FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019017051> ?p ?o ?g. }

• W2019017051 endingPage "21" @default.
• W2019017051 startingPage "1" @default.
• W2019017051 abstract "Mantle-derived ultramafic rocks commonly occur on the seafloor at slow-spreading axes and are tectonically emplaced along shear zones. Since the early 1990s, a growing number of hydrothermal systems have been detected in ultramafic settings. But chemical data for fluid compositions in active systems are still limited. Besides the Logatchev field at 15°N on the Mid-Atlantic Ridge (MAR), the only other active high-temperature (> 300 °C) hydrothermal field known to be strongly influenced by ultramafics is the Rainbow field at 36°N on the MAR. The field at Logatchev consists of six active vent sites at about 3000 m water depth, situated along a NW–SE-trending line with distances of 50–200 m between the individual sites. The vent sites were mapped in detail and re-sampled during two cruises in 2004 and 2005 using a ROV. The geochemical composition of the hydrothermal fluids is characterized by very high concentrations of dissolved methane and hydrogen (up to 3.5 mM and 19 mM, respectively) related to serpentinization processes in the reaction zone. Together with moderate Si concentrations of 9 mM, a depletion in B compared to seawater and Li concentrations lower than in basaltic systems, this fluid composition has been identified as characteristic signature of high-temperature hydrothermal fluids reacting with ultramafic rocks. However, additional alteration of gabbroic intrusions is likely. The fluid composition is very similar at all vent sites, indicating a common source in the reaction zone and little variation during upflow. Spatial differences in fluid composition were observed between smoking craters and the complex chimney system IRINA II, but are restricted to elements with strong temperature-controlled solubility, as Cu and Co. These differences can be related to different exit temperatures (up to 350 °C and < 300 °C, respectively). Concentrations of rare earth elements, and chondrite-normalized patterns with LREE enrichment and positive Eu anomalies are comparable to those of basaltic-hosted systems, thus indicating minor influence of host-rock composition. A comparison of published fluid composition data from 1996 [Douville, E., Charlou, J.L., Oelkers, E.H., Bienvenu, P., Jove Colon, C.F., Donval, J.P., Fouquet, Y., Prieour, D., Appriou, P., 2002. The Rainbow vent fluids (36°14'N, MAR): the influence of ultramafic rocks and phase separation on trace metal content in Mid-Atlantic Ridge hydrothermal fluids. Chemical Geology, 184: 37–48.] with our own data indicates that the system remained stable over the past nine years. There is no clear indication of phase separation taking place at Logatchev. Mineralogical and chemical composition of the rocks, reaction temperature, and partly sub-seafloor mixing with entraining seawater are supposed to be the main controlling parameters of fluid geochemistry in the Logatchev field. As it is known that more ultramafic-hosted hydrothermal systems exist along slow-spreading ridges, this type of hydrothermal systems might have a significant influence on the elemental budget of the oceans. Detailed information about the fluid geochemistry and its spatial and temporal variations is an important prerequisite for an estimation of elemental fluxes in ultramafic-hosted systems and their relative importance compared to basaltic-hosted systems." @default.
• W2019017051 created "2016-06-24" @default.
• W2019017051 creator A5004061568 @default.
• W2019017051 creator A5011926628 @default.
• W2019017051 creator A5025110431 @default.
• W2019017051 creator A5054957489 @default.
• W2019017051 creator A5064076251 @default.
• W2019017051 date "2007-07-01" @default.
• W2019017051 modified "2023-10-14" @default.
• W2019017051 title "Geochemistry of hydrothermal fluids from the ultramafic-hosted Logatchev hydrothermal field, 15°N on the Mid-Atlantic Ridge: Temporal and spatial investigation" @default.
• W2019017051 cites W1489938111 @default.
• W2019017051 cites W1498138919 @default.
• W2019017051 cites W1534791926 @default.
• W2019017051 cites W1965649232 @default.
• W2019017051 cites W1966983664 @default.
• W2019017051 cites W1967678478 @default.
• W2019017051 cites W1971545711 @default.
• W2019017051 cites W1974234490 @default.
• W2019017051 cites W1976573212 @default.
• W2019017051 cites W1977457396 @default.
• W2019017051 cites W1980279852 @default.
