Extrait de : Histoire des plantes de la Guiane Françoise, rangées suivant la méthode sexuelle, avec plusieurs mémoires sur différens objets intéreffans, relatifs à la culture & au commerce de la Guiane Françoife, & une notice des plantes de l'Ifle-de-France, Tome Quatrième (Planche 317)
Siècle(s) traité(s) : 18
Droits : Domaine public
Permalien : http://www.manioc.org/images/FRA110570257i1
FRA110570257i1

Extrait de : Une excursion aux climats tropicaux : voyages aux îles-du-vent St-Kitts, Nevis, Antigue, Monserrat, La Dominique, La Guadeloupe, Ste-Lucie, La Barbade, Trinidad (p. 110)
Résumé : Gravure représentant un corail, Madrepora aspera, Dana
Siècle(s) traité(s) : 19
Droits : Domaine public
Provenance : Université des Antilles et de la Guyane. Service commun de la documentation
Permalien : http://www.manioc.org/images/HASHc49b6127a96579172f1293
HASHc49b6127a96579172f1293

Extrait de : Histoire des plantes de la Guiane Françoise, rangées suivant la méthode sexuelle, avec plusieurs mémoires sur différens objets intéreffans, relatifs à la culture & au commerce de la Guiane Françoife, & une notice des plantes de l'Ifle-de-France, Tome Troisième (Planche 22)
Siècle(s) traité(s) : 18
Droits : Domaine public
Permalien : http://www.manioc.org/images/FRA110560053i1
FRA110560053i1

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
The majority of the largest subduction megathrust earthquakes share the common characteristic of rupturing more than one asperity along strike of the margin. Understanding the factors that control coseismic failure of multiple asperities, and thus maximum magnitude, is central for seismic hazard assessment. To investigate the role of asperities size and spacing on maximum magnitude, seismicity rate, and percentage of synchronized ruptures, we use analog models simulating along-strike rupture behavior of megathrust earthquakes. We found negative correlations between the barrier-to-asperity length ratio Db/Da and maximum magnitude and seismicity rate. Db/Da also controls the process of asperities synchronization along the megathrust. A permanent barrier behavior is observed for Db/Da > 0.5. Comparing our experimental results to the Nankai Trough historical seismicity, we propose that the distribution of megathrust frictional heterogeneities likely explains the diversity of earthquakes which occurred there.
ISSN: 0094-8276

hal-01685546
https://hal.archives-ouvertes.fr/hal-01685546
https://hal.archives-ouvertes.fr/hal-01685546/document
https://hal.archives-ouvertes.fr/hal-01685546/file/Corbi_et_al-2017-Geophysical_Research_Letters.pdf
DOI : 10.1002/2017GL074182

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We use a strike-slip fault analog model to study experimentally the role played by along-fault non-uniform and asymmetric applied normal stress on both coseismic slip and long-term fault behavior. Our model is based on a visco-elasto-plastic multi-layered rheology that allows to produce several hundreds of scaled analog microquakes and associated seismic cycles. Uniform or heterogeneous applied normal stress along the fault plane is imposed and maintained constant during the whole experiment durations. Our results suggest that coseismic slip patterns are strongly controlled by spatial normal stress variations and subsequent accumulated shear stress along fault strike. Major microquakes occur preferentially in zones of major shear stress asperities. Coseismic slip distributions exhibit a pattern similar to the along-fault applied normal stress distribution. The occurrence of isolated low to moderate microquakes where residual stresses persist around secondary stress asperities, indicates that stress conditions along the fault also control the whole variability of fault slip events. Moreover, when fault slip stability conditions are modulated by normal stress distribution, our experiments suggest that the along-fault stress heterogeneity influences the seismic cycle regularity and, consequently, long-term fault slip behavior. Uniform applied normal stress favors irregular seismic cycles and the occurrence of earthquakes clustering, whereas non-uniform normal stress with a single high amplitude stress asperity generates strong characteristic microquake events with stable return periods. Together our results strengthen the assumption that coseismic slip distribution and earthquake variability along an active fault may provide relevant information on long term tectonic stress and could thus improve seismic hazard assessment.
ISSN: 0012-821X

hal-01666379
https://hal.archives-ouvertes.fr/hal-01666379
DOI : 10.1016/j.epsl.2017.10.009

