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

Nora Koltzer; Peter Möller; Nimrod Inbar; Christian Siebert; Eliyahu Rosenthal; Fabien Magri

doi:10.1016/j.egypro.2017.08.071

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

Nora Koltzer, Peter Möller, Nimrod Inbar, Christian Siebert, Eliyahu Rosenthal, Fabien Magri

نتاج البحث: نشر في مجلة › مقالة من مؤنمر › مراجعة النظراء

3 اقتباسات (Scopus)

ملخص

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.

اللغة الأصلية	الإنجليزيّة
الصفحات (من إلى)	80-87
عدد الصفحات	8
دورية	Energy Procedia
مستوى الصوت	125
المعرِّفات الرقمية للأشياء	https://doi.org/10.1016/j.egypro.2017.08.071
حالة النشر	نُشِر - 2017
منشور خارجيًا	نعم
الحدث	European Geosciences Union General Assembly 2017: Energy, Resources and the Environment (ERE): Meeting the Challenges of the Future - Vienna, النمسا المدة: ٢٣ أبريل ٢٠١٧ → ٢٨ أبريل ٢٠١٧

الوصول إلى المستند

10.1016/j.egypro.2017.08.071

الملفات والروابط الأخرى

Link to publication in Scopus

قم بذكر هذا

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

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.",

keywords = "FEFLOW, Lake Tiberias, Tiberias Basin, fault, temperature anomaly, thermal field",

author = "Nora Koltzer and Peter M{\"o}ller and Nimrod Inbar and Christian Siebert and Eliyahu Rosenthal and Fabien Magri",

note = "Publisher Copyright: {\textcopyright} 2017 The Authors. Published by Elsevier Ltd.; European Geosciences Union General Assembly 2017: Energy, Resources and the Environment (ERE): Meeting the Challenges of the Future ; Conference date: 23-04-2017 Through 28-04-2017",

year = "2017",

doi = "10.1016/j.egypro.2017.08.071",

language = "אנגלית",

volume = "125",

pages = "80--87",

journal = "Energy Procedia",

issn = "1876-6102",

publisher = "Elsevier Ltd.",

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TY - JOUR

T1 - Thermal impacts of magmatic intrusions

T2 - European Geosciences Union General Assembly 2017: Energy, Resources and the Environment (ERE): Meeting the Challenges of the Future

AU - Koltzer, Nora

AU - Möller, Peter

AU - Inbar, Nimrod

AU - Siebert, Christian

AU - Rosenthal, Eliyahu

AU - Magri, Fabien

PY - 2017

Y1 - 2017

N2 - 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.

AB - 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.

KW - FEFLOW

KW - Lake Tiberias

KW - Tiberias Basin

KW - fault

KW - temperature anomaly

KW - thermal field

UR - http://www.scopus.com/inward/record.url?scp=85030687703&partnerID=8YFLogxK

U2 - 10.1016/j.egypro.2017.08.071

DO - 10.1016/j.egypro.2017.08.071

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AN - SCOPUS:85030687703

SN - 1876-6102

VL - 125

SP - 80

EP - 87

JO - Energy Procedia

JF - Energy Procedia

Y2 - 23 April 2017 through 28 April 2017

ER -

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

ملخص

الوصول إلى المستند

الملفات والروابط الأخرى

بصمة

قم بذكر هذا