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Crystal chemistry and partitioning of halogens in hydrous silicates
Understanding how halogens are distributed among usual hydrous silicates in the lithosphere is important to constrain their deep geochemical cycle...
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Halogens in serpentinised-troctolites from the Atlantis Massif: implications for alteration and global volatile cycling
The concentrations of halogens in serpentinised olivine-rich lithologies in the lower oceanic crust (e.g. troctolites and wehrlites)...
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The stability of antigorite in subduction zones revisited: the effect of F on antigorite stability and its breakdown reactions at high pressures and high temperatures, with implications for the geochemical cycles of halogens
We present new experimental data on the effect of F on the stability of antigorite and its breakdown products at high pressures (2–6 GPa) and high...
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Textural and compositional variation of mica from the Dexing porphyry Cu deposit: constraints on the behavior of halogens in porphyry systems
The Dexing porphyry deposit is the largest porphyry Cu–Mo–Au deposit in South China. Biotite composition can record the physicochemical conditions...
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Volcanic forcing of high-latitude Northern Hemisphere eruptions
High-latitude explosive volcanic eruptions can cause substantial hemispheric cooling. Here, we use a whole-atmosphere chemistry-climate model to...
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Fluorine and Iodine in Soils of the Kulunda Plain
AbstractThe content and distribution of fluorine (F) and iodine (I) have been studied by the example of four soils on the terrace of Kuchuk Lake in...
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Fluids and physicochemical properties and processes in the Earth
The Earth's fluid budget is dominated by species in the system C–O–H–N–S together with halogens such as F and Cl. H 2 O is by far the most abundant....
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Geochemical characteristics of fluorine- and chlorine-bearing biotite from Tusham Ring Complex, NW India: Constraints on halogen distribution and geodynamic evolution
AbstractThe present study is carried out to understand the factors controlling halogens present in biotites, role of halogens in metallogeny in...
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Substantial halogenated organic chemicals stored in permafrost soils on the Tibetan Plateau
Permafrost in the polar regions potentially stores large amounts of toxic chemicals, including organic compounds bound with halogens. The release of...
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Trace Element Composition of Beryl From the Sherlovaya Gora Deposit, Southeastern Transbaikal Region, Russia
AbstractThe trace element distribution (including water and halogens) has been studied for the first time using SIMS techniques, in two different...
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Fractional degassing of S, Cl and F from basalt magma in the Bárðarbunga rift zone, Iceland
The composition of gas emitted from a volcano producing basalt magma can vary during an eruption and according to the volcano-tectonic setting of the...
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Metal budget and origin of aqueous brines depositing deep-seated Zn-Pb mineralization linked to hydrocarbon reservoirs, North German Basin
The origin, evolution, and interplay of brine and hydrocarbon fluid systems play a crucial role in the formation of deep sediment-hosted base metal...
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Halogens in Chondritic Meteorites
We review the abundances, distributions and isotopic compositions of halogens in chondritic meteorites and discuss formation of the mineral and other...
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Insights into volcanic hazards and plume chemistry from multi-parameter observations: the eruptions of Fimmvörðuháls and Eyjafjallajökull (2010) and Holuhraun (2014–2015)
The eruptions of Eyjafjallajökull volcano in 2010 (including its initial effusive phase at Fimmvörðuháls and its later explosive phase from the...
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Neoproterozoic Felsic Volcano-plutonic Rocks, Tusham Ring Complex, Malani Igneous Suite, NW Indian Shield: Petrogenetic Modeling, Magmatic Source and Geodynamic Evolution
AbstractThis paper reports petrogenetic modelling and geodynamic evolution of felsic volcano-plutonic rocks of Riwasa and Nigana areas from Tusham...
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The Behavior of Halogens During Subduction-Zone Processes
Halogens (Cl, F, I, Br) are enriched in surface reservoirs compared to the mantle. The subduction of these reservoirs in the form of sedimentary pore...
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Halogens in High-Grade Metamorphism
This chapter reviews factors, which control the distribution of the two major halogens, F and Cl, in high-grade metamorphic rocks; their...
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Halogens in Mafic and Intermediate-Silica Content Magmas
As volatile and variably mobile components, halogens play key roles in magmatic, metasomatic, mineralizing, and volcanic processes by influencing the...
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The Development of Water Protection Requirements from the Point of View of Waterworks, with Emphasis on 30 Years of the Memorandum of the International Association of Waterworks in the River Rhine Catchment Area (IAWR)
The International Association of Waterworks in the River Rhine Catchment Area (IAWR) defined water protection requirements for surface water that...