Résumé : The slides were taken on collecting trips sponsored by the William L. Bryant Foundation, where books, music and art indigenous to the regions were gathered. They are organized by geographical location.
View of the mountains of Kenscoff from Fort Jacques. Kenscoff is located southeast of Port-au-Prince.
Haiti -- Caribbean region
Haiti
Haiti
Haiti

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
CFM1972_01a
Sheet 56:19
http://ufdc.ufl.edu/CA01200274/00001

Éditeur(s) : The Illustrated London News The Illustrated London News ( London )
Résumé : (Funding) Support for the development of the technical infrastructure and partner training provided by the United States Department of Education TICFIA program.
Hand colored, ca. 2004.
Page from The Illustrated London News, November 16, 1867.
(Biographical) A major, class-4 hurricane crossed the Virgin Islands--including St. Thomas and Tortola--and southeast Puerto Rico in October 1867.
St. Thomas (V. I.)
St. Thomas (V. I.)

Droits : All rights reserved by the source institution.
2005-274-1

Résumé : Arbusto de 2 a 3 m, aromático, de madera suave. Hojas ovadas u oblongo-ovadas de hasta 60 cm de largo, agudas a corto acuminadas en el ápice, cordadas en la base, lóbulos basales redondeados, marcadamente desiguales. Espigas de color verde pálido, de 10 a 20 cm de largo; brácteas redondeadas y densamente ciliadas. Frutos pequeños agrupados en las espigas.
Arbuste pouvant atteindre 2 à 3 m, aromatique, bois tendre. Feuilles ovées ou oblongues-ovées, pouvant avoir 60 cm de long, à l’extrémité aiguë à terminée en pointe courte, cordées à la base, lobes à base arrondie, fortement inégaux. Epis de couleur vert pâle, de 10 à 20 cm de long; bractées arrondies et pourvues de cils denses. Petits fruits groupés sur les épis.
Soft-wooded aromatic shrub or tree 1-6m high.  Leaves ovate or ovate-elliptical, 20-40 x 12-25 cm, acute to short acuminate at the apex, deeply and unequally cordate-auriculate at base, margins densely white-ciliate, petiole winged to the apex; inflorescence a spike, whitish to light yellow, pendulous, 10-20 cm x 3-5 mm; fruit, small, three-angled.
Nativa del sureste de México y Centroamérica, cultivada y naturalizada en Cuba y Florida.
Originaire du sud-est du Mexique et de l’;Amérique Centrale, cultivée et naturalisée à Cuba et en Floride.
Native to southeast Mexico and Central America

http://www.tramil.net/fototeca/plant283

Résumé : Arbol de hasta 20 m; tronco liso y recto. Hojas opuestas, coriáceas, ovadas o elípticas de hasta 20 cm de largo, muy aromáticas. Panículas de alrededor de 12 cm de largo con muchas flores; flores en su mayoría agrupadas en la punta de la inflorescencia, sésiles; cáliz con 4 lóbulos redondeados, pubérulos; pétalos blancos suborbiculares; numerosos estambres blancos. Fruto aromático, generalmente subgloboso, verrugoso, con dos semillas suborbiculares.
Arbre pouvant atteindre 20 m; tronc lisse et droit. Feuilles opposées, coriaces, ovées ou elliptiques ayant jusqu’à 20 cm de long, très aromatiques. Panicules d’environ 12 cm de long avec nombreuses fleurs; fleurs pour la plupart groupées à la pointe de l’inflorescence, sessiles; calice à 4 lobes arrondis, pubérulents; pétales blancs suborbiculaires; nombreuses étamines blanches. Fruit aromatique, généralement presque arrondi, verruqueux, avec deux graines suborbiculaires.
Tree, up to 20 m high with pale brown bark. Leaves simple, opposite, entire, leathery, oblong to elliptical, 6-20 cm long, glandular dotted, aromatic when crushed; inflorescence a compound panicle 4-12 cm long, with many white, short-lived flowers, 1.5mm long; fruit a globose, reddish-brown berry, 4-6.5 mm in diameter, producing an aromatic flavour of a mixture of nutmeg, clove and cinnamon.
Sureste de México, América Central y Antillas.
Sud-est du Mexique, Amérique Centrale et Antilles.
Southeast Mexico, Central America and the Antilles.

