Title : ( GEOTHERMOMETRY OF TWO HOT SPRINGS IN WESTERN IRAN )
Authors: Yasaman Rafighdoust , ECKSTEIN Yoram , Sayyed Reza Moussavi Harami , Asadollah Mahboubi , Mohamad Hosein Mahmudy Gharaie ,
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Abstract
Reservoir temperatures of Tang-Bijar Oilfield hot springs located at the Zagros Fold and Thrust Belt of western Iran, including Sr17 (Tang-Hamam) and Tb3 (Tang-Bijar), were estimated by using Quartz (Fournier, 1977) and cation geothermometers (Fournier, 1979; Fournier and Potter, 1979) Na–K–Mg triangular diagram (Giggenbach, 1988) and Na–K–Mg–Ca square diagram (Arn?rsson, 2000). water of Sr17 hot spring suggests either partial equilibration at temperature below 70°C (“immature waters”), or mixing and dilution by cold recharge water on the upward flow-path to the ground surface. The brackish water of the Tb3 hot spring are seemingly in full equilibrium (“mature waters”) with the local evaporitic formations at the temperatures between 75 and 100°C.
Keywords
, Reservoir temperatures of Tang-Bijar Oilfield hot springs located at the Zagros Fold and Thrust Belt of western Iran, including Sr17 (Tang-Hamam) and Tb3 (Tang-Bijar), were estimated by using Quartz (Fournier, 1977) and cation geothermometers (Fournier, 1979; Fournier and Potter, 1979) Na–K–Mg
@inproceedings{paperid:1040856,
author = {Rafighdoust, Yasaman and ECKSTEIN Yoram and Moussavi Harami, Sayyed Reza and Mahboubi, Asadollah and Mahmudy Gharaie, Mohamad Hosein},
title = {GEOTHERMOMETRY OF TWO HOT SPRINGS IN WESTERN IRAN},
booktitle = {The GSA- Southeastern Section - 63rd Annual Meeting - April 2014},
year = {2014},
location = {IRAN},
keywords = {Reservoir temperatures of Tang-Bijar Oilfield hot springs located at the Zagros Fold and Thrust Belt of western Iran; including Sr17
(Tang-Hamam) and Tb3 (Tang-Bijar); were estimated by using Quartz (Fournier; 1977) and cation geothermometers (Fournier; 1979;
Fournier and Potter; 1979) Na–K–Mg triangular diagram (Giggenbach; 1988) and Na–K–Mg–Ca square diagram (Arn?rsson; 2000).
water of Sr17 hot spring suggests either partial equilibration at temperature below 70°C (“immature waters”); or mixing and dilution by
cold recharge water on the upward flow-path to the ground surface. The brackish water of the Tb3 hot spring are seemingly in full
equilibrium (“mature waters”) with the local evaporitic formations at the temperatures between 75 and 100°C.},
}
%0 Conference Proceedings
%T GEOTHERMOMETRY OF TWO HOT SPRINGS IN WESTERN IRAN
%A Rafighdoust, Yasaman
%A ECKSTEIN Yoram
%A Moussavi Harami, Sayyed Reza
%A Mahboubi, Asadollah
%A Mahmudy Gharaie, Mohamad Hosein
%J The GSA- Southeastern Section - 63rd Annual Meeting - April 2014
%D 2014
