FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2155406688> ?p ?o ?g. }

• W2155406688 endingPage "211" @default.
• W2155406688 startingPage "193" @default.
• W2155406688 abstract "Abstract. A huge fluorite deposit at Voznesenka in the Khanka massif, Far East Russia is concluded to have formed at ca. 450 Ma in Late Ordovician time based on the K-Ar ages for Li-micas in the fluorite ore and greisenized leucogranite within the deposit. This conclusion is inconsistent with the current view of Devonian mineralization that stemmed from widely scattered whole-rock Rb-Sr isotope data for the heterogeneous leucogranite stocks influenced by strong alteration. The Voznesenka and neighboring fluorite deposits may have formed in Cambrian limestone in relation to the intrusion of the Li-F-rich felsic magma which has a similar chemistry to representative Li-F-rich felsic rocks including topaz granite and ongonite or topaz rhyolite; these rocks may be classified as a specific group of highly fractionated felsic magmas. Biotite granite plutons exposed in the Voznesenka district are divided in age into two groups based on the CHIME age data for zircon, monazite and xenotime: Ordovician and Permian. The Ordovician plutons seem to be coeval to the fluorite deposits and are characterized by F-rich chemistry, reduced nature and association of tin mineralization with the deposition of fluorite and tourmaline. The biotite granite magmas of initially enhanced F contents could have been highly fractionated to form Li-F-rich leucogranite cupolas that provided fluorite deposits within the host limestone. Future prospecting for similar fluorite deposits is to be focused on areas of intersection between Ordovician Li-F-rich granite and Cambrian carbonate sequences. The Permian granite of southeastern margin of the Grodekovo batholith is characterized by lesser F content, oxidized nature and the lack of tin and fluorite mineralization in contrast to the Ordovician granite. The result of Permian age does not support the current view of Silurian age for the batholith and requires overall chronological reinvestigation in connection with the tectonic history of the Khanka massif because the Grodekovo is a representative of Paleozoic batholiths in Primorie." @default.
• W2155406688 created "2016-06-24" @default.
• W2155406688 creator A5003353836 @default.
• W2155406688 creator A5037166750 @default.
• W2155406688 creator A5041339247 @default.
• W2155406688 creator A5046660088 @default.
• W2155406688 creator A5052526066 @default.
• W2155406688 creator A5076873950 @default.
• W2155406688 creator A5083011256 @default.
• W2155406688 date "2003-09-01" @default.
• W2155406688 modified "2023-10-01" @default.
• W2155406688 title "Fluorite Deposits at Voznesenka in the Khanka Massif, Russia: Geology and Age of Mineralization" @default.
• W2155406688 cites W1496345739 @default.
• W2155406688 cites W1514627894 @default.
• W2155406688 cites W1538725375 @default.
• W2155406688 cites W1976258178 @default.
• W2155406688 cites W2014722475 @default.
• W2155406688 cites W2023926717 @default.
• W2155406688 cites W2025852902 @default.
• W2155406688 cites W2029554065 @default.
• W2155406688 cites W2090450139 @default.
• W2155406688 cites W2098235604 @default.
• W2155406688 cites W2139796115 @default.
• W2155406688 cites W2145604970 @default.
• W2155406688 cites W2152731386 @default.
• W2155406688 cites W2395818744 @default.
• W2155406688 cites W1993283035 @default.
• W2155406688 doi "https://doi.org/10.1111/j.1751-3928.2003.tb00169.x" @default.
• W2155406688 hasPublicationYear "2003" @default.
• W2155406688 type Work @default.
• W2155406688 sameAs 2155406688 @default.
• W2155406688 citedByCount "9" @default.
• W2155406688 countsByYear W21554066882013 @default.
• W2155406688 countsByYear W21554066882016 @default.
• W2155406688 countsByYear W21554066882019 @default.
• W2155406688 countsByYear W21554066882021 @default.