http://www.tramil.net/fototeca/plant278

Résumé : Arbol de 10 a 15 m o más, de copa densa, redondeada; corteza resinosa. Hojas alternas, oblongo-lanceoladas, agudas o acuminadas, subcoriáceas. Flores verdosas o amarillentas, fragantes, en grandes panículas; pétalos de 5 mm, glabros. Drupa elipsoidea a oblícuamente reniforme, de 5 a 15 cm, mesocarpo carnoso amarillo, agridulce.
Arbre de 10 à 15 m ou davantage, tête dense, arrondie; écorce résineuse. Feuilles alternes, oblongues-lancéolées, pointues ou acuminées, subcoriaces. Fleurs verdâtres ou jaunâtres, odorantes, en grandes panicules; pétales de 5 mm, glabres. Drupe ellipsoïdale à obliquement réniforme, de 5 à 15 cm, mésocarpe charnu, jaune, aigre-doux.
Tree evergreen, 10-15 m high with a dense, rounded crown of foliage, bark resinous.  Leaves alternate, simple, spirally arranged, lanceolate-elliptical, 10-25 cm x 2.5-8 cm; inflorescence a terminal panicle ca 30 cm long; flowers 5-8 mm in diameter, greenish or yellowish, fragrant; fruit a fleshy drupe, ellipsoid to obliquely reniform, 5-15 cm long.
Nativa del sureste asiático, cultivada en zonas tropicales y subtropicales de todo el mundo.
Originaire du sud-est asiatique, cultivée dans les zones tropicales et subtropicales du monde entier.
Native to Southeast Asia, cultivated in tropical and su

http://www.tramil.net/fototeca/plant220

Éditeur(s) : Amsterdam : G. et I. Blaeu, 1635 Amsterdam : G. et I. Blaeu, 1635
Résumé : Detached from and originally published in the French ed. of W.J. Blaeu's atlas: Le theatre du monde ou Novvel atlas, 1635. Shows southeast coast of North America from Virginia to north coast of South America to east of Trinidad, west coast of Central America, West Indies. Includes embellished title cartouche, coats-of-arms. ill. scale and ill. of ships at sea. Includes scales in milliaria germanica and milliaria hispanica. Text in French on verso: Les isles de Amerique en l'ocean septentrional, audevant du Golfe de Mexique, & quelques provinces du continent. Engraved. Hand colored. Has vertical fold line at center of sheet. Relief represented by hachures. UCF Libraries' copy has reinforcement on right edge. This item is part of the West Indies collection.
(Language) Title in Latin: place names primarily in Spanish and Latin ; text on verso in French.
Caribbean area
North America
South America
Caribbean area
West Indies
West Indies

Droits : All rights to images are held by the respective holding institution. This image is posted publicly for non-profit educational uses, excluding printed publication. For permission to reproduce images and/or for copyright information contact Special Collections & University Archives, University of Central Florida Libraries, Orlando, FL 32816 phone (407) 823-2576, email: speccoll@mail.ucf.edu
G4390 1635.B

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : GPS velocities and seismicity across the Betic-Rif Arc structural domains (Morocco and Iberia) provide a basis to evaluate present-day seismotectonic processes between different deformation belts. The results show asymmetric movements in the complex Alboran system accommodating the convergence between the African (Nubian) and Eurasian plates. While the Betic Mountains are attached to Iberia, moving toward the southeast with respect to Africa, the Rif is divided into three blocks with distinct displacements relative to Nubia: (1) the Tangier block moving southeastward, (2) the Central Rif block moving SSW, and (3) the Oriental Rif block undergoing clockwise rotation. GPS-derived motions decrease in rate from the Rif nappes complex to the foreland.
ISSN: 0010-7999

hal-00411144
https://hal.archives-ouvertes.fr/hal-00411144
DOI : 10.1016/j.crte.2008.02.003

