Novyye dannyye o teplovom potoke Severnoy Atlantiki (New heat flow data of the North Altlantic)
Vitaly Akhmedzyanov, Alexander V Ermakov
This dataset comprises 41 new heat flow measurements collected during two marine expeditions in 2008 and 2010 in the Arctic region west of the Svalbard Archipelago, including the Knipovich Ridge area in the North Atlantic. These measurements provide evidence for elevated geothermal activity consistent with recent geodynamic processes. Numerical modeling using these data reveals deep lithospheric temperatures exceeding 1200°C at depths of approximately 15 km, supporting the interpretation of Knipovich Ridge as a young oceanic rift formed since the Miocene. These data offer valuable constraints for thermal modeling of the North Atlantic lithosphere and contribute to the understanding of Arctic …
Heat flow and temperature gradient data from Spain
This dataset provides geothermal gradient and heat flow estimates derived from temperature loggings in 187 oil exploration wells across Spain, including 43 located in offshore marine areas. The measurements were used to create a preliminary heat flow map of the Iberian Peninsula and surrounding shelf waters. The mean heat flow on land is 82 mW m⁻², while offshore areas exhibit higher values averaging 99 mW m⁻²—both exceeding the European continental average. A regional trend shows increasing heat flow toward the Mediterranean coast, which inversely correlates with crustal thickness. Corresponding Moho temperatures range from 720°C in central Spain to 880°C near …
Heat flow and thermal regime in the Guaymas Basin, Gulf of California: Estimates of conductive and advective heat transport
This dataset presents heat flow estimates from eight drilling sites in the Guaymas Basin, Gulf of California, collected during the International Ocean Discovery Program (IODP) Expedition 385. The data capture the thermal regime of a sediment-filled, magmatically active rift basin where sills intrude into organic-rich sediments. Sedimentation-corrected heat flow values range from 119 to 221 mW m⁻² across the basin and rise dramatically to 257–1003 mW m⁻² at a young sill complex known as Ringvent. Thermal and hydrological modeling indicates that Ringvent is currently cooling via hydrothermal circulation, with discharge velocities of 10–200 mm yr⁻¹. The results provide critical insights …
Systematic heat flow measurements across the Wagner Basin, northern Gulf of California
This dataset comprises heat flow measurements collected along a 40 km transect across the Wagner Basin in the northern Gulf of California, a region of active continental rifting. Measurements were taken using a 6.5 m violin-bow probe at ~1 km spacing, co-located with a seismic reflection profile. Bottom water temperatures were corrected using long-term CTD (conductivity-temperature-depth) records. After correction, mean heat flow values were 220 ± 60 mW m⁻² (western basin), 99 ± 14 mW m⁻² (central basin), and 889 ± 419 mW m⁻² (eastern basin). Additional corrections for sedimentation are estimated to increase central basin heat flow by 40–60%. …
RV SONNE 241 Cruise Report / Fahrtbericht, Manzanillo, 23.6.2015 – Guayaquil, 24.7.2015 : SO241 - MAKS: Magmatism induced carbon escape from marine sediments as a climate driver – Guaymas Basin, Gulf of California
During RV Sonne Expedition SO241, heat flow data were collected in the Guaymas Basin, Gulf of California, to characterize the thermal structure of a sediment-filled rift basin affected by active magmatic intrusions. Heat flow observations were supported by the acquisition of approximately 1100 km of 2D seismic reflection data to identify features such as sills and bottom-simulating reflectors. Additional thermal observations were made at multiple seep sites and at a newly discovered hydrothermal mound using coring tools, fluid sampling equipment, and visual surveys.
The surface heat flow of the Arabian Shield in Jordan
Andrea Förster, Hans Jürgen Förster
Surface heat flow in southern Jordan was determined from a cluster of five boreholes, each reaching depths of up to 900 m and penetrating Paleozoic sedimentary rocks. The study area lies along the eastern margin of the Dead Sea Transform fault system and covers approximately 300 km². Continuous temperature logs were collected from each borehole and combined with laboratory measurements of thermal conductivity obtained from drill cores and surface rock samples to calculate heat flow values.