Geothermal measurements in the Tyrrhenian Sea
| Cobertura |
MEDIAN LATITUDE: 40.329583 * MEDIAN LONGITUDE: 11.421875 * SOUTH-BOUND LATITUDE: 39.361667 * WEST-BOUND LONGITUDE: 10.015000 * NORTH-BOUND LATITUDE: 40.908333 * EAST-BOUND LONGITUDE: 14.393333 * MINIMUM ELEVATION: -3440.0 m * MAXIMUM ELEVATION: -1090.0 m |
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| Data(s) |
17/02/1988
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| Resumo |
Geothermal data obtained during Cruise 12 of the R/V Vityaz-II and published data on heat flux of the Tyrrhenian Sea are analyzed. The thermal field is related to principal tectonic structures of the basin. Distribution of heat flux indicates that the initial stage of rifting occurs in the central basin of the Tyrrhenian Sea. |
| Formato |
text/tab-separated-values, 128 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.757449 doi:10.1594/PANGAEA.757449 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Verzhbitsky, Evgeny V; Sborshchikov, Igor M; Shilovskiy, Pavel P (1988): Heat flux and geology of the Tyrrhenian Sea. Oceanology, 28(4), 498-501 |
| Palavras-Chave | #Archive of Ocean Data; ARCOD; Calculated; Comment; Conductivity, thermal; Conductivity, thermal, standard deviation; Elevation of event; Event label; Geothermic corer; GTC; Heat Flow; Heat Flow, standard deviation; Latitude of event; Longitude of event; Penetration depth; Temperature (thermal) gradient; Temperature (thermal) gradient, standard deviation; Thermal conductive detector (TCD); Thermistor; Tyrrhenian Sea; Vy12-1621; Vy12-1621a; Vy12-1624; Vy12-1632; Vy12-1632a; Vy12-1632b; Vy12-1633; Vy12-1633a; Vy12-1634; Vy12-1634a; Vy12-1634b; Vy12-1664; Vy12-1671; Vy12-1671a; Vy12-1672; Vy12-1672a |
| Tipo |
Dataset |
