ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Collection
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    Displacement time series from GNSS stations in the South-Easten Alps (2020)
    PANGAEA
    Details
    Publication Date: 2023-01-30
    Description: ASCII files reporting the position time-series, in the Adria-fixed reference frame, of GNSS in the Eastern-Southern Alps The columns are: Time, E, N, Se, Sn, Ren, U, Su, Reu, Rnu, site, long, lati, representing, respectively, epoch (in decimal years), displacement in the East component (in mm), displacement in the North component (in mm), uncertainty (one standard deviation) of the East component (in mm), uncertainty (one standard deviation) of the North component (in mm), correlation between the East and North components, displacement in the Up component (in mm), uncertainty (one standard deviation) of the Up component (in mm), correlation between the East and Up components, correlation between the North and Up components, Station ID (four letters), Longitude of the station (°), Latitude of the station (°).
    Keywords: Alps; displacements; GNSS; GPS; time-series
    Type: Dataset
    Format: application/zip, 12.1 MBytes
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 2
    facet.materialart.
    Unknown
    Geopositioning time series from offshore platforms in the Adriatic Sea (2020)
    PANGAEA
    Details
    Publication Date: 2023-11-11
    Description: We provide a dataset of 3D coordinate time series of 37 continuous GNSS stations installed on onshore and offshore industrial settlements along a NW-SE-oriented and ~100-km-wide belt encompassing the eastern Italian coastal area and the Adriatic Sea. The dataset results from the analysis performed by using different geodetic software (Bernese, GAMIT/GLOBK and GIPSY) and is constituted by 6 raw position time series solutions (in ASCII pos format), referred to IGb08 and ITRF2014 reference frames.
    Keywords: Adriatic Sea; GNSS data; GPS; Italy; off-shore hydrocarbon platform
    Type: Dataset
    Format: application/zip, 105.9 MBytes
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 3
    facet.materialart.
    Unknown
    Vertical displacement time series from GNSS stations in the Po river basin area (2023)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Description: ASCII files reporting the daily GNSS vertical ground displacement time series, in the Eurasia-fixed reference frame, from January 2010 to September 2022 of continuous stations located in the Po river basin. The time series are obtained by analyzing the raw GPS observations using the GAMIT/GLOBK (version 10.71) software, following the standard procedures of the repro2 IGS reprocessing scheme (http://acc.igs.org/reprocess2.html). This is part of a large processing effort, including〉4000 stations in the Euro- Mediterranean and African regions (Serpelloni et al., 2022), where sub-networks, made up of 〈50 stations dynamically and optimally selected based on daily data availability, are processed independently with GAMIT and later tied together using common sub-net tie sites and IGb14 core stations using the GLOBK software. This time series are used to study the effect of the drought occurring since 2021 in Northern Italy. The columns of the files are: Time, U, Su, site, long, lati, representing, respectively, epoch (in decimal years), displacement in the Up component (in mm), uncertainty (one standard deviation) of the Up component (in mm), Station ID, Longitude of the station (°), Latitude of the station (°).
