instituto Geográfico Nacional (IGN) Honduras with the collaboration of the National Imagery and Mapping Agency (NIMA).
Honduras -- Puerto Cortés
Puerto Cortés (Honduras)

Droits : This item is a work of the U.S. federal government and not protected by copyright pursuant to 17 U.S.C. §105.
77736380
003712587
http://ufdc.ufl.edu/UF00098776/00001

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Hydrogen can be stored in the structure of nominally anhydrous minerals as point defects, and these impurities substantially modify many physical properties of Earth's mantle minerals. However, mantle rocks are composed of mineral grains separated by grain boundaries and interphase grains boundaries. Therefore, as a potential hydrogen reservoir, grain boundaries should be given proper attention. Here, I report an experimental investigation into hydrogen diffusion through grain boundaries in polycrystalline aggregates Sintering and diffusion experiments were performed using a gas-medium high-pressure vessel at under pressure of 300 MPa and over a temperature range of 900-1,250 degrees C. The diffusion assembly consisted of a polycrystalline cylinder of aluminous spinel + olivine crystals with a talc cylinder as the main hydrogen source. A Ni capsule was used to buffer the oxygen fugacity at Ni-NiO Experimental durations varied from 5 min to 5 h. The presence of hydrogen in the crystals was measured by Fourier-transform infrared spectroscopy. The calculation of the diffusion coefficients was based on the estimation of the characteristic distance. The absence or presence of hydrogen recorded by the 'hydrogen sensor' olivines embedded in the aggregate allows the estimation of bounds on this characteristic distance. Results presented here suggest that hydrogen effective diffusion coefficients are only one order of magnitude faster (similar to 10(-9) m(2)s(-1) at 1,000 degrees C) than in an olivine single crystal along the [100] axis. Resulting diffusion coefficients for hydrogen in grain boundary are four orders of magnitude faster than in a single crystal, but this diffusivity is not fast enough to affect hydrogen mobility in mantle rocks with grain sizes greater than similar to 1 mm. Thus, very limited chemical homogenization would occur using grain boundaries diffusion in mantle hydrous peridotite for incompatible and volatile element, such as hydrogen.
ISSN: 0010-7999

hal-00564353
https://hal.archives-ouvertes.fr/hal-00564353
DOI : 10.1007/s00410-010-0512-4

Éditeur(s) : A Lahure A Lahure ( Paris )
Résumé : (Statement of Responsibility) présenté à Rome le 26 septembre 1903 par Joaquim Nabuco, envoyé extraordinaire et ministre plénipotentiaire du Brésil en mission spéciale auprès de Sa Majesté le roi d'Italie.
Brazil
Guyana
Guyana
Brazil

000128035
23886960
AAP4029

Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
In the Oman ophiolite crustal section, a contact zone between the gabbro unit and the volcanics and diabase sheeted dikes, called the root zone of the sheeted dike complex, has been recently mapped at a fine scale in a selected area. The Oman ophiolite is derived from a fast spreading ridge which had a melt lens located between the main gabbro unit and the root zone of the sheeted dike complex. With a few exceptions accounted for, this horizon has a fairly constant thickness, similar to 100 m, and a crude internal pseudo-stratigraphy. At the base of the root zone are isotropic ophitic gabbros interpreted as a thermal boundary layer. This layer is transitional between the magmatic system of the melt lens, convecting at 1200 degrees C, and a high-temperature (< 1100 degrees C) hydrothermal system, convecting within the root zone. Above this level, the isotropic gabbros have been, locally, largely molten due to an influx of seawater, at similar to 1100 degrees C, thus generating varitextured ophitic and pegmatitic gabbros. These latter gabbros constitute the upper part of the root zone and are associated with trondjhemitic intrusions as screens in the lower sheeted dikes. Diorites and trondjhemites were also generated by hydrous melting, at temperatures below 1000 degrees C. The whole root zone is a domain of very sharp average thermal gradient (similar to 7 degrees C/m). At the top of the root zone, a new thermal boundary layer, with diabase dikes hydrated in amphibolite facies conditions, separates the preceding high- temperature convective system from the well-known greenschist facies (< 450 degrees C) hydrothermal system operating throughout the sheeted dike complex, up to the seafloor. The isotropic gabbros near the base of the root zone are intruded by protodikes with distinctive microgranular margins and an ophitic center. Protodike swarms are exceptional because, intruding a medium at similar to 1100 degrees C, they are largely destroyed by dike-in-dike intrusions and by hydrous melting. However, they demonstrate that this zone was generated by melt conduits issued from the underlying melt lens. Each dike of the sheeted dike complex is thus fed by one protodike. As this zone has been recently drilled by IODP in the eastern Pacific Ocean, a brief comparison is proposed.
ISSN: 1525-2027

hal-00411331
https://hal.archives-ouvertes.fr/hal-00411331
DOI : 10.1029/2007GC001918

