FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2890132084> ?p ?o ?g. }

• W2890132084 endingPage "312" @default.
• W2890132084 startingPage "300" @default.
• W2890132084 abstract "Abstract The newly-discovered Kaladawan South Zn–Pb–Cu orefield in eastern Altyn Mountains is composed of five Zn–Pb(–Cu) deposits, with the largest one containing 414.4 thousand tonnes (kt) Zn, 265.2 kt Pb and 149.2 kt Cu. Stratiform/lenticular orebodies are hosted by the Ordovician volcanic–sedimentary sequences subjected to greenschist-facies metamorphism. Two major ore-forming stages with significant cross-cutting relationship are identified at Kaladawan South: Stage (I) of the earlier massive, banded, disseminated barite-rich sulfide ores, and Stage (II) of the later polymetallic sulfide–quartz veins with economically less importance. Fluid inclusions (FIs) locked in quartz of Stage I massive sulfide ores are homogenized completely at 226–354 °C with calculated seawater-like salinities of 2.7–4.2 wt% NaCl equiv. These characteristics of ore-forming fluids coupled with ore textures of typical VMS deposits, are interpreted to be originated from the modified seawater by sea-floor volcanic-hydrothermal activities. In compared, the Stage II FIs yielded lower homogenization temperatures ranging 251 °C–357 °C with higher salinities of 0.8–14.4 wt% NaCl equiv. Laser Raman analyses identified large amounts of CO2 ± (CH4–N2) in the hydrothermal fluids of Stage II. The δ18OH2O values (0.5–5.7‰) and δDH2O values of (−68.1‰ to −32.3‰) of Stage II quartz are plotted in the range of metamorphic fluids in the D–O isotopic diagram, which indicating that the CO2-rich and mesothermal fluids are metamorphic-derived. The phlogopite paragenetic in the Stage II polymetallic vein yielded a 40Ar/39Ar plateau age of 435.4 ± 3.9 Ma, similar to the age of the metamorphic muscovite (451.0 ± 4.1 Ma) from the ore-hosting schist. Based on the ore deposit geology, mineral assemblages and fluid geochemistry, the Kaladawan South Zn–Pb–Cu mineralization is attributed to be an Ordovician VMS-type deposit overprinted by the Silurian metamorphic fluids." @default.
• W2890132084 created "2018-09-27" @default.
• W2890132084 creator A5020553835 @default.
• W2890132084 creator A5023034963 @default.
• W2890132084 creator A5059477241 @default.
• W2890132084 date "2018-11-01" @default.
• W2890132084 modified "2023-09-26" @default.
• W2890132084 title "Ore genesis and fluid evolution of the Kaladawan South Zn–Pb–Cu ore field, eastern Altyn Mountains (NW China): Evidence from fluid inclusions, H–O isotopes and geochronology" @default.
• W2890132084 cites W1553244339 @default.
• W2890132084 cites W1601706052 @default.
• W2890132084 cites W1825286268 @default.
• W2890132084 cites W1970798863 @default.
• W2890132084 cites W1975256512 @default.
• W2890132084 cites W1977012688 @default.
• W2890132084 cites W1978207900 @default.
• W2890132084 cites W1986971148 @default.
• W2890132084 cites W1996111419 @default.
• W2890132084 cites W2007004781 @default.
• W2890132084 cites W2013943493 @default.
• W2890132084 cites W2018929516 @default.
• W2890132084 cites W2021904361 @default.
• W2890132084 cites W2022223654 @default.
• W2890132084 cites W2025140431 @default.
• W2890132084 cites W2030987430 @default.
• W2890132084 cites W2031554685 @default.
• W2890132084 cites W2033983122 @default.
• W2890132084 cites W2044537972 @default.
• W2890132084 cites W2044853578 @default.
• W2890132084 cites W2047981750 @default.
• W2890132084 cites W2050956082 @default.
• W2890132084 cites W2053308667 @default.
