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Late-stage petroleum fluids are characterized by a yellow color under UV-epifluorescence microscopy, and late-stage, aqueous-fluid inclusions are mainly homogenized between 85 and 135 °C, with salinities ranging from 2.0 to 8.0 wt% NaCl equiv.
Early-stage petroleum fluids are characterized by a blue-white color under UV-epifluorescence microscopy, and early-stage aqueous fluid inclusions are mainly homogenized between 54 and 102 °C, with salinities ranging from 12.0 to 16.7 wt% NaCl equiv.
The vent fluids are characterized by a high concentration of (up to 17 mM) and Fe (Iron), but low in sulfide.
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Herschel Bulkley fluids are characterized by an yield value which leads to the formation of a rigid core in the flow region.
Felsic rock-hosted hydrothermal fluids are characterized by relatively low pH and enrichment in H2S, CO2, K, Mn, and Fe compared to mafic rock-hosted fluids (Figure 2).
In particular, ABA hydrothermal fluids are characterized by large variations in chemical composition (Ishibashi and Urabe 1995; Gamo et al. 2006).
Ultramafic rocks Compared with hydrothermal fluids in mafic rock-hosted systems, ultramafic rock-associated hydrothermal fluids are characterized by conspicuous enrichment in H2 in the presence or absence of phase separation processes (Figure 2).
Newtonian fluids are characterized by constant viscosity when external forces change.
As allanite and monazite preferentially incorporate Th over U (Klimm et al. 2008; Skora and Blundy 2012; Stepanov et al. 2012), the coexisting fluid is characterized by a relative enrichment of U over Th (Figure 2).
The resulting equivalent fluid is characterized by an equivalent velocity and an equivalent pressure both defined in the whole domain.
However, examples of hydrothermal systems for this comparison were still scarce; thus, only microbial populations in chimney habitats adjacent to high-temperature hydrothermal fluids were characterized by quantitative cultivation techniques and included.
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