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Talc is a hydrous magnesium rich layered silicate that is widely disseminated in the Earth from the seafloor to over 100 km depth, in ultra-high pressure metamorphism of oceanic crust. In this paper we determine the single crystal elastic constants at pressures from 0 to 12 GPa of talc triclinic (C 1¯) and monoclinic (C2/c) polytypes using ab initio methods. We find that talc has an extraordinarily high elastic anisotropy at zero pressure that reduces with increasing pressure. The exceptional anisotropy is complemented by a negative Poisson's ratio for many directions in crystal space. Calculations show that talc is not only one of very few common minerals to exhibit auxetic behaviour, but the magnitude of this effect may be the largest reported so far for a mineral. The compression (Vp) and shear (Vs) wave velocity anisotropy is 80% and 85% for the triclinic polytype. At pressures where talc is known be stable in the Earth (up to 5 GPa) the Vp and Vs anisotropy is reduced to about 40% for both velocities, which is still a very high value. Vp is slow parallel to the c-axis and fast perpendicular to it. This remains unchanged with increasing pressure and is observed in both polytypes. The shear wave splitting (difference between fast and slow S-wave velocities) at low pressure has high values in the plane normal to the c-axis, with a maximum near the alow asterisk-axis in the triclinic and the b-axis in the monoclinic polytype. The c-axis is the direction of minimum splitting. The pattern of shear wave splitting does not change significantly with pressure. The volume fraction of talc varies between 11 and 41% for hydrated mantle rocks, but the lack of data on the crystallographic preferred orientation (CPO) precludes a detailed analysis of the impact of talc on seismic anisotropy in subduction zones. However, it is highly likely that CPO can easily develop in zones of deformation due to the platy habit of talc crystals. For random aggregates of talc, the isotropic Vp, Vs and Vp/Vs ratio have significantly lower values than those of antigorite and may explain low-velocity regions in the mantle wedge. Vp/Vs ratios are more complex in anisotropic media because there are fast and slow S-waves, resulting in Vp/Vs1 and Vp/Vs2 ratios for every propagation direction, making interpretation difficult in deformed polycrystalline talc with a CPO. Talc on the subduction plate boundary can strongly influence guided wave velocity as CPO would develop in this region of intense shearing. The very low coefficient of friction (< 0.1) of talc above 100 °C could also explain silent earthquakes at shallow depths (ca 30 km) along the subduction plate boundaries, frequently responsible for tsunami.
ISSN: 0012-821X

hal-00411481
https://hal.archives-ouvertes.fr/hal-00411481
DOI : 10.1016/j.epsl.2008.07.047

Éditeur(s) : Impr. de L. Tasso y Serra Impr. de L. Tasso y Serra ( Barcelona )
Résumé : (Citation/Reference) Batista Villarreal, T. Publicaciones periódicas cubanas (1965), p. 36.
(Dates or Sequential Designation) Año 1, núm. 1 (enero de 1885)-
(Dates or Sequential Designation) -año 4, núm. 6 (29 de feb. de 1888)?
(Numbering Peculiarities) Año 2 complete in two numbers.
Description based on: año 1, núm. 2 (enero de 1885); title from masthead.
Editor: Domingo Figarola-Caneda.
Distributed in Havana.
Indexes issued annually.
Rare Book Copy bound privately in red cloth, stamped with red, black and gold with publisher's index and supplement titled: Ultima moda; bears bookplate of former owner, Alberto Parreño; also inscribed by Federico Cajial to D. Antonio, Elosqui.
Cuba -- Havana
Spain -- Barcelona
Cuba
Cuba
Spain
Barcelona
Cuba
Havana

002934220
52479416
APG5848

Éditeur(s) : Farming Systems Support Project, International Programs, Institute of Food and Agricultural Sciences, University of Florida Farming Systems Support Project, International Programs, Institute of Food and Agricultural Sciences, University of Florida ( Gainesville Fla )
Résumé : (Statement of Responsibility) préparé par: Farming Systems Support Project.
Spiral bound.
Cover title.
(Funding) Electronic resources created as part of a prototype UF Institutional Repository and Faculty Papers project by the University of Florida.
Haiti
Developing countries
Developing countries

71044673

Éditeur(s) : J. Kugelmann J. Kugelmann ( Paris )
Résumé : Bound with this is the author's Haïti et sa Banque nationale. Troisième partie. Paris, Kugelmann, 1896.

24178327
ocm24178327