Extrait de : Histoire des plantes de la Guiane Françoise, rangées suivant la méthode sexuelle, avec plusieurs mémoires sur différens objets intéreffans, relatifs à la culture & au commerce de la Guiane Françoife, & une notice des plantes de l'Ifle-de-France, Tome Quatrième (Planche 350)
Siècle(s) traité(s) : 18
Droits : Domaine public
Permalien : http://www.manioc.org/images/FRA110570323i1
FRA110570323i1

Résumé : Arbol de hasta 30 m, corteza fisurada con látex blanco lechoso. Hojas oblanceoladas, ápice comúnmente agudo, base aguda o atenuada, ferruginosas, finamente reticuladas. Flores en pequeños fascículos axilares, muy perfumadas, actinomorfas. Fruto elipsoide, ovoide o subgloboso de hasta 20 cm, áspero, escamoso, café; pulpa roja; semillas 1 a 2, grandes, negras y lustrosas.
Arbre pouvant atteindre 30 m, écorce fissurée avec latex blanc laiteux. Feuilles oblancéolées, pointe habituellement aiguë, base aiguë ou atténuée, ferrugineuses, finement réticulées. Fleurs en petits fascicules axillaires, très parfumées, actinomorphes. Fruit ellipsoïdal, ovoïde ou subarrondi pouvant atteindre 20 cm, âpre, écailleux, couleur café; pulpe rouge; 1 à 2 graines, grandes, noires et brillantes.
Tree, up to 30 m high, bark fissured, with milky white latex.  Leaves, simple, alternate, blades oblanceolate, 10-60 x 4.5-5 cm, apex acuminate, base cuneate, glabrous above, pubescent beneath; inflorescence in clusters at defoliated nodes or cauliflorus; flowers white with corolla 9-10 mm long; fruit ellipsoid, ovoid or subglobose 8-20 cm long, brown, rough; seeds solitary, broadly obovate, deep brown to black and shiny.
Nativa de México y Centroamérica, cultivada en otras regiones tropicales del continente americano.
Originaire du Mexique et d’;Amérique Centrale, cultivée dans d’;autres régions tropicales du continent américain.
Native to Mexico and Ce

http://www.tramil.net/fototeca/plant260

Résumé : Hierba anual de hasta 2 m de altura. Tallo áspero o rugoso. Hojas anchamente ovadas o suborbiculares de 3 a 5 lóbulos, con la base más o menos cordada, de 8 a 18 cm de largo y dentadas. Cabezuelas masculinas en el ápice de las ramas y en las axilas de las hojas; cabezuelas femeninas una o pocas en la base de las inflorescencias, con brácteas ganchudas. Fruto capsular, ovoide y espinoso; espinas rectas y ganchudas en el ápice.
Herbe annuelle pouvant atteindre 2 m de haut. Tige âpre ou rugueuse. Feuilles largement ovées ou suborbiculaires de 3 à 5 lobes, à base plus ou moins cordée, de 8 à 18 cm de long, dentées. Capitules mâles à la pointe des branches et à l’axe des feuilles; capitules femelles au nombre de 1 (ou un peu plus) à la base des inflorescences, avec bractées en forme de crochets. Fruit à capsule, ovoïde et épineux; épines droites et crochues à la pointe.
Annual monoecious herb 70 cm high. Leaves alternate, 7-12 cm long including petiole, base cordate or reniform, apex acute, 3-5 lobed and dentate, blades, scabrous, with appressed golden glandular hairs, triangular- orbicular 7-12 x 6-12 cm;  inflorescence racemose; male heads globose, numerous florets, female head burrlike with hooked bracts, 2 flowers; Achene, 0.9-1.5cm linear, compressed, beaked, smooth.
Cosmopolita.
Cosmopolite.
Cosmopolitan.

