Éditeur(s) : HAL CCSD Wiley
Résumé : A standardized rapid inventory method providing information on both tree species diversity and aboveground carbon stocks in tropical forests will be an important tool for evaluating efforts to conserve biodiversity and to estimate the carbon emissions that result from deforestation and degradation (REDD). Herein, we contrast five common plot methods differing in shape, size, and effort requirements to estimate tree diversity and aboveground tree biomass (AGB). We simulated the methods across six Neotropical forest sites that represent a broad gradient in forest structure, tree species richness, and floristic composition, and we assessed the relative performance of methods by evaluating the bias and precision of their estimates of AGB and tree diversity. For a given sample of forest area, a several small' (<1ha) sampling strategy led to a smaller coefficient of variation (CV) in the estimate of AGB than a few large' one. The effort (person-days) required to achieve an accurate AGB estimate (<10% CV), however, was greater for the smallest plots (0.1ha) than for a compromise approach using 0.5ha modified Gentry plots, which proved to be the most efficient method to estimate AGB across all forest types. Gentry plots were also the most efficient at providing accurate estimates of tree diversity (<10% CV of Hill number). We recommend the use of the 0.5ha modified Gentry plot method in future rapid inventories, and we discuss a set of criteria that should inform any choice of inventory method.
ISSN: 0006-3606

hal-01032408
https://hal.archives-ouvertes.fr/hal-01032408
DOI : 10.1111/btp.12006

Éditeur(s) : Agency for International Development, Science and Technology/Forestry and Natural Resources Agency for International Development, Science and Technology/Forestry and Natural Resources ( Washington, DC )
Résumé : (Bibliography) Includes bibliographical references.
(Statement of Responsibility) Joshua C. Dickinson.
Dominican Republic
Dominican Republic
Ecuador
Ecuador
Honduras
Honduras

703868980
2010530282

Éditeur(s) : Tip. de la Escuela de Artes y Oficios Tip. de la Escuela de Artes y Oficios ( Quito )
Résumé : Includes index.
(Statement of Responsibility) expedido por el señor General Don Eloy Alfaro, Encargado del Mando Supremo.
Ecuador
Ecuador

13195349
ocm13195349

Éditeur(s) : Printed for Eliz. Nutt for John Nicholson at the King's Arms in Little Britain ( London )
Résumé : (Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program.
Copper engraving, hand colored.
Relief shown pictorially.
Historical nautical chart from Cape Blanco in Costa Rica along the Pacific coast of South America to Arica in northern Chile.
Title in rectangle box with scale bar.
Includes compass rose oriented with north towards the left and rhumb lines.
Longitude lines not shown on map, geographic coordinates estimated from a modern map of the area.
From: Moll's Atlas geographus, vol. 5, dated 1717. London: printed for Eliz. Nutt.
(Citation/Reference) Other author(s),etc:Moll, Herman 1732 Atlas geographus, or a compleat system of geography

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide.
003879570
http://ufdc.ufl.edu/UF00076809/00001

Éditeur(s) : Unión Panamericana, Departamento de Asuntos Económicos y Sociales Unión Panamericana, Departamento de Asuntos Económicos y Sociales ( Washington, D. C. )
Résumé : (Bibliography) Bibliography: p. 134-137.
Ecuador
El Salvador
Brazil
Latin America
Latin America

AAP8922
01690973
000132888
52061848

Éditeur(s) : Bean/Cowpea CRSP, Michigan State University Bean/Cowpea CRSP, Michigan State University ( East Lansing )
Résumé : (Funding) Funded through USAID/BIFAD Grant No.
(Statement of Responsibility) Donald H. Wallace, Porfirio N. Masaya, Paul A. Gniffke.
"Vanguard (East Lansing, Mich.), Volume 1, no. 1, March 1984."
Guatemala
Ecuador
Guatemala
Ecuador

