Los datos constarían de 24 directorios, uno para cada terremoto con los datos brutos, procesados, y resultados. Se pueden comprimir/empaquetar en un archivo tar. El contenido se describe en el archivo README., Data files and modelling results of regional centroid moment tensors obtained for earthquakes in the 2016 South Alboran seismic crisis, and presented in the article "Earthquake crisis unveils the growth of an incipient continental fault system", by Eulàlia Gràcia et al. Large continental faults extend for thousands of kilometres to form boundaries between rigid tectonic blocks. These faults are often associated with prominent topographic features, and they can produce large earthquakes. Here we present first evidence of such a major tectonic structure in its initial growing stage, the Al-Idrissi Fault System (AIFS), in the Alboran Sea. Until now, this fault system had always been described as a complex diffuse boundary between Eurasia and Nubia plates. However, combining newly acquired high-resolution bathymetric and seismic reflection data, together with seismological analyses of the 2016 Mw 6.4 earthquake offshore Morocco – the largest event ever recorded in the area – we unveil a 3D geometry for the AIFS, which definitively correspond to a crustal-scale boundary. We report evidence of left-lateral strike-slip displacement, characterize fault segmentation and demonstrate that the AIFS is the source of the 2016 events. The occurrence of the Mw 6.4 earthquake together with historical and instrumental events supports that the AIFS is currently growing through propagation and linkage of its segments. Thus, the AIFS provides a unique model for inception and growth of a young continental fault system., MINECO CGL2011-30005-C02-02, CTM2015-70155-R and Acción IDRISSI (MINECO/FEDER), The structure of the dataset is indicated in README.txt, Peer reviewed

The Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only., Disclaimer: The EMSS21 is open to later additions and improvements. For these reasons and due to its intrinsic nature, the EMSS21 cannot be guaranteed to be complete, accurate and updated in any part, and will be subjected to successive revisions. Although the Institut de Ciències del Mar of CSIC makes every effort to supply the best available information, no warranty, expressed or implied, is provided as to the accuracy and reliability of all the data supplied in the EMSS21. Users are cautioned to consider carefully the nature of the data and information before using it for decisions that concern personal or public safety. Conclusions drawn from the EMSS21, or actions undertaken on the basis of its contents, are the sole responsibility of the user., The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as these events are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard.

The EMSS21 displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only., Data compilation has been possible thanks to projects: Submarine landslides and Their impact on European continental margins (SLATE) - H2020-MSCA-ITN-2016-721403. ImagiNg large SeismogenIc and tsunamiGenic structures of the Gulf of Cadiz with ultra-High resolution Technologies (INSIGHT). - CTM2015-70155-R., With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), The Euro-Mediterranean Submarine landSlide database (EMSS21) is a catalogue of submarine landslides of the Mediterranean Sea and the European continental margins of the Atlantic and Arctic Oceans. The catalogue is compiled from data available in the literature as well as information collected from geophysical data and not published in the scientific literature. The data set includes polygons and polylines for the landslide deposits and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, geological setting, depth, slope, inferred trigger mechanism, relationship to fluid flow features as well as the relevant metadata. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age, particularly for the smaller events, as theseevents are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard., Peer reviewed

