FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2962504080> ?p ?o ?g. }

• W2962504080 endingPage "103012" @default.
• W2962504080 startingPage "103012" @default.
• W2962504080 abstract "Abstract The Zaopa Ag-Mo prospect is located in the Tongbai-Dabie orogenic belt in central China. The orebodies occur as quartz veins and are controlled by secondary faults of the Wushan fault zone in the Suizao area, and hosted by the Zhoulou granite. We document three hydrothermal stages, characterized by albite-quartz-sulfide veins (stage I), quartz-sulfide (stage II) and quartz-fluorite assemblages (stage III), respectively. Silver is mainly found in hessite and galena. There are three types of fluid inclusions in quartz and fluorite including: (1) liquid-rich aqueous fluid inclusions (L + V); (2) aqueous-carbonic fluid inclusions (L + V + CO2); (3) pure carbonic fluid inclusions (pure CO2). Laser Raman spectroscopic analyses indicate the existence of carbon dioxide in the fluid inclusions. The fluid system of the Zaopa Ag-Mo prospect is composed of CO2-NaCl-H2O. The homogenization temperatures of the three stages are 380 to 495 °C, 337 to 404 °C and 246 to 336 °C, respectively. The salinities of the three stages are 11.1–17.5 wt% NaCl eq., 6.7–12.7 wt% NaCl eq. and 1.6–9.9 wt% NaCl eq., respectively. The stage I sulfides (molybdenite, chalcopyrite, pyrite) show a δ34S value around 0‰ (−3.1 to +1.0‰), indicating a magmatic origin. The stage II sulfides (galena, sphalerite, pyrite) also show a δ34S value around 0‰ (−5.7 to +1.6‰), again indicating a magmatic origin. The C-H-O isotope data shows that the fluids of the early stage were derived from a magmatic source, but the fluids of the late stage mixed with meteoric waters. By comparing the characteristics of the Mo deposits in China and those from other countries, we conclude that the Zaopa Ag-Mo prospect is a structurally-controlled magmatic-hydrothermal vein type deposit." @default.
• W2962504080 created "2019-07-23" @default.
• W2962504080 creator A5003123641 @default.
• W2962504080 creator A5011060321 @default.
• W2962504080 creator A5034237279 @default.
• W2962504080 creator A5072264539 @default.
• W2962504080 creator A5082919794 @default.
• W2962504080 date "2019-08-01" @default.
• W2962504080 modified "2023-10-14" @default.
• W2962504080 title "Geological characteristics, fluid inclusions and H-O-C-S isotopes of the Zaopa Ag-Mo prospect in the Suizao area, Hubei Province: Implications for ore genesis" @default.
• W2962504080 cites W1503794001 @default.
• W2962504080 cites W1523531328 @default.
• W2962504080 cites W1946948618 @default.
• W2962504080 cites W1972889465 @default.
• W2962504080 cites W1990065887 @default.
• W2962504080 cites W1992781439 @default.
• W2962504080 cites W2000563553 @default.
• W2962504080 cites W2003454252 @default.
• W2962504080 cites W2012935449 @default.
• W2962504080 cites W2017605458 @default.
• W2962504080 cites W2019115661 @default.
• W2962504080 cites W2019618011 @default.
• W2962504080 cites W2022261706 @default.
• W2962504080 cites W2025046952 @default.
• W2962504080 cites W2028642961 @default.
• W2962504080 cites W2030820013 @default.
• W2962504080 cites W2035422468 @default.
• W2962504080 cites W2040730825 @default.
• W2962504080 cites W2057162185 @default.
• W2962504080 cites W2060279782 @default.
• W2962504080 cites W2063006645 @default.
• W2962504080 cites W2063754919 @default.
• W2962504080 cites W2078320350 @default.
• W2962504080 cites W2090757504 @default.
• W2962504080 cites W2091736416 @default.
• W2962504080 cites W2092386709 @default.
• W2962504080 cites W2112194000 @default.
• W2962504080 cites W2127276558 @default.
• W2962504080 cites W2137470957 @default.
• W2962504080 cites W2143326753 @default.
• W2962504080 cites W2148239728 @default.
• W2962504080 cites W2148957284 @default.
• W2962504080 cites W2165394332 @default.
• W2962504080 cites W2170770997 @default.
• W2962504080 cites W2302531293 @default.
• W2962504080 cites W2336104486 @default.
• W2962504080 cites W2498946149 @default.
• W2962504080 cites W2535177471 @default.
• W2962504080 cites W2548824709 @default.
• W2962504080 cites W2552598186 @default.
• W2962504080 cites W2566476702 @default.
• W2962504080 cites W2744728052 @default.
• W2962504080 doi "https://doi.org/10.1016/j.oregeorev.2019.103012" @default.
• W2962504080 hasPublicationYear "2019" @default.
• W2962504080 type Work @default.
• W2962504080 sameAs 2962504080 @default.
• W2962504080 citedByCount "8" @default.
• W2962504080 countsByYear W29625040802020 @default.
• W2962504080 countsByYear W29625040802022 @default.
• W2962504080 countsByYear W29625040802023 @default.
• W2962504080 crossrefType "journal-article" @default.
• W2962504080 hasAuthorship W2962504080A5003123641 @default.
• W2962504080 hasAuthorship W2962504080A5011060321 @default.
• W2962504080 hasAuthorship W2962504080A5034237279 @default.
• W2962504080 hasAuthorship W2962504080A5072264539 @default.
• W2962504080 hasAuthorship W2962504080A5082919794 @default.
• W2962504080 hasConcept C121332964 @default.
• W2962504080 hasConcept C127313418 @default.
• W2962504080 hasConcept C151730666 @default.
• W2962504080 hasConcept C164304813 @default.
• W2962504080 hasConcept C16674752 @default.
• W2962504080 hasConcept C17409809 @default.
• W2962504080 hasConcept C2776152364 @default.
• W2962504080 hasConcept C2779870107 @default.
• W2962504080 hasConcept C62520636 @default.
• W2962504080 hasConcept C7145564 @default.
• W2962504080 hasConceptScore W2962504080C121332964 @default.
• W2962504080 hasConceptScore W2962504080C127313418 @default.
• W2962504080 hasConceptScore W2962504080C151730666 @default.
• W2962504080 hasConceptScore W2962504080C164304813 @default.
• W2962504080 hasConceptScore W2962504080C16674752 @default.
• W2962504080 hasConceptScore W2962504080C17409809 @default.
• W2962504080 hasConceptScore W2962504080C2776152364 @default.
• W2962504080 hasConceptScore W2962504080C2779870107 @default.
• W2962504080 hasConceptScore W2962504080C62520636 @default.
• W2962504080 hasConceptScore W2962504080C7145564 @default.
• W2962504080 hasFunder F4320314896 @default.
• W2962504080 hasFunder F4320322815 @default.
• W2962504080 hasLocation W29625040801 @default.
• W2962504080 hasOpenAccess W2962504080 @default.
• W2962504080 hasPrimaryLocation W29625040801 @default.
• W2962504080 hasRelatedWork W1972499769 @default.
• W2962504080 hasRelatedWork W2044111838 @default.
• W2962504080 hasRelatedWork W2085504882 @default.
• W2962504080 hasRelatedWork W2603157196 @default.
• W2962504080 hasRelatedWork W2606911601 @default.
• W2962504080 hasRelatedWork W2743036011 @default.
• W2962504080 hasRelatedWork W2809164047 @default.

• next