• W2890132084 cites W2055142051 @default.
• W2890132084 cites W2075901285 @default.
• W2890132084 cites W2078320350 @default.
• W2890132084 cites W2085577696 @default.
• W2890132084 cites W2085802529 @default.
• W2890132084 cites W2087774564 @default.
• W2890132084 cites W2090757504 @default.
• W2890132084 cites W2091178195 @default.
• W2890132084 cites W2094636417 @default.
• W2890132084 cites W2114044449 @default.
• W2890132084 cites W2145604970 @default.
• W2890132084 cites W2149354811 @default.
• W2890132084 cites W2518079165 @default.
• W2890132084 cites W2954335864 @default.
• W2890132084 cites W2980923541 @default.
• W2890132084 cites W3097553647 @default.
• W2890132084 doi "https://doi.org/10.1016/j.oregeorev.2018.09.011" @default.
• W2890132084 hasPublicationYear "2018" @default.
• W2890132084 type Work @default.
• W2890132084 sameAs 2890132084 @default.
• W2890132084 citedByCount "3" @default.
• W2890132084 countsByYear W28901320842019 @default.
• W2890132084 countsByYear W28901320842021 @default.
• W2890132084 countsByYear W28901320842022 @default.
• W2890132084 crossrefType "journal-article" @default.
• W2890132084 hasAuthorship W2890132084A5020553835 @default.
• W2890132084 hasAuthorship W2890132084A5023034963 @default.
• W2890132084 hasAuthorship W2890132084A5059477241 @default.
• W2890132084 hasConcept C121332964 @default.
• W2890132084 hasConcept C127313418 @default.
• W2890132084 hasConcept C151730666 @default.
• W2890132084 hasConcept C156622251 @default.
• W2890132084 hasConcept C164304813 @default.
• W2890132084 hasConcept C166957645 @default.
• W2890132084 hasConcept C17409809 @default.
• W2890132084 hasConcept C191935318 @default.
• W2890132084 hasConcept C202746551 @default.
• W2890132084 hasConcept C2776152364 @default.
• W2890132084 hasConcept C62520636 @default.
• W2890132084 hasConcept C7145564 @default.
• W2890132084 hasConcept C95457728 @default.
• W2890132084 hasConceptScore W2890132084C121332964 @default.
• W2890132084 hasConceptScore W2890132084C127313418 @default.
• W2890132084 hasConceptScore W2890132084C151730666 @default.
• W2890132084 hasConceptScore W2890132084C156622251 @default.
• W2890132084 hasConceptScore W2890132084C164304813 @default.
• W2890132084 hasConceptScore W2890132084C166957645 @default.
• W2890132084 hasConceptScore W2890132084C17409809 @default.
• W2890132084 hasConceptScore W2890132084C191935318 @default.
• W2890132084 hasConceptScore W2890132084C202746551 @default.
• W2890132084 hasConceptScore W2890132084C2776152364 @default.
• W2890132084 hasConceptScore W2890132084C62520636 @default.
• W2890132084 hasConceptScore W2890132084C7145564 @default.
• W2890132084 hasConceptScore W2890132084C95457728 @default.
• W2890132084 hasLocation W28901320841 @default.
• W2890132084 hasOpenAccess W2890132084 @default.
• W2890132084 hasPrimaryLocation W28901320841 @default.
• W2890132084 hasRelatedWork W1972499769 @default.
• W2890132084 hasRelatedWork W2030082480 @default.
• W2890132084 hasRelatedWork W2085970544 @default.
• W2890132084 hasRelatedWork W2518096272 @default.
• W2890132084 hasRelatedWork W2606911601 @default.
• W2890132084 hasRelatedWork W2885960676 @default.
• W2890132084 hasRelatedWork W2981380824 @default.
• W2890132084 hasRelatedWork W3035876681 @default.
• W2890132084 hasRelatedWork W3065513652 @default.
• W2890132084 hasRelatedWork W4283377881 @default.

• next