Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1016/j.egypro.2017.08.071
Titel (primär) Thermal impacts of magmatic intrusions: a hypothesis of paleo-heating processes in the Tiberias Basin, Jordan-Dead Sea Transform
Autor Koltzer, N.; Möller, P.; Inbar, N.; Siebert, C. ORCID logo ; Rosenthal, E.; Magri, F.
Quelle Energy Procedia
Erscheinungsjahr 2017
Department ENVINF; CATHYD
Band/Volume 125
Seite von 80
Seite bis 87
Sprache englisch
Keywords Lake Tiberias; FEFLOW; thermal field; Tiberias Basin; fault; temperature anomaly
UFZ Querschnittsthemen RU2
Abstract 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.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=19317
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 10.1016/j.egypro.2017.08.071