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  • 1
    Publication Date: 2024-02-08
    Description: Current velocities of the upper water column along the cruise track of R/V Maria S. Merian cruise MSM118 were collected by a vessel-mounted 38 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 32.00 m, a blanking distance of 16.00 m, and a total of 50 bins, covering the depth range between 54.0 m and 1622.0 m. Heading, pitch and roll data from the ship's motion reference unit and the navigation data from the Global Positioning systems were used by the data acquisition software VmDAS internally to convert ADCP velocities into earth coordinates. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). 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 (0.3722° +/- 0.3598°) and scale factor (0.9991 +/- 0.0070) of the Ocean Surveyor signal. The velocity data were averaged in time using an average interval of 60 s. Velocity quality flagging is based on different threshold criteria: Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'. Depth cells with velocities above 1.5 m/s are flagged as 'bad data'. Depth cells with a root-mean-square deviation between the measured ensemble-average velocity and a cell-wise running-mean velocity above 0.2 m/s are flagged as 'probably bad data'.
    Keywords: Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; Maria S. Merian; MSM118; MSM118_0_Underway-3; NOVAMAR (2); Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); Vessel mounted Acoustic Doppler Current Profiler [38 kHz]; VMADCP-38
    Type: Dataset
    Format: text/tab-separated-values, 1922675 data points
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  • 2
    Publication Date: 2024-02-08
    Description: Current velocities of the upper water column along the cruise track of R/V Maria S. Merian cruise MSM118 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins, covering the depth range between 22.0 m and 814.0 m. Heading, pitch and roll data from the ship's motion reference unit and the navigation data from the Global Positioning systems were used by the data acquisition software VmDAS internally to convert ADCP velocities into earth coordinates. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). 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 (-47.3100° +/- 0.5215°) and scale factor (1.0011 +/- 0.0087) of the Ocean Surveyor signal. The velocity data were averaged in time using an average interval of 60 s. Velocity quality flagging is based on different threshold criteria: Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'. Depth cells with velocities above 1.5 m/s are flagged as 'bad data'. Depth cells with a root-mean-square deviation between the measured ensemble-average velocity and a cell-wise running-mean velocity above 0.2 m/s are flagged as 'probably bad data'.
    Keywords: Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; Maria S. Merian; MSM118; MSM118_0_Underway-4; NOVAMAR (2); Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75
    Type: Dataset
    Format: text/tab-separated-values, 4608350 data points
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  • 3
    Publication Date: 2024-02-24
    Description: Upper-ocean velocities along the cruise track of RV MARIA S. MERIAN cruise MSM102 were continuously collected by a vessel-mounted Teledyne RD Instruments 38 kHz Ocean Surveyor ADCP. The transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode with 32 m bins and a blanking distance of 16 m, while 50 bins were recorded using a pulse of 2.87 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 (0.40° +/- 0.6886°) and scale factor (1.0008 +/- 0.0494) of the Ocean Surveyor signal. The average interval was set to 120 s.
    Keywords: Acoustic Doppler Current Profiler; ADCP; Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; Maria S. Merian; MSM102; MSM102_0_Underway-3; MSM102_0_Underway-6; NAMOC; Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); Vessel mounted Acoustic Doppler Current Profiler [38 kHz]; VMADCP-38
    Type: Dataset
    Format: text/tab-separated-values, 4943560 data points
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  • 4
    Publication Date: 2024-02-24
    Description: Upper-ocean velocities along the cruise track of RV MARIA S. MERIAN cruise MSM102 were continuously collected by a vessel-mounted Teledyne RD Instruments 75 kHz Ocean Surveyor ADCP. The transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode with 8 m bins and a blanking distance of 8 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 (0.76° +/- 0.4377°) and scale factor (1.0017 +/- 0.0091) of the Ocean Surveyor signal. The average interval was set to 120 s.