Éditeur(s) : Amer Geophysical Union
Résumé : New high-resolution multichannel seismic data (GWADASEIS-2009 and JC45/46-2010 cruises; 72 and 60 channels, respectively) combined with previous data (AGUADOMAR-1999 and CARAVAL-2002; 6 and 24 channels, respectively) allow a detailed investigation of mass-wasting processes around the volcanic island of Montserrat in the Lesser Antilles. Seven submarine deposits have sources on the flanks of Montserrat, while three are related to the nearby Kahouanne submarine volcanoes. The most voluminous deposit (similar to 20 km(3)) within the Bouillante-Montserrat half-graben has not been described previously and is probably related to a flank instability of the Centre Hills Volcano on Montserrat, while other events are related to the younger South Soufriere Hills-Soufriere Hills volcanic complex. All deposits are located to the south or southeast of the island in an area delimited by faults of the Bouillante-Montserrat half-graben. They cover a large part of the southeast quarter of the surrounding seafloor (similar to 520 km(2)), with a total volume of similar to 40 km(3). Our observations suggest that the Bouillante-Montserrat half-graben exerts a control on the extent and propagation of the most voluminous deposits. We propose an interpretation for mass-wasting processes around Montserrat similar to what has happened for the southern islands of the Lesser Antilles.
Geochemistry Geophysics Geosystems (1525-2027) (Amer Geophysical Union), 2011-05 , Vol. 12 , N. 5 , P. Q05006

Droits : Copyright 2011 by the American Geophysical Union
http://archimer.ifremer.fr/doc/00200/31100/29510.pdf
DOI:10.1029/2010GC003451
http://archimer.ifremer.fr/doc/00200/31100/

Éditeur(s) : HAL CCSD
Résumé : The Karakorum Fault zone (KFZ), lying in the west of the Tibetan plateau, is an important dextral strike-slip fault and the important northern geological boundary of the west Himalaya. In the AyilaRi' gyu Range-Gai Basin area lying in the southeast of the KFZ, Ar-40/Ar-39 thermochronologic analysis was performed on the syn-tectonic minerals in the, metamorphic rocks in the Karakorum ductile shear zone, with the base of petrology and deformation structure researches. According to the microstructure features, the minerals in the shear zone recorded the continuous deformation from high ( > 600 degrees C) to low temperature ( < 250 degrees C) appeared as that the nearly horizontal dextral shearing has transformed into the oblique dextral normal slip, made the greenschist facies of deformation stack oil the early medium-high temperature deformation, indicated the uplift during the slip. The thermochronologic revealed the continuous shear process from the early Miocene to 4Ma at least, which containing three rapid cooling stage: from 25 similar to 22Ma to 21 similar to 18Ma, the deformation locally stopped or slower in the, shallow high temperature shear process; from 15Ma to 12Ma, the rapid uplift of the AyilaRi' gyu Range, the initial formation of the Gar Basin together with the main deep incision of river during the strip-slip of the KFZ; since 9Ma, the AyilaRi' gyu Range has increased the rapid uplift and the Gar Basin has formed finally. According to the different levels of deformation and the dextral displacement of the surface landform with different ages, the long term slip rate and the uplift rate indicated the intense dextral strike slip and uplift associated since the late Quarternary Period.
Acta Petrologica Sinica

hal-00411572
https://hal.archives-ouvertes.fr/hal-00411572

Éditeur(s) : Amer Geophysical Union
Résumé : A tectonic model of the evolution of the northern half of the South Fiji Basin, including the Minerva Triple Junction and Cook Fracture Zone, is developed from regional gravity, multibeam bathymetry, and a new interpretation of magnetic anomalies pinned to radiometric dates of oceanic crust in the basin. The geometry and age of a portion of the Minerva Triple Junction and the Cook-Minerva spreading center (the connection from the triple junction to the Cook Fracture Zone, which accommodated coeval opening of the Norfolk Basin), are resolved with multibeam bathymetry and magnetics. The South Fiji Basin opened from about 34 to 15 Ma in an anticlockwise sweep about an Euler pole located at the northern end of the present Lau Ridge. This rotation and a rigidly straight southeastward motion of the Three Kings Ridge were accommodated by the configuration of the triple junction changing from ridge-fault-fault to ridge-ridge-fault to ridge-ridge-ridge. During this evolution the southeastern arm of the system, the Julia Fracture Zone, underwent several transformations and the Cook-Minerva spreading center experienced repeated ridge jumps. The kinematics of the northern South Fiji Basin dictate, to a large extent, the evolution of the southern South Fiji Basin and the Norfolk Basin. This in turn leads to the interpretation of a complex trench-trench-double transform fault framework at the northern New Zealand margin, which explains most aspects of the geology, structure, and arc volcanic history of the margin and provides a radical new setting for the origin of the Northland Allochthon.
Geochemistry Geophysics Geosystems (1525-2027) (Amer Geophysical Union), 2011-02 , Vol. 12 , N. Q02004 , P. 1-20