    Keywords: ACCE_GPS; AGNE_GPS; ALE9_GPS; ALIN_GPS; ALSN_GPS; AO01_GPS; AOST_GPS; AQNC_GPS; ARGN_GPS; ASOL_GPS; ASTI_GPS; BDZZ_GPS; BERG_GPS; BIEL_GPS; BIEN_GPS; BOBB_GPS; BOR__GPS; BORM_GPS; BRDI_GPS; BREA_GPS; BREN_GPS; BREU_GPS; BRIX_GPS; BUSL_GPS; CAMN_GPS; CANL_GPS; CARP_GPS; CARZ_GPS; CAST_GPS; CATU_GPS; CAVO_GPS; CDVL_GPS; CEL1_GPS; CHA9_GPS; CHIA_GPS; CHRI_GPS; CIMO_GPS; CNC5_GPS; CNV2_GPS; COCL_GPS; CODI_GPS; COLI_GPS; COLL_GPS; COMO_GPS; CONC_GPS; COPX_GPS; CRE1_GPS; CREA_GPS; CREM_GPS; CRSN_GPS; CSLD_GPS; CUNE_GPS; CUOR_GPS; CURN_GPS; CVNE_GPS; DALM_GPS; DARF_GPS; DATE/TIME; DEMA_GPS; DEMN_GPS; DESE_GPS; DEVE_GPS; displacements; DOMS_GPS; Event label; FE01_GPS; FERA_GPS; FERR_GPS; FOS2_GPS; FRUG_GPS; GAVI_GPS; GAZZ_GPS; GNSS; GNSS data; GNSS Receiver; GOZZ_GPS; GPS; GRAV_GPS; GRN1_GPS; GSTN_GPS; GUAS_GPS; IENG_GPS; LATITUDE; LDNS_GPS; LEC1_GPS; LECC_GPS; LGNN_GPS; LOD0_GPS; LOD2_GPS; LODI_GPS; LOMO_GPS; LONGITUDE; LUI9_GPS; LUIN_GPS; LVFR_GPS; MAGA_GPS; MAN3_GPS; MAN9_GPS; MANT_GPS; MARX_GPS; MCAR_GPS; MENA_GPS; MIL2_GPS; MLNO_GPS; MO01_GPS; MO02_GPS; MO03_GPS; MO05_GPS; MODE_GPS; MOGE_GPS; MON8_GPS; MONC_GPS; MOND_GPS; MONF_GPS; MONV_GPS; MONZ_GPS; MOPS_GPS; MORB_GPS; MRGE_GPS; NERO_GPS; NOVA_GPS; NOVR_GPS; NVR2_GPS; NVRA_GPS; OATO_GPS; ORZI_GPS; OSTA_GPS; PALA_GPS; PAMX_GPS; PARM_GPS; PARO_GPS; PAV2_GPS; PAVA_GPS; PAVI_GPS; PERS_GPS; PIA1_GPS; PIAC_GPS; PINE_GPS; PORA_GPS; PR01_GPS; PREM_GPS; PRSE_GPS; PRST_GPS; PTO1_GPS; PTOL_GPS; PVIA_GPS; PVLM_GPS; QUI__GPS; RAMS_GPS; RE01_GPS; REGG_GPS; RONC_GPS; RSPX_GPS; RUMI_GPS; SAV2_GPS; SAVI_GPS; SBPO_GPS; SERR_GPS; SEVI_GPS; SGIP_GPS; SIR2_GPS; SMAR_GPS; SOND_GPS; SONP_GPS; STUE_GPS; SUSA_GPS; TARO_GPS; Text file; Text file (File Size); time-series; TNUS_GPS; TOGR_GPS; TORC_GPS; TORI_GPS; TRNO_GPS; TRTN_GPS; TRVG_GPS; UNF0_GPS; UNFE_GPS; VARE_GPS; VARZ_GPS; VEBG_GPS; VERB_GPS; VERC_GPS; VERL_GPS; VERR_GPS; VIC__GPS; VIGE_GPS; VIGX_GPS; VLFR_GPS
    Type: Dataset
    Format: text/tab-separated-values, 178 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 4
    facet.materialart.
    Unknown
    Vertical displacement time series from GNSS stations in the great Alpine area (2021)
    PANGAEA
    Details
    Publication Date: 2024-04-20
    Description: ASCII files reporting the position time-series, in the Eurasia-fixed reference frame, of GNSS in the great Alpine area (excluding Switzerland). The columns are: Time, U, Su, site, long, lati, representing, respectively, epoch (in decimal years), displacement in the Up component (in mm), uncertainty (one standard deviation) of the Up component (in mm), Station ID, Longitude of the station (°), Latitude of the station (°).
