Insights into geochemical characteristics of the geothermal fluids of northwestern algeria: An updated conceptual model

•Water chemistry highlights the heterogeneity of mineralization.•Trace elements identify two chlorides water sources.•The paleoclimatological effect explains the isotopic depletion.•Geothermometrical techniques corroborate on reservoir temperatures

Saved in:
Bibliographic Details
Published in:Geothermics 2022-02, Vol.99, p.102304, Article 102304
Main Authors: Belhai, Mohamed, Fujimitsu, Yasuhiro, Barragan-Reyes, Rosa Maria, Iwanaga, Tatsuto, Maeno, Mamiko, Ayad, Brahim, Bouchareb-Haouchine, Fatima Zohra, Nishijima, Jun, Belhai, Djelloul, Haouchine, Abdelhamid
Format: Article
Language:English
Subjects:
Altitude
Calcium ions
Carbon dioxide
Climatic conditions
Depletion
Electrical raceways
Geochemical models
Geochemistry
Geothermal fluids
Geothermal power
Geothermal zones
geothermometers
Glacial periods
Gypsum
Heat
Heat flow
Heat transmission
Heterogeneity
High altitude
Hot springs
Intrusive bodies
Isotopes
Magma
Magnesium
Meteoric water
Mineralization
Northwestern algeria
Percolation
Quaternary
Recharging
Spring water
Stable isotopes
Tectonics
Thermal water
Travertine
Vents
Volcanic activity
Water analysis
Water circulation
Water sampling
Water springs
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:•Water chemistry highlights the heterogeneity of mineralization.•Trace elements identify two chlorides water sources.•The paleoclimatological effect explains the isotopic depletion.•Geothermometrical techniques corroborate on reservoir temperatures
ISSN:0375-6505
1879-3576
DOI:10.1016/j.geothermics.2021.102304