Droits : 2011 American Geophysical Union. All Rights Reserved.
http://archimer.ifremer.fr/doc/00030/14112/11362.pdf
DOI:10.1029/2010GC003291
http://archimer.ifremer.fr/doc/00030/14112/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Tyrrhenian Sea is usually interpreted to be a Neogene back-arc basin that opened by continental rifting and oceanic spreading caused by the eastward migration of the Apennine subduction system during Miocene and Pliocene times. Rifting of the southern Tyrrhenian Sea started first along the Eastern Sardinian margin during the middle to late Miocene times, including the Messinian. The "METYSS" project aims at better constraining the relationships between crustal tectonics, salt tectonics and sedimentation from Messinian times to present-day. The "METYSS 1" cruise (2009) allowed to acquire about 1200 km of HR seismic-reflection profiles along the Eastern Sardinian margin, Western Tyrrhenian Sea. This data set clearly illustrates that this area has been highly dissected during the rifting stage by N-S trending normal faults delineating ridges and basins, as previously described. The Messinian seismic markers (UU and MU) locally display fan-shaped stratal geometries, but the mechanism responsible for such geometries, salt tectonics or rifting, has yet to be carefully deciphered. We also mapped the spatial distribution of the mobile salt. The highly variable thickness of the small confined salt basins may be related to the initial pre-Messinian basin geometry, to the fact that salt deposition was syn-rift or to salt movement. Southeastward, salt tectonics is vigorous in unconfined basins and appears to have started early during the UU deposition. More surprisingly, our data demonstrate that some of the major faults have been significantly reactivated during the post-rift period, up to late Quaternary time, as shown by bathymetric scarps and associated debris flows. Moreover, some of this post-rift deformation can be evidenced within the Plio-Quaternary sequence by a regional unconformity. The post-Miocene deformation style varies greatly between different areas of the margin, and can also be strongly influenced by the presence or absence of mobile Messinian salt.
ISSN: 0040-1951

hal-00996665
https://hal.archives-ouvertes.fr/hal-00996665
DOI : 10.1016/j.tecto.2013.12.015

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The NW-trending Talas-Ferghana Fault (TFF) in Kyrgyzstan, Central Asia, is one of the largest intracontinental strike-slip faults in the world. It extends over a distance of more than 2000 km from southern Tourghai to western Tarim and exhibits a maximum dextral offset of ∼200 km during the late Palaeozoic to present. The history of the fault provides important insights for the understanding of the evolution of southern Central Asia but remains poorly constrained due to lack of reliable geochronological data. We present new Ar-Ar ages and structural data from the Kyrgyz West Tianshan, that elucidate the kinematic history of the TFF in the Palaeozoic and Mesozoic. 40Ar/39Ar ages on mylonitic white micas document a deformational history consisting of several episodes. A late Carboniferous age of 312 ± 4 Ma point to initiation of top-to-the-south and dextral transpressional deformation during a metamorphic overprint in Precambrian and Palaeozoic rocks along the northern compartment of the TFF. The main phase of dextral motion along the entire fault occurred in the Permian as suggested by minimum ages of 260-290 Ma obtained at two different locations in the NW and central parts of the TFF. Partial isotopic resetting occurred between 240 and 210 Ma and younger ages of <200-210 Ma are ascribed to late brittle reactivation and hydrothermal fluid flow in the Late Triassic to Early Jurassic times. The Jurassic trans-tensional phase is featured by emplacement of 195 ± 3 Ma pegmatitic dykes. The Ar-Ar mineral ages and structural data argue for a major phase of dextral shearing, affecting the entire region from the West Tianshan to Mongolia in the late Permian and leading to formation of almost equally spaced major NW-trending dextral strike-slip faults. The uniform character of this deformation indicates that the process of amalgamation in this part of the CAOB ended prior to the late Permian, and Central Asia evolved as a single coherent continental block since that time.
ISSN: 0743-9547

hal-00831326
https://hal.archives-ouvertes.fr/hal-00831326
DOI : 10.1016/j.jseaes.2013.02.012

