Title : ( Geothermal Rreservoir Characteristics (T & D) of Ayub Peighambar and Shafa Hot Springs Using Geothermometers and Environmental 2H and 18O Isotopes )
Authors: Hossein Mohammadzadeh , majid kazemi ,
Full TextAbstract
Hot springs are evidence of geothermal filed, where the internal thermal of the earth, resulted from volcanic activities and from geochemical reactions, is transferring to the land surface. Ayub Peighambar and Shafa hot springs, with temperature of about 40 oC and CaSO4 water type, are located in Northeast of Iran. These springs due to have high temperature than other adjacent springs and are using for balneotherapy purposes, are very important. According to geotermometery and stable isotope (18O and 2H) studies, depth of Ayub Peighambar hot spring geothermal reservoir is about 4-5 kilometer and its temperature is less than 150 oC.
Keywords
, Ayub Peighambar hot spring, Geothermal, stable isotope (18O and 2H)
@inproceedings{paperid:1048526,
author = {Mohammadzadeh, Hossein and Kazemi, Majid},
title = {Geothermal Rreservoir Characteristics (T & D) of Ayub Peighambar and Shafa Hot Springs Using Geothermometers and Environmental 2H and 18O Isotopes},
booktitle = {International Symposium on Isotope Hydrology},
year = {2015},
location = {Vienna, Austria},
keywords = {Ayub Peighambar hot spring; Geothermal; stable isotope (18O and 2H)},
}
%0 Conference Proceedings
%T Geothermal Rreservoir Characteristics (T & D) of Ayub Peighambar and Shafa Hot Springs Using Geothermometers and Environmental 2H and 18O Isotopes
%A Mohammadzadeh, Hossein
%A Kazemi, Majid
%J International Symposium on Isotope Hydrology
%D 2015
