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  • 3D tomography  (1)
  • 551.22  (1)
  • A30/S30; Costa Rica; crustal structure; Event label; EW9502; EW9502_obh81; EW9502_obh83; EW9502_obh89; EW9502_obh91; EW9502_obh93; EW9502_obh95; EW9502_obh97; EW9502_p301; EW9502_p302; File content; File format; File name; File size; L02; L03; L05; L07; L09; L12; L14; Latitude of event; Longitude of event; Maurice Ewing; OBH; obh81; obh83; obh89; obh91; obh93; obh95; obh97; Ocean bottom hydrophone; onshore/offshore; Osa peninsula; S30; Sampling on land; SEIS; Seismic; Seismic refraction data; TICOSECT; TICOSECT_L02; TICOSECT_L03; TICOSECT_L05; TICOSECT_L07; TICOSECT_L09; TICOSECT_L12; TICOSECT_L14; Uniform resource locator/link to metadata file; Uniform resource locator/link to sgy data file; Vertical geophone; V-GP  (1)
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  • 1
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 551.22 ; 550
    Language: English
    Type: article , publishedVersion
    Format: 98 S.
    Format: application/pdf
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2022-12-01
    Description: About 25% of the Earth’s mid-ocean ridges spread at ultraslow rates of less than 20 mm/yr. However, most of these ultraslow spreading ridges are located in geographically remote areas, which hamper investigation. Consequently, how the crust forms and ages at such spreading centres, which traditional models predict to be magma-starved and cold, remains poorly understood. One of the most accessible ultra-slow spreading centres is the Mid Cayman Spreading Centre (MCSC), in the Caribbean Sea, with spreading rates of ~15-17 mm/yr. CAYSEIS project was proposed to survey the Cayman Trough area in order to obtain new data that constraints the nature of the crust, tectonic structures, lithologies outcropping and hydrothermal processes taking place in this area. Understanding the sub-seabed geophysical structure of the MCSC is key to understanding not only the lithologies and structures exposed at the seabed, but more fundamentally, how they are related at depth and what role hydrothermal fluid flow plays in the geodynamics of ultraslow spreading. CAYSEIS was a joint and multidisciplinary programme of German, British and US American top tier scientists designed for the obtaining of a new high-quality dataset, including 3D Wide-Angle Seismic (WAS), magnetic, gravimetric and seismological data. During the CAYMAN project, we took leverage of the CAYSEIS dataset to invert a 3D tomographic model of the Cayman Trough lithosphere using the Tomo3D code (Meléndez et al., 2015; 2019). This is one of the first times that the Tomo3D code is used for 3D inversion of real datasets. Thus, we are checking our results comparing them with tomographic inversions of 2D lines and testing the different parameters to obtain the more accurate and higher resolution model as possible. The results of this experiment will show not only the lithospheric structure along and across the MSCS, including the exhumed Ocean Core Complexes in the surrounding areas, but the 3D lithospheric configuration of the region which is important to understand the crustal formation processes and the evolution of ultra-slow spreading settings.
    Description: Poster
    Description: poster
    Keywords: ddc:550 ; 3D tomography ; crustal characterization ; ultra-slow spreading ; Cayman Trough
    Language: English
    Type: doc-type:conferenceObject
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  • 3
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    PANGAEA
    In:  Supplement to: Martinez-Loriente, Sara; Sallarès, Valenti; Ranero, César R; Ruh, Jonas B; Barckhausen, Udo; Grevemeyer, Ingo; Bangs, N L (2019): Influence of Incoming Plate Relief on Overriding Plate Deformation and Earthquake Nucleation: Cocos Ridge Subduction (Costa Rica). Tectonics, 38(12), 4360-4377, https://doi.org/10.1029/2019TC005586
    Publication Date: 2023-05-20
    Description: The TICOSECT program aimed to investigate the crustal structure of the active continental margin of Costa Rica and to understand the geodynamic processes within the subduction system. With the help of a comprehensive wide-angle seismic data set, composed of an onshore/offshore experiment as well as refraction measurements on land in northern Costa Rica, the lithospheric structure from the Middle America Trench (MAT) to the Caribbean lowland was surveyed seismically. Here we provide seismic refraction data from an onshore/offshore seismic profile shot with the US American research vessel RV Mauris Ewing in spring of 1995 offshore of the Osa peninsula during the cruise EW9502. Data are reduced with 6 km/s and origin of the time series is at -2 sec. Note: the profile has been shot twice with a different shot interval at 25 s (p301) and 60 s (p302). Additional data from US partners can be found at http://www-udc.ig.utexas.edu/sdc/cruise.php?cruiseIn=ew9502.
    Keywords: A30/S30; Costa Rica; crustal structure; Event label; EW9502; EW9502_obh81; EW9502_obh83; EW9502_obh89; EW9502_obh91; EW9502_obh93; EW9502_obh95; EW9502_obh97; EW9502_p301; EW9502_p302; File content; File format; File name; File size; L02; L03; L05; L07; L09; L12; L14; Latitude of event; Longitude of event; Maurice Ewing; OBH; obh81; obh83; obh89; obh91; obh93; obh95; obh97; Ocean bottom hydrophone; onshore/offshore; Osa peninsula; S30; Sampling on land; SEIS; Seismic; Seismic refraction data; TICOSECT; TICOSECT_L02; TICOSECT_L03; TICOSECT_L05; TICOSECT_L07; TICOSECT_L09; TICOSECT_L12; TICOSECT_L14; Uniform resource locator/link to metadata file; Uniform resource locator/link to sgy data file; Vertical geophone; V-GP
    Type: Dataset
    Format: text/tab-separated-values, 122 data points
    Location Call Number Limitation Availability
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