234307156

Éditeur(s) : Impr. de Hallet & Breen, Impr. de Hallet & Breen Impr. de Hallet & Breen, Impr. de Hallet & Breen ( Nueva York )
Résumé : (Internal Comments) compiladas y publicadas por el sr. dr. d. Jose Antonio Garcia y Garcia.
(Statement of Responsibility) compiladas y publicadas por el sr. dr. d. Jose Antonio Garcia y Garcia.
Preface with caption "El editor" signed: Ignacio Gomez.
Reports from the viceroys and from anonymous sources, 1760-1818.
Colombia
Ecuador
Panama
Venezuela
Colombia
Venezuela
Ecuador
South America
VENEZUELA
COLOMBIA
PANAMA

ADK1934
04675394
000661683
41040469

Éditeur(s) : Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida ( Gainesville Fla )
Résumé : (Dates or Sequential Designation) 1999-
Latest issue consulted: 2002.
Mexico
Costa Rica
El Salvador
Guatemala
Honduras
Nicaragua
Panama
Dominican Republic
Uruguay
Jamaica
Trinidad and Tobago
Bolivia
Colombia
Ecuador
Peru
Venezuela
Brazil
Argentina
Chile
Paraguay
Latin America
Latin America
Latin America

AEW7530
48447906
000990589
2004233277

Éditeur(s) : Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida ( Gainesville Fla )
Résumé : (Dates or Sequential Designation) 1999-
Latest issue consulted: 2002.
Mexico
Costa Rica
El Salvador
Guatemala
Honduras
Nicaragua
Panama
Dominican Republic
Uruguay
Jamaica
Trinidad and Tobago
Bolivia
Colombia
Ecuador
Peru
Venezuela
Brazil
Argentina
Chile
Paraguay
Latin America
Latin America
Latin America

AEW7530
48447906
000990589
2004233277

Éditeur(s) : HAL CCSD Springer-Verlag
Résumé : International audience
With hull-mounted multibeam echosounder data, wereport for the first time along the active Ecuadorian margin,acoustic signatures of water column fluid emissions and seep-relatedstructures on the seafloor. In total 17 flare-shaped acousticanomalies were detected from the upper slope (1250 m) to the shelfbreak (140 m). Nearly half of the flare-shaped acoustic anomaliesrise 200–500 m above the seafloor. The base of the flares is generallyassociated with high-reflectivity backscatter patchescontrasting with the neighboring seafloor. We interpret these flaresas caused by fluid escape in the water column, most likely gases.High-resolution seismic profiles show that most flares occur closeto the surface expression of active faults, deformed areas, slopeinstabilities or diapiric structures. In two areas tectonic deformationdisrupts a Bottom Simulating Reflector (BSR), suggesting thatburied frozen gas hydrates are destabilized, thus supplying free gasemissions and related flares. This discovery is important as it opensthe way to determine the nature and origin of the emitted fluids andtheir potential link with the hydrocarbon system of the forearcbasins along the Ecuadorian margin.
ISSN: 0033-4533

insu-01267238
https://hal-insu.archives-ouvertes.fr/insu-01267238
DOI : 10.1007/s00024-015-1230-7

