English
 
Privacy Policy Disclaimer
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT
Add to Basket
  Local TagsRelease HistoryDetailsSummary

Released
Journal Article

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

Authors
/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;

External Ressource
No external resources are shared
Fulltext (public)

2609888.pdf
(Publisher version), 4MB

Supplementary Material (public)
There is no public supplementary material available
Citation

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


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_2609888
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.