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Mobilization of rhenium in magmatic fluids with implications for its exploration

B2FIND2026-04-25 收录

稀有金属成矿机制

岩浆流体地球化学

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https://b2find.eudat.eu/dataset/2cabd1e1-06f5-5013-96e6-c16988305d38 数据链接链接失效反馈

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Rhenium (Re) is one of the rarest elements on Earth (average abundance < 1 ppb) and is of fundamental importance for our modern high-tech industry due to its high thermal...

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稀有金属成矿机制

岩浆流体地球化学勘探

Rhenium (Re) is one of the rarest elements on Earth (average abundance < 1 ppb) and is of fundamental importance for our modern high-tech industry due to its high thermal stability (melting tempera

DataCite Commons2022-03-11 更新40

Supplementary Table 1-9 of the manuscript: Magmatic Cl-H2O contents, fluid extraction and porphyry fertility: Evidence from zircon and its apatite inclusions

斑岩矿床评价

岩浆流体地球化学

Table DR1 Major element composition of biotite from the three intrusions in the ZOF Table DR2 Laser Raman spectra and trace element compositions of zircon grains from the Cretaceous intrusions in the

NIAID Data Ecosystem00

Mobilization of rhenium in magmatic fluids with implications for its exploration

岩浆流体地球化学

金属勘探

Rhenium (Re) is one of the rarest elements on Earth (average abundance < 1 ppb) and is of fundamental importance for our modern high-tech industry due to its high thermal...

B2FIND00

In-situ XAS measurements as a new approach to probe metal extraction from magmas: Distribution and speciation of Cu in fluid+melt systems

矿床成矿机制

岩浆流体地球化学

The transition to a zero-emission economy requires the access to a growing amount of metals as Cu to construct new energy systems and connect them together. In such context, a better understanding of

ESRF Portal2027-01-01 更新10

Mobilization of rhenium in magmatic fluids with implications for its exploration

稀有金属成矿机制

岩浆流体地球化学

Rhenium (Re) is one of the rarest elements on Earth (average abundance < 1 ppb) and is of fundamental importance for our modern high-tech industry due to its high thermal stability (melting tempera

ESRF Portal2025-01-01 更新00

Mobilization of rhenium in magmatic fluids with implications for its exploration

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