• W2019017051 cites W1981846692 @default.
• W2019017051 cites W1983023133 @default.
• W2019017051 cites W1984232107 @default.
• W2019017051 cites W1990367391 @default.
• W2019017051 cites W2006593586 @default.
• W2019017051 cites W2009701084 @default.
• W2019017051 cites W2017118946 @default.
• W2019017051 cites W2017264474 @default.
• W2019017051 cites W2018359597 @default.
• W2019017051 cites W2030495234 @default.
• W2019017051 cites W2031190434 @default.
• W2019017051 cites W2033804331 @default.
• W2019017051 cites W2034058675 @default.
• W2019017051 cites W2038814991 @default.
• W2019017051 cites W2039066042 @default.
• W2019017051 cites W2040625411 @default.
• W2019017051 cites W2050777681 @default.
• W2019017051 cites W2058604980 @default.
• W2019017051 cites W2065629370 @default.
• W2019017051 cites W2067719049 @default.
• W2019017051 cites W2070087392 @default.
• W2019017051 cites W2071501853 @default.
• W2019017051 cites W2076338250 @default.
• W2019017051 cites W2080083416 @default.
• W2019017051 cites W2081071023 @default.
• W2019017051 cites W2085487206 @default.
• W2019017051 cites W2086145083 @default.
• W2019017051 cites W2087930089 @default.
• W2019017051 cites W2092174737 @default.
• W2019017051 cites W2107710538 @default.
• W2019017051 cites W2108947678 @default.
• W2019017051 cites W2121536019 @default.
• W2019017051 cites W2157256930 @default.
• W2019017051 cites W2162859581 @default.
• W2019017051 cites W2170918707 @default.
• W2019017051 cites W2324550407 @default.
• W2019017051 doi "https://doi.org/10.1016/j.chemgeo.2007.01.023" @default.
• W2019017051 hasPublicationYear "2007" @default.
• W2019017051 type Work @default.
• W2019017051 sameAs 2019017051 @default.
• W2019017051 citedByCount "243" @default.
• W2019017051 countsByYear W20190170512012 @default.
• W2019017051 countsByYear W20190170512013 @default.
• W2019017051 countsByYear W20190170512014 @default.
• W2019017051 countsByYear W20190170512015 @default.
• W2019017051 countsByYear W20190170512016 @default.
• W2019017051 countsByYear W20190170512017 @default.
• W2019017051 countsByYear W20190170512018 @default.
• W2019017051 countsByYear W20190170512019 @default.
• W2019017051 countsByYear W20190170512020 @default.
• W2019017051 countsByYear W20190170512021 @default.
• W2019017051 countsByYear W20190170512022 @default.
• W2019017051 countsByYear W20190170512023 @default.
• W2019017051 crossrefType "journal-article" @default.
• W2019017051 hasAuthorship W2019017051A5004061568 @default.
• W2019017051 hasAuthorship W2019017051A5011926628 @default.
• W2019017051 hasAuthorship W2019017051A5025110431 @default.
• W2019017051 hasAuthorship W2019017051A5054957489 @default.
• W2019017051 hasAuthorship W2019017051A5064076251 @default.
• W2019017051 hasConcept C111368507 @default.
• W2019017051 hasConcept C117485682 @default.
• W2019017051 hasConcept C127313418 @default.
• W2019017051 hasConcept C151730666 @default.
• W2019017051 hasConcept C156622251 @default.
• W2019017051 hasConcept C161509811 @default.
• W2019017051 hasConcept C17409809 @default.
• W2019017051 hasConcept C195081551 @default.
• W2019017051 hasConcept C197248824 @default.
• W2019017051 hasConcept C199289684 @default.
• W2019017051 hasConcept C2778044477 @default.
• W2019017051 hasConcept C32277403 @default.
• W2019017051 hasConcept C67236022 @default.
• W2019017051 hasConceptScore W2019017051C111368507 @default.
• W2019017051 hasConceptScore W2019017051C117485682 @default.
• W2019017051 hasConceptScore W2019017051C127313418 @default.
• W2019017051 hasConceptScore W2019017051C151730666 @default.
• W2019017051 hasConceptScore W2019017051C156622251 @default.

• next