Tracing fluid migration pathways in the root zone below unconformity-related hydrothermal veins: Insights from trace element systematics of individual fluid inclusions
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- 作者：Mathias Burischa ; mathias.burisch@ifg.uni-tuebingen.de" class="auth_mail" title="E-mail the corresponding author ; Benjamin F. Waltera ; Markus Wä ; lleb ; Gregor Markla
- 关键词：Ore mineralization ; Fluid mixing ; Rb/Cs ; Clay formation ; Alteration ; Water&ndash ; rock interaction
- 刊名：Chemical Geology
- 出版年：2016
- 出版时间：1 July 2016
- 年：2016
- 卷：429
- 期：Complete
- 页码：44-50
- 全文大小：999 K
文摘
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Temporarily and spatially resolved LA-ICPMS study of individual fluid inclusions
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Temporal and chemical evolution of fracture root zones below hydrothermal veins
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The evolution of dynamic fracture systems shows distinct cyclicality in their fluid chemistry.
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Ore deposition, primarily occurs at the beginning of these cycles.
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Ore formation is promoted by dynamic fracture systems, in which new fracture branches are established abundantly.