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le 26 septembre 2007, lors d’un discours à l’Assemblée générale des Nations Unies, Rafael Correa, le président équatorien, critiqua la vision du développement sous-jacente aux Objectifs du Millénaire pour le Développement (OMD). Récusant la stratégie de libéralisation économique et les objectifs d’accroissement de la consommation qu’elle implique, son gouvernement s’est prononcé en faveur d’un « développement endogène, d’inclusion économique et de cohésion sociale et territoriale » afin de diminuer les inégalités pour permettre à tous de mener une vie décente et digne, ajoutant « notre vision du développement est très différente : nous entendons par développement le bien-être de tous, en paix et en harmonie avec la nature, et la prolongation infinie des cultures humaines. »Le tourisme, source majeure de devises étrangères en Équateur à côté du pétrole et des envois d’argent des migrants, peut-il contribuer à l’atteinte de cet objectif ? Comment ? Atteignant plus d’un million de visiteurs étrangers en 2008 (dont 24 % en provenance des États-Unis et 45 % de pays d’Amérique latine, les recettes du tourisme international ont représenté la même année, 754 millions de dollars. Considérant le tourisme comme une activité opportune, de plus en plus de communautés autochtones développent des projets touristiques. En 2009, la fédération plurinationale de tourisme communautaire d’Équateur regroupait 90 communautés membres alors même que toutes celles qui développent des projets de tourisme communautaire n’adhèrent pas à la fédération. Comment comprendre cet engouement pour le tourisme de la part des communautés autochtones ? Quelles sont leurs attentes ? Les projets permettent-ils d’y répondre ? Nous apporterons des éléments de réponse à ces questions à travers l’analyse de deux expériences de tourisme communautaire menées par des communautés quechuas dans les Andes et en Amazonie.
In September 2007, during a speech to the General Assembly of the United Nations, Ecuadorian president Rafael Correa criticized the vision underlying the Millennium Development Goals (MDGs). Rejecting the strategy of economic liberalization and the increased consumption it implies, Correa stated that his government was in favour of "endogenous development, economic inclusion and social and territorial cohesion" to reduce inequalities and permit a decent standard of life for everyone, adding "our vision of development is very different: we believe in developing the welfare of all, in peace and harmony with nature, and the infinite extension of human cultures."Tourism is one of the largest form of foreign exchange in Ecuador beside oil and remittances from migrants. Can tourism contribute to achieving the goal defined by Correa? How? With more than one million foreign visitors in 2008 (including 24% from the United States and 45% from Latin American countries), international tourism contributed $745 millions to Ecuador’s economy in 2008. Acknowledging tourism as a timely activity, more and more indigenous communities are developing tourism projects. The multinational federation of community-based tourism in Ecuador includes 90 communities, even though all those who set up community tourism projects have not adhered to the federation’s requirements. How can we understand this surge in popularity for tourism from indigenous communities and what are their expectations? Do these projects result in adequate solutions? We will provide some answers through the analysis of two experiments conducted on community-based tourism by Kechua communities in the Andes and the Amazon rainforest.
Équateur

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6551
http://journals.openedition.org/etudescaribeennes/6551

Éditeur(s) : Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida Center for Latin American Studies, University of Florida, Center for Latin American Studies, University of Florida ( Gainesville, Fla )
Résumé : (Dates or Sequential Designation) 1999-
Latest issue consulted: 2002.
Mexico
Costa Rica
El Salvador
Guatemala
Honduras
Nicaragua
Panama
Dominican Republic
Uruguay
Jamaica
Trinidad and Tobago
Bolivia
Colombia
Ecuador
Peru
Venezuela
Brazil
Argentina
Chile
Paraguay
Latin America
Latin America
Latin America

AEW7530
48447906
000990589
2004233277

Éditeur(s) : HAL CCSD The Geochemical Society of Japan
Résumé : International audience
The Western Cordillera of Ecuador consists of Cretaceous crustal fragments of oceanic plateaux and superimposed insular arcs, which were accreted to the northwestern South American margin during the Late Cretaceous and Paleocene. Slices of high-grade metabasites, ultramafic rocks, gabbros and basalts, unmetamorphosed radiolarian cherts and scarce garnet-bearing metasediments were randomly exhumed along Miocene to Recent transcurrent faults crosscutting the Western Cordillera. The basalts show geochemical characteristics of oceanic plateau basalts (flat REE patterns, La/Nb = 0.85). The gabbros differ from the basalts in having lower REE levels, positive Eu anomalies, and negative Nb and Ta anomalies; they are interpreted as resulting from arc magmatism. The amphibolites and banded amphibolites have major and trace element chemistry similar to that of oceanic plateau basalts (flat REE patterns, La/Nb = 0.86) or to cumulate gabbros. The granulite shares with oceanic plateaus similar trace element chemistry (flat REE patterns, La/Nb < 1) and εNdi values (+7.6). Continent-derived metasediments are depleted in heavy REE (La/Y = 4.8) and have a negative Eu anomaly. Foliated lherzolites, melagabbronorites and pyroxenites consist of serpentinized olivine + cpx + opx ± Ca-plagioclase. Lherzolites, melagabbronorites and pyroxenites are LREE depleted with positive Eu anomalies, while the harzburgite displays a U-shaped REE pattern. The trace element abundances of the ultramafic rocks are very low (0.1 to 1 times the chondritic and primitive mantle values). The ultramafic rocks represent fragments of depleted mantle, deformed cpx-rich cumulate, and continental lithospheric mantle or mantle contaminated by subduction-fluid. Except the scarce quartz-rich metasediments, all these rocks likely represent remnants of accreted oceanic crustal fragments and associated depleted mantle. Since these samples were randomly sampled at depth by the fault, we propose that the Western Cordillera and its crustal root are mainly of oceanic nature.
ISSN: 0016-7002

