Geo-genic arsenic contamination in the Kerman Cenozoic Magmatic Arc, Kerman, Iran: Implications for the source identification and regional analysis
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- 作者：Mehdi Khorasanipoura ; khorasani@uk.ac.ir" class="auth_mail" title="E-mail the corresponding author ; khorasani_283@yahoo.com" class="auth_mail" title="E-mail the corresponding author ; Esmat Esmaeilzadehb
- 关键词：Arsenic ; Kerman Cenozoic Magmatic Arc ; Geothermal activities
- 刊名：Applied Geochemistry
- 出版年：2015
- 出版时间：December 2015
- 年：2015
- 卷：63
- 期：Complete
- 页码：610-622
- 全文大小：3803 K
文摘
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Arsenic concentration was investigated in the old and active geothermal indicators.
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Very high arsenic content was measured in the reddish-brown deposits.
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Yukonite, a rare Ca ferric arsenate hydrous mineral, was identified.
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Arsenic concentration in the hydrothermal warm springs ranged from 15,900 to 30,500 μg/L.
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High values of As, B, Cs, Fe, Li, Rb, Sb, Si, and Tl are good fingerprints for geothermal source.