New boron isotopic evidence for sedimentary and magmatic fluid influence in the shallow hydrothermal vent system of Milos Island (Aegean Sea, Greece)
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- 作者：Shein-Fu Wua ; b ; sheinfuwu@ntu.edu.tw" class="auth_mail" title="E-mail the corresponding author ; Chen-Feng Youa ; cfy20@mail.ncku.edu.tw" class="auth_mail" title="E-mail the corresponding author ; Yen-Po Lina ; 1 ; Eugenia Valsami-Jonesc ; Emmanuel Baltatzisd
- 关键词：Hydrothermal system ; Boron isotope ; Water/rock interaction ; Magmatic fluids ; Milos
- 刊名：Journal of Volcanology and Geothermal Research
- 出版年：2016
- 出版时间：15 January 2016
- 年：2016
- 卷：310
- 期：Complete
- 页码：58-71
- 全文大小：1278 K
文摘
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High-Cl and low-Cl fluids with high B/Cl and distinct low δ11B were detected at Milos.
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Sediment/magmatic fluids contributions play important role in vent fluid chemistry.
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B isotopes and Br/I/Cl ratios support slab-derived addition in Milos parent magma.
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Deep water reservoirs were affected by magmatic volatiles via slab-derived processes.