    Keywords: 0256_GPS; 0257_GPS; 0258_GPS; 0259_GPS; 0261_GPS; 0264_GPS; 0265_GPS; 0266_GPS; 0268_GPS; 0269_GPS; 0270_GPS; 0272_GPS; 0273_GPS; 0275_GPS; 0276_GPS; 0278_GPS; 0279_GPS; 0280_GPS; 0281_GPS; 0282_GPS; 0285_GPS; 0286_GPS; 0291_GPS; 0292_GPS; 0293_GPS; 0294_GPS; 0296_GPS; 0384_GPS; 0386_GPS; 0388_GPS; 0389_GPS; 0391_GPS; 0392_GPS; 0396_GPS; 0397_GPS; 0398_GPS; 0400_GPS; 0401_GPS; 0402_GPS; 0403_GPS; 0404_GPS; 0405_GPS; 1271_GPS; ACCE_GPS; ACOM_GPS; AGDE_GPS; AGDS_GPS; AGEN_GPS; AGNE_GPS; AIGL_GPS; AILT_GPS; ALPE_GPS; Alps; ALSN_GPS; ALST_GPS; ALU2_GPS; AMB2_GPS; AMPE_GPS; AMST_GPS; ANAY_GPS; ANDA_GPS; ANDE_GPS; ANDF_GPS; AO01_GPS; AOST_GPS; ARAN_GPS; ARDN_GPS; ARNA_GPS; ASIA_GPS; ASTI_GPS; ATHI_GPS; ATPU_GPS; AUBG_GPS; AUTN_GPS; AVAL_GPS; AVR1_GPS; AXPV_GPS; BACT_GPS; BADE_GPS; BAJA_GPS; BAL2_GPS; BANN_GPS; BARC_GPS; BBYS_GPS; BEAU_GPS; BEVA_GPS; BEVE_GPS; BFO1_GPS; BIEL_GPS; BLEI_GPS; BLFT_GPS; BLG2_GPS; BLGN_GPS; BLIX_GPS; BLNO_GPS; BOBB_GPS; BODO_GPS; BOLG_GPS; BOLO_GPS; BOLZ_GPS; BOR__GPS; BORC_GPS; BORM_GPS; BOSC_GPS; BOUS_GPS; BOVE_GPS; BRBZ_GPS; BRET_GPS; BREZ_GPS; BRSE_GPS; BRU1_GPS; BSCN_GPS; BTAC_GPS; BUAN_GPS; BUSL_GPS; BUTE_GPS; BZRG_GPS; CACI_GPS; CAEN_GPS; CAFV_GPS; CAKO_GPS; CAMA_GPS; CAMN_GPS; CANL_GPS; CANV_GPS; CARP_GPS; CARZ_GPS; CAST_GPS; CATU_GPS; CAUS_GPS; CBRY_GPS; CDOM_GPS; CEL9_GPS; CELJ_GPS; CERN_GPS; CERV_GPS; CEVY_GPS; CFRM_GPS; CGIA_GPS; CHA9_GPS; CHAM_GPS; CHAS_GPS; CHBL_GPS; CHBS_GPS; CHI9_GPS; CHIA_GPS; CHIV_GPS; CHMX_GPS; CHOD_GPS; CHOT_GPS; CHPH_GPS; CHRM_GPS; CHTL_GPS; CITD_GPS; CJIH_GPS; CKRO_GPS; CLAP_GPS; CLFD_GPS; CLMT_GPS; COAU_GPS; CODR_GPS; COLI_GPS; COLL_GPS; COMO_GPS; CONC_GPS; CPRA_GPS; CPRI_GPS; CREA_GPS; CREI_GPS; CREM_GPS; CRNO_GPS; CRSN_GPS; CSTN_GPS; CSVI_GPS; CT30_GPS; CTAB_GPS; CTB5_GPS; CUOR_GPS; CVSE_GPS; CZNO_GPS; DALA_GPS; DATE/TIME; DELN_GPS; DEMN_GPS; DEVE_GPS; DIJO_GPS; DILL_GPS; displacements; DJON_GPS; DLBG_GPS; DOCO_GPS; DOJX_GPS; DOMS_GPS; DRUS_GPS; EGLT_GPS; ENTZ_GPS; EOST_GPS; ERCK_GPS; ERLA_GPS; ESAB_GPS; ESCO_GPS; Event label; EZEV_GPS; FAEZ_GPS; FDET_GPS; FDOS_GPS; FELT_GPS; FERA_GPS; FERR_GPS; FETA_GPS; FEUR_GPS; FIED_GPS; FJCP_GPS; FLDB_GPS; FLRC_GPS; FRTT_GPS; FUSE_GPS; GANP_GPS; GARD_GPS; GDIJ_GPS; GENO_GPS; GENU_GPS; GIE1_GPS; GLRA_GPS; GNSS; GNSS data; GNSS Receiver; GOD9_GPS; GORI_GPS; GOZZ_GPS; GPS; GRA__GPS; GRAC_GPS; GRAS_GPS; GRAV_GPS; GRAZ_GPS; GRON_GPS; GRZM_GPS; GSR1_GPS; GUAS_GPS; GUIL_GPS; GUMM_GPS; GUSS_GPS; HKBL_GPS; HUEG_GPS; IENG_GPS; ILBO_GPS; ILIB_GPS; IMP3_GPS; ISLA_GPS; ITIM_GPS; JARG_GPS; JENB_GPS; JOAN_GPS; JOUX_GPS; KARL_GPS; KARX_GPS; KIBG_GPS; KLA__GPS; KLAG_GPS; KOE2_GPS; KRBG_GPS; KTZ2_GPS; KUNZ_GPS; LAND_GPS; LANK_GPS; LASP_GPS; LATITUDE; LBUG_GPS; LEBE_GPS; LECC_GPS; LEIB_GPS; LENE_GPS; LEOB_GPS; LEOP_GPS; LERO_GPS; LFAZ_GPS; LGES_GPS; LIN__GPS; LINZ_GPS; LLIV_GPS; LOA9_GPS; LOAN_GPS; LOD0_GPS; LONGITUDE; LOZN_GPS; LRTZ_GPS; LSIE_GPS; LUCE_GPS; LYSH_GPS; MABZ_GPS; MAGA_GPS; MAKS_GPS; MAN2_GPS; MAN9_GPS; MANT_GPS; MARI_GPS; MARO_GPS; MARS_GPS; MARY_GPS; MATR_GPS; MATT_GPS; MAUP_GPS; MAVE_GPS; MDEA_GPS; MEDI_GPS; MELN_GPS; MENA_GPS; MERY_GPS; MGIS_GPS; MGRD_GPS; MICH_GPS; MINE_GPS; MIRA_GPS; MIRE_GPS; MIST_GPS; MLNO_GPS; MLVL_GPS; MNBL_GPS; MOCA_GPS; MODA_GPS; MOGG_GPS; MOGN_GPS; MONB_GPS; MONC_GPS; MONF_GPS; MONV_GPS; MONZ_GPS; MOP2_GPS; MOPI_GPS; MORB_GPS; MORN_GPS; MPRA_GPS; MPRV_GPS; MRGE_GPS; MRON_GPS; MSEL_GPS; MSGT_GPS; MSMM_GPS; MSRT_GPS; MT01_GPS; MT06_GPS; MTMN_GPS; MTRZ_GPS; MUEJ_GPS; MURZ_GPS; NARB_GPS; NAYC_GPS; NERO_GPS; NICA_GPS; NICE_GPS; NOGT_GPS; NOVE_GPS; NOVG_GPS; NOVR_GPS; NVPT_GPS; OATO_GPS; OBE__GPS; OBE4_GPS; OCHS_GPS; ODEZ_GPS; OGAG_GPS; OPMT_GPS; OSTA_GPS; OTER_GPS; PADO_GPS; PALI_GPS; PAM__GPS; PANA_GPS; PARD_GPS; PARM_GPS; PARO_GPS; PARR_GPS; PASS_GPS; PAT2_GPS; PAVI_GPS; PAYR_GPS; PAZO_GPS; PDOM_GPS; PEJO_GPS; PENC_GPS; PERP_GPS; PERX_GPS; PFA2_GPS; PIA1_GPS; PIAC_GPS; POBU_GPS; PORD_GPS; PORE_GPS; POZE_GPS; POZZ_GPS; PREM_GPS; PREX_GPS; PRIE_GPS; PRIJ_GPS; PRNY_GPS; PTRC_GPS; PTUJ_GPS; PUYA_GPS; PUYV_GPS; PZNA_GPS; RABU_GPS; RADO_GPS; RAMS_GPS; RAYL_GPS; REBO_GPS; REGG_GPS; RGNC_GPS; RIJE_GPS; RISO_GPS; RIXH_GPS; ROET_GPS; RONC_GPS; ROSD_GPS; ROV9_GPS; ROVE_GPS; ROVI_GPS; ROVR_GPS; RSPX_GPS; RST2_GPS; RSTL_GPS; SAAL_GPS; SABA_GPS; SALZ_GPS; SAPP_GPS; SAQU_GPS; SARL_GPS; SARN_GPS; SAUN_GPS; SAUV_GPS; SAV2_GPS; SAVI_GPS; SBG2_GPS; SBLS_GPS; SBPO_GPS; SCDA_GPS; SCHI_GPS; SDNA_GPS; SEEF_GPS; SEES_GPS; SERM_GPS; SERR_GPS; SETE_GPS; SEUR_GPS; SEVI_GPS; SGIL_GPS; SGIO_GPS; SHEI_GPS; SHLA_GPS; SILA_GPS; SILL_GPS; SIRT_GPS; SJDV_GPS; SJPL_GPS; SLOG_GPS; SLVT_GPS; SMNE_GPS; SMSP_GPS; SOMB_GPS; SON9_GPS; SOPH_GPS; SORI_GPS; SOUS_GPS; SPER_GPS; SPRN_GPS; SRBO_GPS; SRJV_GPS; STBX_GPS; STBZ_GPS; STEY_GPS; STJ9_GPS; STMA_GPS; STMR_GPS; STPO_GPS; STPS_GPS; STV2_GPS; SUBO_GPS; SUSE_GPS; TAMB_GPS; TANC_GPS; TANY_GPS; TARO_GPS; TARV_GPS; TEOL_GPS; Text file; Text file (File Size); THNV_GPS; Time series; TLIA_GPS; TLMF_GPS; TLSE_GPS; TOIR_GPS; TORC_GPS; TORI_GPS; TRAI_GPS; TRBL_GPS; TRE5_GPS; TRE8_GPS; TRE9_GPS; TREB_GPS; TREN_GPS; TREX_GPS; TRF2_GPS; TRI1_GPS; TRIE_GPS; TRMO_GPS; TRNO_GPS; TROP_GPS; TRYS_GPS; TUBO_GPS; TVSO_GPS; UDI1_GPS; UDI2_GPS; UNUD_GPS; VACO_GPS; VALJ_GPS; VALX_GPS; VARE_GPS; VAUD_GPS; VDOM_GPS; VELO_GPS; VEN1_GPS; VERB_GPS; VERG_GPS; VERO_GPS; VFCH_GPS; VICE_GPS; VIGE_GPS; VILR_GPS; VISN_GPS; VITT_GPS; VLCH_GPS; VLKM_GPS; VMIG_GPS; VNTE_GPS; VOUR_GPS; VSBO_GPS; WAB2_GPS; WEL2_GPS; WEYE_GPS; WIEN_GPS; WLBH_GPS; WOBG_GPS; WOFU_GPS; WT21_GPS; WTZA_GPS; WTZR_GPS; WTZS_GPS; WTZZ_GPS; ZABO_GPS; ZADA_GPS; ZALA_GPS; ZIDF_GPS; ZIM2_GPS; ZIMJ_GPS; ZIMM_GPS; ZOUF_GPS; ZYWI_GPS
    Type: Dataset
    Format: text/tab-separated-values, 545 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Recent tectonic reorganization of the Nubia-Eurasia convergent boundary heading for the closure of the western Mediterranean (2011)
