FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2891498119> ?p ?o ?g. }

• W2891498119 endingPage "448" @default.
• W2891498119 startingPage "437" @default.
• W2891498119 abstract "Chlorite is one of the most widely developed minerals in propylitic alteration around porphyry deposits and can be used to investigate element transport and enrichment processes during hydrothermal alteration. The Paleozoic Tuwu porphyry Cu deposit (metal reserve: 0.7 Mt Cu @ 0.67%), located in the southern margin of the Central Asian Orogenic Belt, is one of the most economical and largest porphyry Cu deposits in NW China. The Tuwu porphyry Cu deposit comprises an early porphyry Cu mineralization (including potassic, propylitic and phyllic alteration stages) and later overprinting Cu mineralization periods with chlorite found in both. Chlorite from the propylitic zone at Tuwu is geochemically similar to propylitic chlorite in younger Cenozoic porphyry systems, but enriched in Mg and K and depleted in Fe and Al relative to the overprinting chlorite. Scandium, V, Ti and Ga are enriched, and Li, Sr, Mn and Zn are depleted in the Tuwu propylitic chlorite proximal to the orebody, consistent with Cenozoic deposits. Compared with metamorphic chlorite from Proterozoic metamorphic terranes in Australia, Tuwu propylitic chlorite has higher Mg and K, lower Fe, Al and As. Our results suggest propylitic alteration in the Tuwu district is probably the product of cooling of fluids derived from the magmatic-hydrothermal system, but not from peripheral waters, and trace element variations in chlorite are mainly controlled by temperature although other factors such as fault development could affect variation trends. The common elemental features of chlorite in both Paleozoic and Cenozoic porphyry Cu deposits indicate it could act as a potential tool for mineral exploration." @default.
• W2891498119 created "2018-09-27" @default.
• W2891498119 creator A5003497492 @default.
• W2891498119 creator A5035633443 @default.
• W2891498119 creator A5052716256 @default.
• W2891498119 creator A5054917719 @default.
• W2891498119 creator A5056111411 @default.
• W2891498119 creator A5078530516 @default.
• W2891498119 date "2018-11-01" @default.
• W2891498119 modified "2023-10-16" @default.
• W2891498119 title "Element transport and enrichment during propylitic alteration in Paleozoic porphyry Cu mineralization systems: Insights from chlorite chemistry" @default.
• W2891498119 cites W1441895316 @default.
• W2891498119 cites W1853946581 @default.
• W2891498119 cites W1968970602 @default.
• W2891498119 cites W1969761050 @default.
• W2891498119 cites W1987939856 @default.
• W2891498119 cites W1991249933 @default.
• W2891498119 cites W1996236623 @default.
• W2891498119 cites W2015446317 @default.
• W2891498119 cites W2020409799 @default.
• W2891498119 cites W2034533410 @default.
• W2891498119 cites W2035024922 @default.
• W2891498119 cites W2036143042 @default.
• W2891498119 cites W2043966930 @default.
• W2891498119 cites W2082386950 @default.
• W2891498119 cites W2094369922 @default.
• W2891498119 cites W2098118170 @default.
• W2891498119 cites W2098292298 @default.
• W2891498119 cites W2109234433 @default.
• W2891498119 cites W2117584266 @default.
• W2891498119 cites W2121130326 @default.
• W2891498119 cites W2136887969 @default.
• W2891498119 cites W2138822821 @default.
• W2891498119 cites W2153415869 @default.
• W2891498119 cites W2162457106 @default.
• W2891498119 cites W2165394332 @default.
• W2891498119 cites W2169963845 @default.
• W2891498119 cites W2274077492 @default.
• W2891498119 cites W2322075083 @default.
• W2891498119 cites W2336592524 @default.
• W2891498119 cites W2589883011 @default.
• W2891498119 doi "https://doi.org/10.1016/j.oregeorev.2018.09.020" @default.
• W2891498119 hasPublicationYear "2018" @default.
• W2891498119 type Work @default.
• W2891498119 sameAs 2891498119 @default.
• W2891498119 citedByCount "17" @default.
• W2891498119 countsByYear W28914981192019 @default.
• W2891498119 countsByYear W28914981192020 @default.
• W2891498119 countsByYear W28914981192021 @default.
• W2891498119 countsByYear W28914981192022 @default.
• W2891498119 countsByYear W28914981192023 @default.
• W2891498119 crossrefType "journal-article" @default.
• W2891498119 hasAuthorship W2891498119A5003497492 @default.
• W2891498119 hasAuthorship W2891498119A5035633443 @default.
• W2891498119 hasAuthorship W2891498119A5052716256 @default.
• W2891498119 hasAuthorship W2891498119A5054917719 @default.
• W2891498119 hasAuthorship W2891498119A5056111411 @default.
• W2891498119 hasAuthorship W2891498119A5078530516 @default.
• W2891498119 hasBestOaLocation W28914981191 @default.
• W2891498119 hasConcept C111696902 @default.
• W2891498119 hasConcept C127313418 @default.
• W2891498119 hasConcept C145761182 @default.
• W2891498119 hasConcept C151730666 @default.
• W2891498119 hasConcept C156622251 @default.
• W2891498119 hasConcept C159390177 @default.
• W2891498119 hasConcept C159750122 @default.
• W2891498119 hasConcept C165205528 @default.
• W2891498119 hasConcept C17409809 @default.
• W2891498119 hasConcept C179319051 @default.
• W2891498119 hasConcept C2776062231 @default.
• W2891498119 hasConcept C2776152364 @default.
• W2891498119 hasConcept C2776268066 @default.
• W2891498119 hasConcept C2777844515 @default.
• W2891498119 hasConcept C2779870107 @default.
• W2891498119 hasConcept C92720285 @default.
• W2891498119 hasConceptScore W2891498119C111696902 @default.
• W2891498119 hasConceptScore W2891498119C127313418 @default.
• W2891498119 hasConceptScore W2891498119C145761182 @default.
• W2891498119 hasConceptScore W2891498119C151730666 @default.
• W2891498119 hasConceptScore W2891498119C156622251 @default.
• W2891498119 hasConceptScore W2891498119C159390177 @default.
• W2891498119 hasConceptScore W2891498119C159750122 @default.
• W2891498119 hasConceptScore W2891498119C165205528 @default.
• W2891498119 hasConceptScore W2891498119C17409809 @default.
• W2891498119 hasConceptScore W2891498119C179319051 @default.
• W2891498119 hasConceptScore W2891498119C2776062231 @default.
• W2891498119 hasConceptScore W2891498119C2776152364 @default.
• W2891498119 hasConceptScore W2891498119C2776268066 @default.
• W2891498119 hasConceptScore W2891498119C2777844515 @default.
• W2891498119 hasConceptScore W2891498119C2779870107 @default.
• W2891498119 hasConceptScore W2891498119C92720285 @default.
• W2891498119 hasFunder F4320306076 @default.
• W2891498119 hasFunder F4320321133 @default.
• W2891498119 hasLocation W28914981191 @default.
• W2891498119 hasOpenAccess W2891498119 @default.
• W2891498119 hasPrimaryLocation W28914981191 @default.
• W2891498119 hasRelatedWork W194418204 @default.
• W2891498119 hasRelatedWork W1994406246 @default.

• next