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  • 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)
  • Acoustic Doppler Current Profiling (ADCP); Calculated; Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; GPF 20‐3_090, TRANSFORMERS; LATITUDE; LONGITUDE; M170; M170_0_Underway-1; Meteor (1986); Pings, averaged to a double ensemble value; Quality flag, current velocity; Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75  (1)
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  • 1
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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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  • 2
    Publication Date: 2024-01-26
    Description: Upper-ocean velocities along the cruise track of Meteor cruise M170 were continuously collected by a vessel-mounted Teledyne RD Instruments 75 kHz Ocean Surveyor ADCP. The transducer was located at 5.0 m below the water line. The instrument was operated in narrowband mode with 8 m bins and a blanking distance of 4.0 m, while 100 bins were recorded using a pulse of 1.43 s. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Heading, pitch and roll data from the ship's gyro platforms and the navigation data were used by the data acquisition software VmDas internally to convert ADCP velocities into earth coordinates. Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data post-processing included water track calibration of the misalignment angle ( -0.18° +/- 0.5601°) and scale factor (0.9992 +/- 0.0098) of the Ocean Surveyor signal. The average interval was set to 60 s.
    Keywords: Acoustic Doppler Current Profiling (ADCP); Calculated; Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; GPF 20‐3_090, TRANSFORMERS; LATITUDE; LONGITUDE; M170; M170_0_Underway-1; Meteor (1986); Pings, averaged to a double ensemble value; Quality flag, current velocity; Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75
    Type: Dataset
    Format: text/tab-separated-values, 9276100 data points
    Location Call Number Limitation Availability
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