Geothermal measurements in the Tyrrhenian Sea

DOI

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.

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

Identifier
DOI https://doi.org/10.1594/PANGAEA.757449
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.757449
Provenance
Creator Verzhbitsky, Evgeny V; Sborshchikov, Igor M; Shilovskiy, Pavel P
Publisher PANGAEA
Publication Year 1988
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 128 data points
Discipline Earth System Research
Spatial Coverage (10.015W, 39.362S, 14.393E, 40.908N); Tyrrhenian Sea