insu-00679228
https://hal-insu.archives-ouvertes.fr/insu-00679228

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
The El Oro metamorphic province of SW Ecuador is a composite massif made of juxtaposed terranes of both continental and oceanic affinity that has been located in a fore-arc position since Late Paleozoic times. Various geochemical, geochronological, and metamorphic studies have been undertaken on the El Oro metamorphic province, providing an understanding of the origin and age of the distinct units. However, the internal structures and geodynamic evolution of this area remain poorly understood. Our structural analysis and thermal modeling in the El Oro metamorphic province show that this fore-arc zone underwent four main geological events. (1) During Triassic times (230–225 Ma), the emplacement of the Piedras gabbroic unit at crustal-root level (~9 kbar) triggered partial melting of the metasedimentary sequence under an E-W extensional regime at pressure-temperature conditions ranging from 4.5 to 8.5 kbar and from 650 to 900°C for the migmatitic unit. (2) At 226 Ma, the tectonic underplating of the Arenillas-Panupalí oceanic unit (9 kbar and 300°C) thermally sealed the fore-arc region. (3) Around the Jurassic-Cretaceous boundary, the shift from trench-normal to trench-parallel subduction triggered the exhumation and underplating of the high-pressure, oceanic Raspas Ophiolitic Complex (18 kbar and 600°C) beneath the El Oro Group (130–120 Ma). This was followed by the opening of a NE-SW pull-apart basin, which tilted the massif along an E-W subhorizontal axis (110 Ma). (4) In Late Cretaceous times, an N-S compressional event generated heterogeneous deformation due to the presence of the Cretaceous Celica volcanic arc, which acted as a buttress and predominantly affected the central and eastern part of the massif.
ISSN: 0278-7407

hal-01115714
https://hal.archives-ouvertes.fr/hal-01115714
DOI : 10.1002/2014TC003618

Éditeur(s) : SANREM CRSP SANREM CRSP
Résumé : Description based on: 1995; title from cover.
Costa Rica
Ecuador
Honduras
Burkina Faso
Philippines