http://www.tramil.net/fototeca/plant361

Éditeur(s) : Société des Sciences Naturelles de la Charente-Maritime
Résumé : The authors give data on the catches during 1991 of some rare fishes to the French harbours : some fishes are recorded for the first time: Dibranchus atlanticus from the North-eastern Atlantic, Paralepis atlantica and Seriola rivoliana from the Baya of Biscay, Lepidocybium flavobrunneum from the statistical ICES Division 8 E. With the growth of the net-fishing for tunna, some pelagic rare species (Taractes asper; Luvarus imperialis, Istiophorid fishes are caught. Tetragonurus cuvieri is recorded for the second time from the Bay of Biscay. NOT CONTROLLED OCR
En 1991, les auteurs ont observé des poissons rares dans les ports français de l'Atlantique. Certains sont signalés pour la première fois dans les zones de capture concernées: Dibranchus atlanticus dans l'Atlantique nord-est, Paralepis atlantica et Seriola rivoliana dans le golfe de Gascogne, Lepidocybium flavobrunneum dans la zone CIEM Large Gascogne. Avec le développement de la pêche au thon au filet, des espèces pélagiques rares (Taractes asper; Luvarus imperialis, des lstiophoridés) ont été également observées. Tetragonurus cuvieri est signalé pour la seconde fois dans le golfe de Gascogne. OCR NON CONTROLE
Annales de la Société des Sciences Naturelles de la Charente-Maritime (Société des Sciences Naturelles de la Charente-Maritime), 1992 , Vol. 8 , N. 1 , P. 51-57

Droits : 1992 Société des Sciences Naturelles de la Charente-Maritime
http://archimer.ifremer.fr/doc/1992/publication-3683.pdf
http://archimer.ifremer.fr/doc/00000/3683/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
To improve earthquake location, we create a 3-D a priori P-wave velocity model (3-DVM) that approximates the large velocity variations of the Ecuadorian subduction system. The 3-DVM is constructed from the integration of geophysical and geological data that depend on the structural geometry and velocity properties of the crust and the upper mantle. In addition, specific station selection is carried out to compensate for the high station density on the Andean Chain. 3-D synthetic experiments are then designed to evaluate the network capacity to recover the event position using only P arrivals and the MAXI technique. Three synthetic earthquake location experiments are proposed: (1) noise-free and (2) noisy arrivals used in the 3-DVM, and (3) noise-free arrivals used in a 1-DVM. Synthetic results indicate that, under the best conditions (exact arrival data set and 3-DVM), the spatiotemporal configuration of the Ecuadorian network can accurately locate 70 per cent of events in the frontal part of the subduction zone (average azimuthal gap is 289° ± 44°). Noisy P arrivals (up to ± 0.3 s) can accurately located 50 per cent of earthquakes. Processing earthquake location within a 1-DVM almost never allows accurate hypocentre position for offshore earthquakes (15 per cent), which highlights the role of using a 3-DVM in subduction zone. For the application to real data, the seismicity distribution from the 3-D-MAXI catalogue is also compared to the determinations obtained in a 1-D-layered VM. In addition to good-quality location uncertainties, the clustering and the depth distribution confirm the 3-D-MAXI catalogue reliability. The pattern of the seismicity distribution (a 13 yr record during the inter-seismic period of the seismic cycle) is compared to the pattern of rupture zone and asperity of the Mw = 7.9 1942 and the Mw = 7.7 1958 events (the Mw = 8.8 1906 asperity patch is not defined). We observe that the nucleation of 1942, 1958 and 1906 events coincides with areas of positive Simple Bouguer anomalies and areas where marine terraces are still preserved on the coastal morphology. From north to south: (1) the 1958 rupture zone is almost aseismic and is attributed to a zone of high coupling; (2) south of the Galera alignment (perpendicular to the trench), the 1942 rupture zone presents moderate seismicity, deeper on the seismogenic interplate zone, and abutting on the Jama cluster (to the south). This cluster is facing the Cabo Pasado cap and positive Bouguer anomalies on the overriding margin. We suspect that this cluster reflects a zone of local asperity (partial coupling). South of the Jama cluster, the spherical aseismic zone in the Bahia area is interpreted as having a low seismic coupling (steady creep motion or slow slip events). We suspect that the site that generated the three M > 7 events (1896, 1956 and 1998) correspond to a small patch of strong coupling. To the south, in the Manta-Puerto Lopez zone, the seismicity is mainly organized in earthquake swarms (1998, 2002, 2005). Although slow slip events have been observed in the area (Vallée et al. submitted), we infer from the coastline shape, the marine terraces and the high positive Bouguer anomalies that the seismicity here might reveal a significant amount of seismic coupling.
ISSN: 0956-540X

hal-00873478
https://hal.archives-ouvertes.fr/hal-00873478
DOI : 10.1093/gji/ggs083