Description of methods used for collection/generation of data: The EMSS21 displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.-- Data Quality Assurance: The EMSS25 Data quality control is carried out according to the standards and flow chart established by the EPOS Tsunami Thematic Core Services and based on the principles expressed by the EPOS Data Policy. These can be consulted here: https://www.tsunamidata.org/organization/data-quality-assurance.-- Disclaimer: The EMSS25 is open to later additions and improvements. For these reasons and due to its intrinsic nature, the EMSS25 cannot be guaranteed to be complete, accurate and updated in any part, and will be subjected to successive revisions. Although the Institut de Ciències del Mar of CSIC makes every effort to supply the best available information, no warranty, expressed or implied, is provided as to the accuracy and reliability of all the data supplied in the EMSS25. Users are cautioned to consider carefully the nature of the data and information before using it for decisions that concern personal or public safety. Conclusions drawn from the EMSS25, or actions undertaken on the basis of its contents, are the sole responsibility of the user, The Euro-Mediterranean Submarine landSlide database (EMSS25) is a catalogue of several morphological and sedimentary features of submarine landslides of the Mediterranean Sea and the Atlantic and Arctic continental margins of Europe. It also contains limited information from other areas of the world oceans. The catalogue is compiled from results in the scientific literature as well as information collected from geophysical data and not published yet. The data set includes polygons and polylines for the landslide deposits, landslide source areas and landslide scars as well as information relative to age, volume, area, runout, thickness, typology, scar elevation, depth, slope as well as relevant metadata. Deposits, sources and scars are linked/related by the MatchingID field. The catalogue includes submarine landslides that span the Miocene to Present day. Nevertheless a clear bias exist towards submarine landslides of younger age and large size. Smaller events, particularly older than Holocene events, are difficult to map/identify on lower resolution geophysical data sets typically collected in deep-water and large sub-surface depths and are likely underrepresented in the database. The catalogue aims to offer improved understanding of mass-wasting processes, the potentially resulting tsunamis and derived geohazard, Geosphere INfrastructures for QUestions into Integrated REsearch (Geo-INQUIRE) - HORIZON-INFRA-2021-SERV-01-101058518; Korea Institute of Geosciences and Mineral Resources (KIGAM); MArine Geo-hazards InduCed by underwater LANDslides in the SW Iberian Margin (MAGICLAND) - PTDC/CTA-GEO/30381/2017 Fundação para a Ciência e a Tecnologia (Portugal); Submarine landslides and Their impact on European continental margins (SLATE) - H2020-MSCA-ITN-2016-721403 European Commission; ImagiNg large SeismogenIc and tsunamiGenic structures of the Gulf of Cadiz with ultra-High resolution Technologies (INSIGHT) - CTM2015-70155-R Ministerio de Economía y Competitividad (España), With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), 1. Number of variables: 104; 2. Number of cases/rows: 16091; 3. Variable List: Scar {Id, MatchingID, Name, Latitude, Longitude, MinDepth, MaxDepth, SlopeHeadS, SlHeScMeta, MaxScarHt, MeanScarHt, ScarHtMeta, EvacHeight, EvacHtMeta, Source1, Source2, Source3, Source4, HoriResol, VertiResol, PubSource1, PubSource2, PubSource3, PubSource4, Notes, Operator}; Source area {Id, MatchingID, Name, Longitude, Latitude, MinDepth, MaxDepth, Min_Slope, Max_Slope, Avg_Slope, SlopeMeta, LengthSh2D, LengthMeta, SourceWidt, WidthMeta, MaxScarHt, MeanScarHt, ScarHtMeta, SourceArea, SourceVolu, VolumMeta, Burial_m, Burial_T, BurialMeta, SedRate, SedRateSTD, SedRateMet, Age_BP, AgeMeta, AgeError, AgErMet, AgePeriod, Source1, Source2, Source3, Source4, HoriResol, VertiResol, PubSource1, PubSource2, PubSource3, PubSource4, Notes, Operator}; Deposits {Id, MatchingID, Name, Typology, Longitude, Latitude, MinDepth, MaxDepth, Min_Slope, Max_Slope, Avg_Slope, SlopeMeta, SlopeToe, SlopeToeMe, LengthSh2D, LengthMeta, AvgWidth_m, MaxWidth, WidthMeta, MaxThick_m, MeanThik_m, MaxThick_T, MeanThik_T, Thick_meta, Area_km2, Volume_km3, VolumeMeta, Burial_m, Burial_T, BurialMeta, SedRate, SedRateSTD, SedRateMet, Age_BP, AgeMeta, AgeError, AgErMet, AgePeriod, Source1, Source2, Source3, Source4, HoriResolu, VertiResol, PubSource1, PubSource2, PubSource3, PubSource4, Notes, Operator}, Peer reviewed

Supplementary material for "Complex architecture of mud volcano systems: new insights on flow pathways unravel intricate fluid circulation" https://doi.org/10.1130/B37954.1, Shuhui Xu is supported by the China Scholarship Council (CSC), and Walter Menapace is supported by the H2020 MSCA-IF-TURBOMUD project (grant 101018321). This research was funded in part by the Austrian Science Fund (FWF; grant M 3146-417 N) and projects CTM2015-70155-R (INSIGHT) and PID2020-114856RB-100 (ICEFLAME) funded by the Spanish Ministry of Science and Innovation (MCIN/ AEI/10.13039/501100011033). The European project EUMarineRobots (EUMR) is acknowledged for cofunding the M167 expedition (grant 731103), With the institutional support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), Peer reviewed