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Yamano, Makoto; Uyeda, Seiya (1990): (Table 1) Heat flow measurements during the MW8506 cruise. PANGAEA,, In supplement to: Yamano, M; Uyeda, S (1990): Heat-flow studies in the Peru trench subduction zone. In: Suess, E; von Huene, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 112, 653-661,

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Median Latitude: -10.458880 * Median Longitude: -79.608000 * South-bound Latitude: -11.425000 * West-bound Longitude: -80.743300 * North-bound Latitude: -9.018300 * East-bound Longitude: -78.756700
Minimum DEPTH, sediment/rock: 1.0 m * Maximum DEPTH, sediment/rock: 5.0 m
DEPTH, sediment (m) is the estimated penetration of the lowermost active thermistor. At HF2 (11°29.1'S, 78°22.3'W, 1435 m water depth) and HF3 (11°17.4'S, 78°38.5'W, 2205 m water depth), temperature gradients cannot be determined as the temperature profiles are nonlinear.
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Sample code/labelSample labelYamano, Makoto
4Depth, bathymetricBathy depthmYamano, Makoto
5DEPTH, sediment/rockDepthmGeocode
6NumberNoYamano, Makotoof active thermistors in mud
7Temperature (thermal) gradientT grad10-3 °C/cmYamano, Makoto
8Conductivity, thermalkW/m/KYamano, Makoto
9Heat FlowHFmW/m2Yamano, Makoto
90 data points

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