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
Fluid-rock interactions can control earthquake nucleation and the evolution of earthquake sequences. Experimental studies of fault frictional properties in the presence of fluid can provide unique insights into these interactions. We report the first results from experiments performed on cohesive silicate-bearing rocks (microgabbro) in the presence of pressurized pore fluids (H2O, drained conditions) at realistic seismic deformation conditions. The experimental data are compared with those recently obtained from carbonate-bearing rocks (Carrara marble). Contrary to theoretical arguments, and consistent with the interpretation of some field observations, we show that frictional melting of a microgabbro develops in the presence of water. In microgabbro, the initial weakening mechanism (flash melting of the asperities) is delayed in the presence of water; conversely, in calcite marble the weakening mechanism (brittle failure of the asperities) is favored. This opposite behavior highlights the importance of host-rock composition in controlling dynamic (frictional) weakening in the presence of water: cohesive carbonate-bearing rocks are more prone to slip in the presence of water, whereas the presence of water might delay or inhibit the rupture nucleation and propagation in cohesive silicate-bearing rocks.
ISSN: 0091-7613

hal-01054327
https://hal.archives-ouvertes.fr/hal-01054327
DOI : 10.1130/G34916.1

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
Detailed seafloor mapping in the area east of Taiwan revealed trench-parallel stretching and folding of the Ryukyu forearc and lateral motion of the accretionary wedge under oblique convergence. East of 122ø40'E, a steep accretionary wedge is elongated in an E-W direction. A major transcurrent right-lateral strike-slip fault accommodates the strain partitioning caused by an oblique convergence of 40 ø. A spectacular out-of-sequence thrust may be related to the subduction of a structural high lying in the axis of the N-S trending Gagua Ridge. This asperity is likely responsible for the uplift of the accretionary wedge and forearc basement and may have augmented strain partitioning by increasing the coupling between the two plates. West of 122ø40'E, the low-taper accretionary wedge is sheared in a direction subparallel to the convergence vector with respect to the Ryukyu Arc. The bayonet shape of the southern Ryukyu Arc slope partly results from the recent (re)opening of the southern Okinawa Trough at a rate of about 2 to 4 cm/yr. Right-lateral shearing of the sedimentary forearc with respect to the nonlinear Ryukyu backstop generates trench-parallel extension in the forearc sediment sequence at dilational jogs and trench-parallel folding at compressive jogs. The Hoping Basin lies above a diffuse trench/trench/fault (TTF) or TFF unstable triple junction moving toward the south along a N-S transform zone which accommodates the southward drift of the Ryukyu Arc with respect to Eurasia.
ISSN: 0278-7407

hal-01261555
https://hal.archives-ouvertes.fr/hal-01261555
https://hal.archives-ouvertes.fr/hal-01261555/document
https://hal.archives-ouvertes.fr/hal-01261555/file/Lallemand_et_al-1999-Tectonics.pdf
DOI : 10.1029/1998TC900011

Éditeur(s) : HAL CCSD American Association for the Advancement of Science
Résumé : International audience
Large earthquakes produce crustal deformation that can be quantified by geodetic measurements, allowing for the determination of the slip distribution on the fault. We used data from Global Positioning System (GPS) networks in Central Chile to infer the static deformation and the kinematics of the 2010 moment magnitude (M-w) 8.8 Maule megathrust earthquake. From elastic modeling, we found a total rupture length of similar to 500 kilometers where slip (up to 15 meters) concentrated on two main asperities situated on both sides of the epicenter. We found that rupture reached shallow depths, probably extending up to the trench. Resolvable afterslip occurred in regions of low coseismic slip. The low-frequency hypocenter is relocated 40 kilometers southwest of initial estimates. Rupture propagated bilaterally at about 3.1 kilometers per second, with possible but not fully resolved velocity variations.
ISSN: 0036-8075

hal-00783213
https://hal.archives-ouvertes.fr/hal-00783213
DOI : 10.1126/science.1204132