Éditeur(s) : HAL CCSD Elsevier
Résumé : Une approche par datations multiples a été menée sur les dépôts de sédiments de crue retrouvés dans les gorges du Gardon (Languedoc). Le plomb-210, le césium-137 et l’analyse géochimique des sédiments contaminés par les mines ont été utilisés pour reconstruire l’histoire des dépôts de crue. Cette approche a été combinée avec l’historique des crues du Gardon depuis 1890 pour affiner l’approche géochronologique. Au niveau de la cavité GG et de la terrasse GE les analyses ont permis d’illustrer les mécanismes d’érosion-redéposition pouvant perturber les séquences de sédiments. Les enregistrements des dépôts de sédiments de crue sont complets sur la terrasse GE située à 10 m au-dessus du lit mineur à partir de 1958, et incomplets auparavant. Sur la période 1880-1958, 25 crues ont eu un débit suffisant (>1450 m3/s) pour recouvrir la terrasse, alors que l’on recense seulement 5 à 6 crues depuis 1958 (pour un débit de submersion supérieur à 1700 m3/s). L’augmentation progressive du débit de submersion et la fréquence moindre d’inondation de la terrasse ont pu permettre sur la période récente la stabilisation de la couche de surface par la végétation et limiter l’érosion lors de crues importantes. Les enregistrements semblent complets dans la cavité GG située à 15 m au-dessus du lit mineur. La fréquence moindre de submersion à ce niveau plus élevé peut expliquer une meilleure stabilisation des dépôts de crue, rendus moins vulnérables à l’érosion. La datation au radiocarbone a été testée même si elle ne permet pas de dater avec précision les dépôts de crue des derniers siècles. Sur la terrasse GE, 80% des dates au carbone 14 sur charbon de bois sont beaucoup trop vieilles par rapport aux autres techniques de datation, ce qui peut s’expliquer par une remobilisation/déstockage de charbons de bois anciens. Les datations radiocarbone sur graines donnent de meilleurs résultats, car issues d’une production annuelle, plus facilement décomposable et moins sujette à des dépôts intermédiaires. Au final, il apparaît que la technique de datation par radiocarbone sur des charbons de bois retrouvés dans les séquences sédimentaires n’est pas fiable, alors qu’elle est la plus pratiquée en paléo-hydrologie. L’utilisation combinée du plomb-210, du césium-137, de l’analyse géochimique des sédiments et des informations sur les crues historiques a permis de discriminer et de dater les différents dépôts de crue de ce dernier siècle dans la cavité GG et la terrasse GE. / A multidating approach was carried out on slackwater flood deposits, preserved in valley side rock cave and terrace, of the Gardon River in Languedoc, southeast France. Lead-210, caesium-137, and geochemical analysis of mining-contaminated slackwater flood sediments have been used to reconstruct the history of these flood deposits. These age controls were combined with the continuous record of Gardon flow since 1890, and the combined records were then used to assign ages to slackwater deposits. The stratigraphic records of terrace GE and cave GG were excellent examples to illustrate the effects of erosion/preservation in a context of a progressively self-censoring, vertically accreting sequence. The sedimentary flood record of the terrace GE located at 10 m above the channel bed is complete for years post-1958 but incomplete before. During the 78-year period 1880-1958, 25 floods of a sufficient magnitude (> 1450 m3/s) have covered the terrace. Since 1958, however, the frequency of inundation of the deposits has been lower:only 5 or 6 floods in 52 years have been large enough to exceed the necessary threshold discharge (> 1700 m3/s). The progressive increase of threshold discharge and the reduced frequency of inundation at the terrace could allow stabilisation of the vegetation cover and improved protection against erosion from subsequent large magnitude flood events. The sedimentary flood record seems complete for cave GG located at 15 m above the channel bed. Here, the low frequency of events would have enabled a high degree of stabilisation of the sedimentary flood record, rendering the deposits less susceptible to erosion. Radiocarbon dating are used in this study and compared to the other dating techniques.Eighty percent of radiocarbon dates on charcoals were considerably older than those obtained by the other techniques in the terrace. On the other hand, radiocarbon dating on seeds provided better results. This discrepancy between radiocarbon dates on charcoal and seeds is explained by the nature of the dated material (permanent wood vs. annual production and resistance to degradation process). Finally, we showed in this study that although the most common dating technique used in paleoflood hydrology is radiocarbon dating, usually on charcoal preserved within slackwater flood sediments, this method did not permitus to define a coherent age model. Only the combined use of lead-210, caesium-137, and geochemical analysis of mining-contaminated sediments with the instrumental flood record can be applied to discriminate and date the recent slackwater deposits of the terrace GE and cave GG.
ISSN: 0169-555X

hal-01059669
https://hal.archives-ouvertes.fr/hal-01059669
https://hal.archives-ouvertes.fr/hal-01059669/document
https://hal.archives-ouvertes.fr/hal-01059669/file/ly2014-pub00040953.pdf
IRSTEA : PUB00040953