    Societe Geologique de France (SGF)
    Details
    Publication Date: 2011-07-01
    Description: In the western Mediterranean area, after a long period (late Paleogene-Neogene) of Nubian (W-Africa) northward subduction beneath Eurasia, subduction has almost ceased, as well as convergence accommodation in the subduction zone. With the progression of Nubia-Eurasia convergence, a tectonic reorganization is therefore necessary to accommodate future contraction. Previously-published tectonic, seismological, geodetic, tomographic, and seismic reflection data (integrated by some new GPS velocity data) are reviewed to understand the reorganization of the convergent boundary in the western Mediterranean. Between northern Morocco, to the west, and northern Sicily, to the east, contractional deformation has shifted from the former subduction zone to the margins of the two back-arc oceanic basins (Algerian-Liguro-Provencal and Tyrrhenian basins) and it is now mainly active in the south-Tyrrhenian (northern Sicily), northern Liguro-Provencal, Algerian, and Alboran (partly) margins. Onset of compression and basin inversion has propagated in a scissor-like manner from the Alboran (c. 8 Ma) to the Tyrrhenian (younger than c. 2 Ma) basins following a similar propagation of the cessation of the subduction, i.e., older to the west and younger to the east. It follows that basin inversion is rather advanced on the Algerian margin, where a new southward subduction seems to be in its very infant stage, while it has still to really start in the Tyrrhenian margin, where contraction has resumed at the rear of the fold-thrust belt and may soon invert the Marsili oceanic basin. Part of the contractional deformation may have shifted toward the north in the Liguro-Provencal basin possibly because of its weak rheological properties compared with those of the area between Tunisia and Sardinia, where no oceanic crust occurs and seismic deformation is absent or limited. The tectonic reorganization of the Nubia-Eurasia boundary in the study area is still strongly controlled by the inherited tectonic fabric and rheological attributes, which are strongly heterogeneous along the boundary. These features prevent, at present, the development of long and continuous thrust faults. In an extreme and approximate synthesis, the evolution of the western Mediterranean is inferred to follow a Wilson Cycle (at a small scale) with the following main steps : (1) northward Nubian subduction with Mediterranean back-arc extension (since ~35 Ma); (2) progressive cessation, from west to east, of Nubian main subduction (since ~15 Ma); (3) progressive onset of compression, from west to east, in the former back-arc domain and consequent basin inversion (since ~8-10 Ma); (4) possible future subduction of former back-arc basins.