• W2155406688 countsByYear W21554066882022 @default.
• W2155406688 crossrefType "journal-article" @default.
• W2155406688 hasAuthorship W2155406688A5003353836 @default.
• W2155406688 hasAuthorship W2155406688A5037166750 @default.
• W2155406688 hasAuthorship W2155406688A5041339247 @default.
• W2155406688 hasAuthorship W2155406688A5046660088 @default.
• W2155406688 hasAuthorship W2155406688A5052526066 @default.
• W2155406688 hasAuthorship W2155406688A5076873950 @default.
• W2155406688 hasAuthorship W2155406688A5083011256 @default.
• W2155406688 hasBestOaLocation W21554066881 @default.
• W2155406688 hasConcept C111696902 @default.
• W2155406688 hasConcept C120806208 @default.
• W2155406688 hasConcept C127313418 @default.
• W2155406688 hasConcept C151730666 @default.
• W2155406688 hasConcept C159390177 @default.
• W2155406688 hasConcept C159750122 @default.
• W2155406688 hasConcept C160776313 @default.
• W2155406688 hasConcept C167284885 @default.
• W2155406688 hasConcept C171701179 @default.
• W2155406688 hasConcept C172660882 @default.
• W2155406688 hasConcept C17409809 @default.
• W2155406688 hasConcept C178790620 @default.
• W2155406688 hasConcept C185592680 @default.
• W2155406688 hasConcept C192241223 @default.
• W2155406688 hasConcept C193429443 @default.
• W2155406688 hasConcept C25822816 @default.
• W2155406688 hasConcept C26687426 @default.
• W2155406688 hasConcept C2776212575 @default.
• W2155406688 hasConcept C2777081348 @default.
• W2155406688 hasConcept C2777229588 @default.
• W2155406688 hasConcept C2777825866 @default.
• W2155406688 hasConcept C2777980256 @default.
• W2155406688 hasConcept C2778849375 @default.
• W2155406688 hasConcept C2779532088 @default.
• W2155406688 hasConcept C2779870107 @default.
• W2155406688 hasConcept C34122518 @default.
• W2155406688 hasConcept C77928131 @default.
• W2155406688 hasConcept C91442348 @default.
• W2155406688 hasConceptScore W2155406688C111696902 @default.
• W2155406688 hasConceptScore W2155406688C120806208 @default.
• W2155406688 hasConceptScore W2155406688C127313418 @default.
• W2155406688 hasConceptScore W2155406688C151730666 @default.
• W2155406688 hasConceptScore W2155406688C159390177 @default.
• W2155406688 hasConceptScore W2155406688C159750122 @default.
• W2155406688 hasConceptScore W2155406688C160776313 @default.
• W2155406688 hasConceptScore W2155406688C167284885 @default.
• W2155406688 hasConceptScore W2155406688C171701179 @default.
• W2155406688 hasConceptScore W2155406688C172660882 @default.
• W2155406688 hasConceptScore W2155406688C17409809 @default.
• W2155406688 hasConceptScore W2155406688C178790620 @default.
• W2155406688 hasConceptScore W2155406688C185592680 @default.
• W2155406688 hasConceptScore W2155406688C192241223 @default.
• W2155406688 hasConceptScore W2155406688C193429443 @default.
• W2155406688 hasConceptScore W2155406688C25822816 @default.
• W2155406688 hasConceptScore W2155406688C26687426 @default.
• W2155406688 hasConceptScore W2155406688C2776212575 @default.
• W2155406688 hasConceptScore W2155406688C2777081348 @default.
• W2155406688 hasConceptScore W2155406688C2777229588 @default.
• W2155406688 hasConceptScore W2155406688C2777825866 @default.
• W2155406688 hasConceptScore W2155406688C2777980256 @default.
• W2155406688 hasConceptScore W2155406688C2778849375 @default.
• W2155406688 hasConceptScore W2155406688C2779532088 @default.

• next