Éditeur(s) : HAL CCSD Springer
Résumé : International audience
We present here a synthesis of the evolution of rifted continental margin systems in the Gulf of Aden. These margins are volcanic to the west of the Gulf of Aden, where they are influenced by the Afar hotspot, and non-volcanic east of longitude 46° E. The combined use of magnetics, gravity, seismic reflection, field observations (tectonic, stratigraphic and sedimentological) and oil well data allowed us to obtain better constraints on the timing of continental rifting and seafloor spreading. From the Permo-Triassic to the Oligocene, the Arabian-African plate was subject to distributed extension, probably due, at least from the Cretaceous, to tensile stresses related to the subduction of the Tethysian slab in the north. In Late Eocene-Early Oligocene, 34-33 Ma ago, rifting started to localise along the future area of continental breakup. Initially guided by the inherited basins, continental rifting then occurred synchronously over the entire gulf before becoming localised on the northern and southern borders of the inherited grabens, in the direction of the Afar hotspot. In the areas with non-volcanic margins (in the east), the faults marking the end of rifting trend parallel to the inherited grabens. Only the transfer faults cross-cut the inherited grabens, and some of these faults later developed into transform faults. The most important of these transform faults follow a Precambrian trend. Volcanic margins were formed in the west of the Gulf, up to the Guban graben in the southeast and as far as the southern boundary of the Bahlaf graben in the northeast. Seaward dipping reflectors can be observed on many oil industry seismic profiles. The influence of the hotspot during rifting was concentrated on the western part of the gulf. Therefore, it seems that the western domain was uplifted and eroded at the onset of rifting, while the eastern domain was characterised by more continuous sedimentation. The phase of distributed deformation was followed by a phase of strain localisation during the final rifting stage, just before formation of the Ocean-Continent Transition (OCT), in the most distal graben (DIM graben). About 20 Ma ago, at the time of the continental break-up, the emplacement of the OCT started in the east with exhumation of the subcontinental mantle. Farther west, the system was heated up by the strong influence of the Afar hotspot, which led to breakup with much less extension. In the Gulf of Aden (s.str), up to the Shukra El Sheik fracture zone, oceanic spreading started 17.6 Ma ago. West of this fracture zone, oceanic accretion started 10 Ma ago, and 2 Ma ago in the Gulf of Tadjoura. Post-rift deformation of the eastern margins of the Gulf of Aden can be seen in the distal and proximal domains. Indeed, the substantial post-rift uplift of these margins could be associated with either the continental break-up, or activity of the Afar hotspot and related volcanic/magmatic activity. Uplift of the northern proximal margin was still active (e.g. stepped beach rocks exposed at 60 m of 2 Ma; 30 m of 35,200 years; 10 and 2 m) and active volcanoes can be inferred at depths of between 70 and 200 km beneath the margin (at 5-10 km distance from the coast). On the distal margin, heat flow measurements show a high value that is associated with post-rift volcanic activity and the development of a volcano (with flows and sills) shortly after the formation of the OCT. The Afar hotspot is therefore important for several reasons. It allows the localisation of deformation along the Red Sea/Aden system and the rapid opening of the Gulf after the continental break-up; its influence also seems to persist during the post-rift period.
ISSN: 1866-7411

hal-01053089
https://hal.archives-ouvertes.fr/hal-01053089
DOI : 10.1007/s12517-011-0475-4

Éditeur(s) : HAL CCSD MAIK Nauka/Interperiodica
Résumé : International audience
The paper is concerned with the kinematics of the major faults, their pattern, and the time of occurrence of compression and extension deformations in the southeast of the Eastern Sayan. The geometry of the mountain ranges and the kinematics of the major faults exhibit northeast-oriented compression responsible for the current processes of relief formation, which corresponds to the direction of the vector of deformations associated with the Indo-Asian collision. The results obtained thus far may be indicative of the remote influence of collision on the orogenic activity and transpressional deformations in the Eastern Sayan since the end of the Miocene. Morphotectonic analysis has shown that the areas of Quaternary extension- related deformations in the Eastern Sayan are not a response to active rifting in the Baikal Rift Zone. The position and geometry of the subsided blocks and magma ruptures point to the fact that they form locally as extension structural elements near the strike-slip faults. The strike-slip and thrust faults are widespread and play the leading role in the development of the southeastern part of the Eastern Sayan.
ISSN: 0016-8521

insu-00667345
https://hal-insu.archives-ouvertes.fr/insu-00667345
DOI : 10.1134/S001685211101002X

