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  • IODP  (1)
  • advective heat transport; Bottom water temperature; Bottom water temperature, error; Calculated; continental rupture; CTD; DATE/TIME; DEPTH, water; distributed deformation; Event label; Gulf of California; Gulf of California extensional province; Heat flow; Heat flow, standard deviation; Heat-Flow probe; HF; HF003P01; HF004P01; HF004P03; HF004P04; HF005P04; HF005P06; HF005P07; HF005P08; HF005P09; HF005P10; HF005P11; HF005P12; HF006P01; HF006P02; HF006P03; HF006P04; HF006P05; HF006P06; HF006P07; HF006P08; HF007P01; HF007P02; HF007P03; HF007P04; HF007P05; HF008P010; HF008P013; HF010P03; narrow rift; Temperature, difference; Temperature, standard deviation; Violin-bow probe (Multipenetration Heat Flow Probe)  (1)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Neumann, Florian; Negrete-Aranda, Raquel; Harris, Robert N; Contreras, Juan; Sclater, John G; González-Fernández, Antonio (2017): Systematic heat flow measurements across the Wagner Basin, northern Gulf of California. Earth and Planetary Science Letters, 479, 340-353, https://doi.org/10.1016/j.epsl.2017.09.037
    Publication Date: 2023-01-13
    Description: A primary control on the geodynamics of rifting is the thermal regime. To better understand the geodynamics of rifting in the northern Gulf of California we systematically measured heat-flow across the Wagner Basin, a tectonically active basin that lies near the southern terminus of the Cerro Prieto fault. The heat flow profile is 40 km long, has a nominal measurement spacing of ∼1 km, and is collocated with a seismic reflection profile. Heat flow measurements were made with a 6.5-m violin-bow probe. Although heat flow data were collected in shallow water, where there are significant temporal variations in bottom water temperature, we use CTD data collected over many years to correct our measurements to yield accurate values of heat flow. After correction for bottom water temperature, the mean and standard deviation of heat flow across the western, central, and eastern parts of the basin are 220 ±60, 99 ±14, 889 ±419mWm−2, respectively. Corrections for sedimentation would increase measured heat flow across the central part of basin by 40 to 60%. We interpret the relatively high heat flow and large variability on the western and eastern flanks in terms of upward fluid flow at depth below the seafloor, whereas the lower and more consistent values across the central part of the basin are suggestive of conductive heat transfer. Moreover, heat flow across the central basin is consistent with gabbroic underplating at a depth of 15 km and suggests that continental rupture here has not gone to completion.
    Keywords: advective heat transport; Bottom water temperature; Bottom water temperature, error; Calculated; continental rupture; CTD; DATE/TIME; DEPTH, water; distributed deformation; Event label; Gulf of California; Gulf of California extensional province; Heat flow; Heat flow, standard deviation; Heat-Flow probe; HF; HF003P01; HF004P01; HF004P03; HF004P04; HF005P04; HF005P06; HF005P07; HF005P08; HF005P09; HF005P10; HF005P11; HF005P12; HF006P01; HF006P02; HF006P03; HF006P04; HF006P05; HF006P06; HF006P07; HF006P08; HF007P01; HF007P02; HF007P03; HF007P04; HF007P05; HF008P010; HF008P013; HF010P03; narrow rift; Temperature, difference; Temperature, standard deviation; Violin-bow probe (Multipenetration Heat Flow Probe)
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2023-02-15
    Description: Abstract
    Description: The data publication contains all heat-flow data of offshore in the Guaymas basin. The data release contains data generated between 1959 and 2019 and constitutes a substantial update and extension compared to the last compilation provided by Becker & Fisher (1991). The data set comprises new heat-flow determinations published after 1991 as well as data from before 1991, which were not included in the Becker & Fisher (1991). The resulting updated database contains 487 determinations of heat-flow at 464 locations from 17 publications. 95% of the reported heat-flow values are determined from marine probe sensing technique and 5% in boreholes.
    Description: Methods
    Description: The reporting and storing of the database are following the structure of the IHFC Global Heat Flow Database (Fuchs et al., 2021). A comprehensive description, including field classifications and examples of associated data, is documented there. The IHFC database concept introduces parent elements (providing site-specific information), child elements (i.e., heat-flow values determined at the site and associated meta-data) and further fields providing additional information for the evaluation of heat flow quality. Thus, it provides a detailed collection of data and meta-data information, exceeding the sparse information on coordinates, name and heat-flow value.
    Keywords: Heat flow ; Guaymas Basin ; IODP ; EARTH SCIENCE 〉 OCEANS 〉 MARINE VOLCANISM 〉 BENTHIC HEAT FLOW ; physical property 〉 temperature
    Type: Dataset , Dataset
    Location Call Number Expected Availability
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