104632668

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The eastern part of the Cordillera Occidental of Ecuador comprises thick buoyant oceanic plateaus associated with island-arc tholeiites and subduction-related calc-alkaline series, accreted to the Ecuadorian Continental Margin from Late Cretaceous to Eocene times. One of these plateau sequences, the Guaranda Oceanic Plateau is considered as remnant of the Caribbean–Colombian Oceanic Province (CCOP) accreted to the Ecuadorian Margin in the Maastrichtien. Samples studied in this paper were taken from four cross-sections through two arc-sequences in the northern part of the Cordillera Occidental of Ecuador, dated as (Río Cala) or ascribed to (Macuchi) the Late Cretaceous and one arc-like sequence in the Chogòn-Colonche Cordillera (Las Orquídeas). These three island-arcs can clearly be identified and rest conformably on the CCOP. In all four localities, basalts with abundant large clinopyroxene phenocrysts can be found, mimicking a picritic or ankaramitic facies. This mineralogical particularity, although not uncommon in island arc lavas, hints at a contribution of the CCOP in the genesis of these island arc rocks. The complete petrological and geochemical study of these rocks reveals that some have a primitive island-arc nature (MgO values range from 6 to 11 wt.%). Studied samples display marked Nb, Ta and Ti negative anomalies relative to the adjacent elements in the spidergrams characteristic of subduction-related magmatism. These rocks are LREE-enriched and their clinopyroxenes show a tholeiitic affinity (FeOT–TiO2 enrichment and CaO depletion from core to rim within a single crystal). The four sampled cross-sections through the island-arc sequences display homogeneous initial Nd, and Pb isotope ratios that suggest a unique mantellic source for these rocks resulting from the mixing of three components: an East-Pacific MORB end-member, an enriched pelagic sediment component, and a HIMU component carried by the CCOP. Indeed, the ankaramite and Mg-basalt sequences that form part of the Caribbean-Colombian Oceanic Plateau are radiogenically enriched in 206Pb/204Pb and 207Pb/204Pb and contain a HIMU component similar to that observed in the Gorgona basalts and Galápagos lavas. The subduction zone that generated the Late Cretaceous arcs occurred far from the continental margin, in an oceanic environment. This implies that no terrigenous detrital sediments interacted with the source at this period. Thus, the enriched component can only result from the melting of subducted pelagic sediments. We have thus defined the East-Pacific MORB, enriched (cherts, pelagic sediments) and HIMU components in an attempt to constrain and model the genesis of the studied island-arc magmatism, using a compilation of carefully selected isotopic data from literature according to rock age and paleogeographic location at the time of arc edification. Tripolar mixing models reveal that proportions of 12–15 wt.% of the HIMU component, 7–15 wt.% of the pelagic sediment end-member and 70–75 wt.% of an East-pacific MORB end-member are needed to explain the measured isotope ratios. These surprisingly high proportions of the HIMU/CCOP component could be explained by the young age of the oceanic plateau (5–15 Ma) during the Late Cretaceous arc emplacement. The CCOP, basement of these arc sequences, was probably still hot and easily assimilated at the island-arc lava source.
ISSN: 0895-9811

insu-00353692
https://hal-insu.archives-ouvertes.fr/insu-00353692
DOI : 10.1016/j.jsames.2008.06.003

Éditeur(s) : HAL CCSD
Résumé : International audience
An efficient management of natural hazards cannot be only a hazard assessment and the location of population in danger. It is necessary to take into account an estimation of the human vulnerability, communications, local infrastructure (individual and collective). Research work engaged in Ecuador on the Cotopaxi volcanic region and more recent projects illustrate this taking into account human factors and contribute to a hazard global approach.
La gestión completa de los riesgos naturales debe tener en cuenta la evaluación de probabilidades, la localización de la población, pero también el conjunto de factores humanos de vulnerabilidad. Las investigaciones llevadas a cabo en Ecuador, en la región del volcán Cotopaxi, constituyen un buen ejemplo.
Une gestion efficace des risques naturels ne peut se satisfaire de la seule évaluation des aléas et de la localisation des populations menacées. Elle doit également s'appuyer sur l'appréciation des facteurs humains de vulnérabilité, que ce soit sur le plan individuel ou collectif. Les travaux de recherche engagés en Equateur dans les régions exposées au volcan Cotopaxi el d'autres projets plus récents vont dans cette voie et concourent à une approche globale des risques. Leur caractère opérationnel ne peut que contribuer â la mitigation des effets des catastrophes naturelles.
Pangea

hal-01168555
https://hal.archives-ouvertes.fr/hal-01168555
https://hal.archives-ouvertes.fr/hal-01168555/document
https://hal.archives-ouvertes.fr/hal-01168555/file/D%27Ercole%201993%20Pangea%20Gestion%20risques%20r%C3%A9alit%C3%A9s%20sociales.pdf

Éditeur(s) : A. Combette ( Paris )
Résumé : From: Atlas Universel Illustre.
Extensive illustrations surround the smaller map. A colorful framework of landscape, animals, people, with steel gengravings of cities.
Engraved by Laguillermie.
Illustrations by Raimond Bonheur.
(Funding) Funded in part by the University of Florida, the Florida Heritage Project of the State University Libraries of Florida, the Institute for Museum and Library Services, and the U.S. Department of Education's TICFIA granting program.
Mexico
Belize
Guatemala
Honduras
El Salvador
Costa Rica
Nicaragua
Panama
Cuba
Cayman Islands
Jamaica
Haiti
Dominican Republic
Puerto Rico
United States Virgin Islands
British Virgin Islands
Anguilla
Antigua and Barbuda
Guadeloupe
Dominica
Montserrat
Martinique
Saint Kitts and Nevis
Saint Lucia
Saint Vincent and the Grenadines
Barbados
Grenada
Trinidad and Tobago
Netherlands Antilles
Aruba
Colombia
Venezuela
Guyana
French Guiana
Suriname
Argentina
Chile
Brazil
Uruguay
Paraguay
Ecuador
Peru
Falkland Islands
South America
South America
Early Maps
South America