    Keywords: Acoustic Doppler Current Profiler; ADCP; Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; Maria S. Merian; MSM102; MSM102_0_Underway-3; MSM102_0_Underway-7; NAMOC; Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75
    Type: Dataset
    Format: text/tab-separated-values, 12233125 data points
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  • 5
    Publication Date: 2020-08-21
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 6
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    Geoscience Society of New Zealand Miscellaneous Publication 145A
    In:  EPIC3Geosciences 2016, Wanaka, New Zealand, 2016-11-28-2016-12-01Geoscience Society of New Zealand Miscellaneous Publication 145A
    Publication Date: 2016-12-12
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
    Publication Date: 2017-09-21
    Description: The easternmost Chatham Rise is a key focus area for understanding the Cretaceous tectonics of the New Zealand region. It is the region where seafloor spreading between New Zealand and Antarctica first initiated. The West Wishbone Ridge, a major 1200 km long, northeast trending, gravity and bathymetry lineament intersects the Chatham Rise immediately east of where the Hikurangi Plateau LIP abuts the northern Chatham Rise, and 150 km east of the Chatham islands. The southeast Chatham Rise was once adjacent to Marie Byrd land in Antarctica, a key research focus area for the Alfred Wegener Helmholtz Institute (AWI), Germany. A seven-week seismic reflection/refraction and volcanic rock-dredging survey was conducted across the eastern Chatham Rise by the Alfred Wegener Helmholtz Institute in early 2016 using the new R/V Sonne research vessel. The survey collected four crustal scale seismic reflection and refraction lines across the eastern Chatham Rise, two seismic reflection lines across the Wishbone Ridge complex, and numerous dredges of seafloor volcano structures on the southeast Chatham Terrace, guided by multibeam swath data. GNS Science operated their gravity meter and magnetometer throughout most of the survey. The initial results from the survey will be presented and linked with existing data and concepts on the structure of the Chatham Rise accretionary prism structure (Rakaia versus Pahau) and its onshore South Island prolongation. The nature of the West Wishbone Ridge and similar Cretaceous fault structures and their role in Gondwana breakup will also be discussed.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 8
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    Wiley
    In:  EPIC3Geochemistry Geophysics Geosystems, Wiley, 19, pp. 1199-1216, ISSN: 1525-2027
    Publication Date: 2019-04-16
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 9
    Publication Date: 2021-07-27
    Description: Subduction of oceanic plateaux are events that have occurred infrequently in Earth's history. Although rare, these events are thought to considerably influence regional tectonics and global plate motions. In the mid-Cretaceous the oceanic Hikurangi Plateau collided with the formerly active East Gondwana margin: An event which falls into the same of a sudden change from subduction to extensional processes, including graben formation, development rift basin development, and exhumation of metamorphic core complexes in the Zealandia continent as well as a global-scale plate reorganization event. In this study, we use recently acquired seismic refraction and gravity data along one profile across the submarine Chatham Rise, which represent a former accretionary wedge of the East Gondwana subduction zone. We demonstrate that the southward extent of the subducted Hikurangi Plateau in the lower crust beneath the submarine Chatham Rise along our profile is only ~150. This is ~150 km less than the previously suggested extent. Furthermore, we interpret that a slice of the subducted Phoenix Plate remains attached to the southern edge of the Hikurangi Plateau. We suggest that cessation of subduction in response to the Hikurangi Plateau jamming as well as the rollback and detachment of the Phoenix Plate slab played an important role in the changing tectonic forces across Zealandia in mid-Cretaceous. Moreover, we suggest that the subduction cessation along the Hikurangi Plateau segment led to the fragmentation of the Gondwana subduction zone and Phoenix Plate, which significantly influenced and potentially prolonged the global mid-Cretaceous plate reorganization event.
    Keywords: 551.136 ; Chatham Rise ; accretionary wedge ; Hikurangi Plateau ; oceanic plateau ; Zealandia ; refraction seismics
    Language: English
    Type: article
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  • 10
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