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Neumann, Florian; Negrete-Aranda, Raquel; Contreras, Juan; González-Fernández, Antonio (2019): Heat flow measurements from the northern Gulf of California [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.905091, 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

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Abstract:
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.
Keyword(s):
advective heat transport; continental rupture; distributed deformation; Gulf of California extensional province; narrow rift
Coverage:
Median Latitude: 30.988432 * Median Longitude: -114.167982 * South-bound Latitude: 30.923400 * West-bound Longitude: -114.311200 * North-bound Latitude: 31.091200 * East-bound Longitude: -113.940600
Date/Time Start: 2018-01-01T00:00:00 * Date/Time End: 2018-12-01T00:00:00
Minimum DEPTH, water: 57 m * Maximum DEPTH, water: 208 m
Event(s):
HF003P01 * Latitude: 31.056400 * Longitude: -114.016600 * Location: Gulf of California * Method/Device: Heat-Flow probe (HF)
HF004P01 * Latitude: 31.053300 * Longitude: -114.023300 * Location: Gulf of California * Method/Device: Heat-Flow probe (HF)
HF004P03 * Latitude: 31.045900 * Longitude: -114.042600 * Location: Gulf of California * Method/Device: Heat-Flow probe (HF)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventNeumann, Florian
2DEPTH, waterDepth watermNeumann, FlorianGeocode
3Bottom water temperatureBWT°CNeumann, FlorianCTD
4Bottom water temperatureBWT°CNeumann, FlorianCTDLong-term
5Bottom water temperature, errorBWT e±Neumann, FlorianCTDLong-term, 2 sigma
6Temperature, differencedelta T°CNeumann, FlorianCalculatedAmplitude
7Temperature, standard deviationT std dev±Neumann, FlorianCalculatedAmplitude, 2 sigma
8DATE/TIMEDate/TimeNeumann, FlorianGeocode – Month of year
9Heat flowHFmW/m2Neumann, FlorianViolin-bow probe (Multipenetration Heat Flow Probe)
10Heat flow, standard deviationHF std dev±Neumann, FlorianViolin-bow probe (Multipenetration Heat Flow Probe)
Size:
196 data points

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