Éditeur(s) : Gauthier-Villars
Résumé : Moored current measurements carried out from 31 March 1990 to 15 September 1991 in two stages at a point (near 6 degrees N) located over the mid-continental slope off French Guiana are presented. Six current meters were positioned between 200 and 2700 m depth. Upper level mean current data showed a northwestward flowing North Brazil Current (NBC) with mean velocity values decreasing from 10 cm/s in the range 200-250 m to almost zero at 800 m depth, the level of the Antarctic Intermediate Waters. In the range 500-800 m, the current reversed in spring in the presence of the southeastward Western Boundary Under Current (WBUC); the mean velocity from February to June 1991 is around 2 cm/s. Deep currents over the continental rise show a strong southeastward Deep Western Boundary Current extending from around 1000 m depth to the bottom (3000 m depth in this case) with mean core speeds of 20 cm/s at 2000-2070 m depth. Transport estimates based on these data and a few Pegasus sections for the mean vertical and lateral extensions of the DWBC yield a value of 21 x 10(6) m(3)/s at that location. Low-frequency current fluctuations were dominated by a well-defined 50- to 70-day period oscillation with peak-to-peak northwestward velocity amplitude of around 90 cm/s at the upper level. The mean vertical eddy kinetic energy distribution showed an abrupt decrease of the energy down to 800 m depth and a slight decrease below and down to the bottom.
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1994 , Vol. 17 , N. 4 , P. 345-354

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00098/20897/18510.pdf
http://archimer.ifremer.fr/doc/00098/20897/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La zona del sudeste de la provincia de Buenos Aires (Argentina), se vislumbra como territorio fértil para los estudios culturales debido a su densidad histórica, social y patrimonial, en un marco de disímiles condiciones geográficas. Dos ciudades bonaerenses intermedias, Mar del Plata y Tandil, se han destacado por sus procesos de construcciones socio-culturales asociadas al ocio y al turismo. El estudio propuesto abarca la primera mitad del siglo XX para reconocer las transformaciones acontecidas en el hábitat y en el habitar, observando las prácticas sociales y las renovadas relaciones entre cuerpo y espacio que darán lugar a propuestas diferenciadas en relación con la estadía costera o serrana. Para ello se hará hincapié en la lectura de la revista ilustrada Caras y Caretas, en particular, en las imágenes de notas y avisos publicitarios.
The southeast zone of the province of Buenos Aires (Argentina), it is glimpsed as fertile territory for the cultural studies due to its historical, social and heritage density, in a frame of dissimilar geographical conditions. Two intermediate cities, Mar del Plata and Tandil, have been outlined for their processes of sociocultural constructions associated with leisure and tourism. The proposed study includes the first half of the XXth century to recognize the transformations happened in the habitat and the living, observing the social practices and the renewed relations between body and space that will give place to different proposals in relation with the coastal or highland demurrage. For this, it will be emphisized in the reading of the illustrated magazine Caras y Caretas, especially, the images of notes and advertising notices.
La zone du sud-est de la province du Buenos Aires (Argentine) est perçue comme un territoire fertile pour les études culturelles pour des raisons historique, sociale et patrimoniale, avec des conditions géographiques dissemblables. Deux villes intermédiaires, Mar del Plata et Tandil, se distinguent par leur processus de construction socioculturelle associée aux loisirs et au tourisme. L'étude proposée concerne la première moitié du XXe siècle. Elle s’attache à reconnaître les transformations des habitats et des modes de vie, en observant les pratiques sociales et les relations renouvelées entre le corps et l'espace en relation avec l’environnement du lieu de séjour, côtier ou montagnard. Pour cela, on mettra l'accent sur la lecture de la revue illustrée Caras y Caretas, en particulier les illustrations et les avis publicitaires.
Argentine
Buenos Aires
Mar del Plata
Tandil

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7626
http://journals.openedition.org/etudescaribeennes/7626