Droits : This item is presumed to be in the public domain. The University of Florida George A. Smathers Libraries respect the intellectual property rights of others and do not claim any copyright interest in this item. Users of this work have responsibility for determining copyright status prior to reusing, publishing or reproducing this item for purposes other than what is allowed by fair use or other copyright exemptions. Any reuse of this item in excess of fair use or other copyright exemptions may require permission of the copyright holder. The Smathers Libraries would like to learn more about this item and invite individuals or organizations to contact Digital Services (UFDC@uflib.ufl.edu) with any additional information they can provide.
002730767
ANK8537
http://ufdc.ufl.edu/UF90000235/00001

Éditeur(s) : Department of State Department of State
Résumé : (Acquisition) Collected for University of Florida's Institutional Repository by the UFIR Self-Submittal tool. Submitted by Margarita Vargas-Betancourt.
(Publication Status) Unpublished
In July 2012, Elenita M. Tapawan, who was then Information Resource Officer, at the Embassy of the U.S. in Mexico invited me to participate as an international speaker for State Department library partners in Latin America. As stated above, on October 24 and November 20, 2012, Natalie Baur (University of Miami) and I presented two webinars on the tools used to develop special collections. There were 273 participants from eight different countries (Peru, Paraguay, Ecuador, Colombia, Honduras, El Salvador, Guatemala, Chile, and Venezuela).

Droits : All rights reserved by the submitter.
http://ufdc.ufl.edu/IR00001560/00001

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
At the North-Ecuadorian convergent margin (1°S–1.5°N), the subduction of the rough Nazca oceanic plate leads to tectonic erosion of the upper plate and complex seismogenic behavior of the megathrust. We used three selected pre-stack depth migrated, multi-channel seismic reflection lines collected during the SISTEUR cruise to investigate the margin structure and decipher the impact of the subducted Atacames seamounts on tectonic erosion, interseismic coupling, and seismogenesis in the region of the 1942 Mw7.8 earthquake.This dataset highlights a subducted ∼30×40 km∼30×40 km, double-peak seamount that belongs to the Atacames seamount chain and that is associated with a deep morphologic re-entrant containing mass transport deposits.The seamount subduction uplifted the margin basement by ∼1.6 km and pervasively broke the margin by deep and intense reverse faulting ahead of the seamount, a process that is likely to weaken considerably the margin. In the seamount wake, the basement reverse fault system rotated counter-clockwise. This faulted basement is overlain with slope sediment sliding along listric normal faults that sole out onto the BSR. This superposition of deep tectonic contraction within the basement and shallow gravitational extension deformation within the sediment highlights the key role of gas hydrate on outer slope erosion.In addition to long-term regional basal erosion, the margin basement has thinned locally by an extra 0.8–1 km in response to the subduction of the Atacames seamount chain and hydrofracturing by overpressured fluids at the margin toe. This pervasively and deeply fractured margin segment is associated with a seismically quiet and GPS-modeled low interseismic coupling corridor that terminates downdip near the 1942 epicenter and locked zone. We suggest that the deeply buried double-peak Atacames seamount triggered the 1942 earthquake ahead of its leading flank. This result supports previous studies proposing that subducted seamounts provide unfavorable conditions for locking the updip segment of the plate boundary limiting the updip extent of seismogenic zones, but may favor large subduction earthquakes at greater depths.
ISSN: 0012-821X

hal-01256399
https://hal.archives-ouvertes.fr/hal-01256399
DOI : 10.1016/j.epsl.2015.10.043