    Print ISSN: 0037-9409
    Electronic ISSN: 0037-9409
    Topics: Geosciences
    Published by Societe Geologique de France (SGF)
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 6
    facet.materialart.
    Unknown
    Poroelasticity and Fluid Flow Modeling for the 2012 Emilia-Romagna Earthquakes: Hints from GPS and InSAR Data (2018)
    Hindawi
    Details
    Publication Date: 2018-07-19
    Print ISSN: 1468-8115
    Electronic ISSN: 1468-8123
    Topics: Geosciences
    Published by Hindawi
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 7
    facet.materialart.
    Unknown
    Flooding scenario for four Italian coastal plains using three relative sea level rise models (2017)
    Taylor & Francis
    Details
    Publication Date: 2017-11-30
    Electronic ISSN: 1744-5647
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Taylor & Francis
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 8
    facet.materialart.
    Unknown
    Interference of tectonic signals in subsurface hydrologic monitoring through gravity and GPS due to mountain building (2018)
    Elsevier
    Details
    Publication Date: 2018-08-01
    Print ISSN: 0921-8181
    Electronic ISSN: 1872-6364
    Topics: Geosciences , Physics
    Published by Elsevier
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 9
    facet.materialart.
    Unknown
    New insights into active tectonics and seismogenic potential of the Italian Southern Alps from vertical geodetic velocities (2020)
    Copernicus
    Details
    Publication Date: 2020-09-04
    Description: This study presents and discusses horizontal and vertical geodetic velocities for a low strain rate region of the south Alpine thrust front in northeastern Italy obtained by integrating GPS, interferometric synthetic aperture radar (InSAR) and leveling data. The area is characterized by the presence of subparallel, south-verging thrusts whose seismogenic potential is still poorly known. Horizontal GPS velocities show that this sector of the eastern Southern Alps is undergoing ∼1 mm a−1 of NW–SE shortening associated with the Adria–Eurasia plate convergence, but the horizontal GPS velocity gradient across the mountain front provides limited constraints on the geometry and slip rate of the several subparallel thrusts. In terms of vertical velocities, the three geodetic methods provide consistent results showing a positive velocity gradient, of ∼ 1.5 mm a−1, across the mountain front, which can hardly be explained solely by isostatic processes. We developed an interseismic dislocation model whose geometry is constrained by available subsurface geological reconstructions and instrumental seismicity. While a fraction of the measured uplift can be attributed to glacial and erosional isostatic processes, our results suggest that interseismic strain accumulation at the Montello and the Bassano–Valdobbiadene thrusts it significantly contributing to the measured uplift. The seismogenic potential of the Montello thrust turns out to be smaller than that of the Bassano–Valdobbiadene fault, whose estimated parameters (locking depth equals 9.1 km and slip rate equals 2.1 mm a−1) indicate a structure capable of potentially generating a Mw〉6.5 earthquake. These results demonstrate the importance of precise vertical ground velocity data for modeling interseismic strain accumulation in slowly deforming regions where seismological and geomorphological evidence of active tectonics is often scarce or not conclusive.
    Print ISSN: 1869-9510
    Electronic ISSN: 1869-9529
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 10
    facet.materialart.
    Unknown
    AlpArray-Italy: Site description and noise characterization (2017)
    Copernicus
    Details
    Publication Date: 2017-03-13
    Description: Within the framework of the European collaborative research initiative AlpArray (http://www.alparray.ethz.ch), the Istituto Nazionale di Geofisica e Vulcanolgia (INGV) deployed overall 20 broad-band seismic stations in Northern Italy and on two islands in the Tyrrhenian Sea (Capraia and Montecristo) during Fall-Winter 2015. The temporary deployment (16 stations) will run for two to three years and 4 INGV National Seismic Network accelerometric sites are now equipped with additional permanent broad-band sensors. The 16 temporary stations are equipped with REF TEK 130 digitizers and Nanometrics Trillium Compact 120 s sensors, a couple have Nanometrics Trillium 120P sensors and one a Streckeisen STS2. For each site we describe the settings and discuss the noise levels, the site effects and the preliminary sensitivity analysis.
    Print ISSN: 1680-7340
    Electronic ISSN: 1680-7359
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...