Deutsch
 
Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT

Freigegeben

Zeitschriftenartikel

Thermal impacts of magmatic intrusions: a hypothesis of paleo-heating processes in the Tiberias Basin, Jordan-Dead Sea Transform

Urheber*innen
/persons/resource/koltzer

Koltzer,  Nora
6.1 Basin Modelling, 6.0 Geotechnologies, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

/persons/resource/pemoe

Möller,  Peter
3.4 Fluid Systems Modelling, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Inbar,  Nimrod
External Organizations;

Siebert,  Christian
External Organizations;

Rosenthal,  Eliyahu
External Organizations;

Magri,  Fabien
External Organizations;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (frei zugänglich)

2609888.pdf
(Verlagsversion), 4MB

Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Koltzer, N., Möller, P., Inbar, N., Siebert, C., Rosenthal, E., Magri, F. (2017): Thermal impacts of magmatic intrusions: a hypothesis of paleo-heating processes in the Tiberias Basin, Jordan-Dead Sea Transform. - Energy Procedia, 125, 80-87.
https://doi.org/10.1016/j.egypro.2017.08.071


Zitierlink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_2609888
Zusammenfassung
Extensive evidence of Ca-rich brine at the western side of Lake Tiberias (LT), Israel, refers to dolomitization processes. Dolomitization of Mg-rich brine saturated limestones preferentially occurs at enhanced temperatures. The presence of wide areas of fissured basalt in that area suggests that magma, which erupted through fissures, sufficiently heated initiating dolomitization. In this study we numerically investigate possible paleo-heating processes related to magmatic intrusions.