Résumé : Arbol pequeño o mediano de hasta 15 m de alto, glabro. Hojas alternas, compuestas, grandes; folíolos subcoriáceos, oblongos, redondeados en el ápice, cuneados en la base, verdes en el haz, pálidos o glaucos en el envés. Panículas muy ramificadas; numerosas flores blancuzcas, densamente agregadas en las ramas. Drupa oval a oblongo-oval de color rojo brillante y negra al madurar, con delgada pulpa blanca.
Arbre petit ou moyen pouvant atteindre 15 m de hauteur, glabre. Feuilles alternes, composées, grandes; folioles subcoriaces, oblongs, arrondis à la pointe, cunéiformes à la base, verts sur le dessus, pâles ou glauques à l&rsquo;envers. Panicules très ramifiées; nombreuses fleurs blanchâtres, recouvrant densément les branches. Drupe ovale à oblongue-ovale de couleur rouge brillant, noire à maturité, avec fine pulpe blanche.
Small or medium-sized tree,6-30 m high, glabrous.  Leaves alternate, compound; leaflets 8-15 subcoriaceous, oblong, round at the apex, cuneate at the base, green on the upper side, pale or glaucous on the underside.  Panicles very ramified; flowers numerous, whitish, densely clustered on branches.  Drupe oval to oblong-oval, bright red, black when ripe, with thin white pulp.
Sureste de Florida, Cuba, La Hispaniola, sureste de México y Centroamérica.
Sud-est de la Floride, Cuba, La Hispaniola, sud-est du Mexique et Amérique centrale.
Southeast Florida, Cuba, La Hispaniola, Southeast Mexico and Central America.

http://www.tramil.net/fototeca/plant325

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
[1] Zircons and monazites from 6 samples of the North Ayilari dextral shear zone (NAsz), part of the Karakorum fault zone (KFZ), have been dated with the U-Th-Pb method, using both ID-TIMS and SIMS techniques. The ages reveal (1) inheritance from several events spanning a long period between the late Archean and the Jurassic; (2) an Eocene-Oligocene magmatic event (similar to 35-32 Ma); (3) an Oligo-Miocene magmatic event (similar to 25-22 Ma), at least partly synkinematic to the right-lateral deformation; and (4) a period of metamorphism metasomatism (similar to 22-14 Ma) interpreted as thermal and fluid advection in the shear zone. The Labhar Kangri granite located similar to 375 km farther Southeast along the KFZ is dated at 21.1 +/- 0.3 Ma. Such occurrence of several Oligo-Miocene granites along the KFZ, some of which show evidence for synkinematic emplacement, suggests that the fault zone played an important role in the genesis and /or collection of crustal melts. We discuss several scenarios for the onset and propagation of the KFZ, and offset estimates based on the main sutures zones. Our preferred scenario is an Oligo-Miocene initiation of the fault close to the NA range, and propagation along most of its length prior to similar to 19 Ma. In its southern half, the averaged long-term fault-rate of the KFZ is greater than 8 to 10 mm/a, in good agreement with some shorter-term estimates based on the Indus river course, or Quaternary moraines and geodesy. Our results show the KFZ cannot be considered as a small transient fault but played a major role in the collision history.
ISSN: 0278-7407

hal-00412570
https://hal.archives-ouvertes.fr/hal-00412570
DOI : 10.1029/2007TC002184

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A large sand injectite network is very well exposed in the area of Bevons, Southeast France. The associated sandstone turbiditic channel–fill and the host marls are the Aptian–Albian rocks of the Vocontian Basin. The sand injection network is composed of dykes, sills and sedimentary laccoliths ranging in thickness from mm to pluri–m. The dykes and sills have vertical and horizontal lengths of up to and over 100 m and 1 km, respectively. Outcrop observations show that the architecture and morphology of the sand injectites in the marls is governed by the local stress field during injection, pre–existing faults, the host–rock lithology, compaction, and distance to the potential sand source(s). The main set of dykes is oriented N50–60° perpendicular to the minimum compressive stress σ3 during sand injection. Two other sets of dykes are intruded along pre–existing syn–sedimentary faults oriented N140–150° (set 2) and N90° (set 3) during the Apto–Cenomanian interval. Sills and dykes thin laterally away from their potential sand sources and thin laterally away from them. The vertical thickness variations of the dykes and wings are more complex, as thinning away from the sand sources is often compensated by thickening toward the palaeo–surface. Based on field observations and measurements, we characterized the 3D architecture of the sand injectites and showed that the injectites probably formed due to a forceful injection from an overpressured sand body sealed by low–permeability lithologies.
ISSN: 0191-8141

hal-01243488
https://hal.archives-ouvertes.fr/hal-01243488
DOI : 10.1016/j.jsg.2015.07.001