FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2071241185> ?p ?o ?g. }

• W2071241185 endingPage "376" @default.
• W2071241185 startingPage "359" @default.
• W2071241185 abstract "Abstract: The skarns and genesis were studied of the Huanggang Fe-Sn deposit and the nearby Sumugou Zn-Pb deposit in Inner Mongolia, China. In the Huanggang mine, Nos. 1 to 4 Fe ore bodies are arranged along a calcareous horizon from proximal to distal in this order to a granite intrusion named Luotuochangliang, while Sn ore body is situated near another granite intrusion named 204. According to the distance from the granitic intrusions, mineral assemblages in skarns are systematically changed. Garnet is the most predominant skarn mineral throughout the deposit. Hastingsitic amphiboles, however, predominate in the proximal skarns. Fluorite is common in the proximal skarns, while instead calcite is common in the distal skarns. Chlorite is characteristically present only in No. 3 ore body, and chlorite geothermometry gives near 300C for the mineralization of later stage. When garnet crystal shows zonal structure, isotropic andraditic garnet occupies the core, and is surrounded with anisotropic less-andraditic garnet. The presence of white skarn along the boundary between main skarns and host sedimentary rocks confirms relatively reducing environment prevailing as a whole in the studied area. However, the compositional relation between coexisting garnet and clinopyroxene demonstrates that relatively oxidizing condition was achieved for garnet skarn and magnetite ore in the distal, Nos. 2 to 4 Fe ore bodies and Sumugou deposit, compared to that for garnet skarn in the proximal, No. 1 and Sn ore bodies. Preliminary study on the tin content of garnets in the studied area revealed a certain degree of contribution brought from granitic intrusives since the early stage of skarn formation, irrespective of proximal or distal. Oxygen isotope study on garnet, magnetite, quartz and skarn calcite, as well as hydrogen isotope study on hastingsitic amphibole, demonstrates mainly meteoric water origin for the skarn– and ore-forming solutions. The occurrence of Sn, W, Mo and F minerals indicates that those elements were mainly supplied to the deposit later than the formation of skarns and iron ores, overlapping to them. These constraints allow to delineate the formation model of the deposit as follows (Fig. 10): At the time of late Jurassic to early Cretaceous, felsic activity occurred in this region as a part of Yanshanian magmatism, and formed granitic intrusions as well as thick volcanic piles on the surface. The circulation of meteoric water was provoked by the heat brought by the intrusions. By this circulation, much amount of iron was extracted from andesites of the Dashizhai Formation, and precipitated as skarns and magnetite ores along calcareous horizons near the bottom of the Huanggangliang Formation. Subsequently, volatile-rich fluids with Sn, W and Mo were expelled from the solidifying granitic magmas, and precipitated these metals in the pre-existing skarns and ores." @default.
• W2071241185 created "2016-06-24" @default.
• W2071241185 creator A5046047064 @default.
• W2071241185 creator A5059639936 @default.
• W2071241185 creator A5061498578 @default.
• W2071241185 date "2001-12-01" @default.
• W2071241185 modified "2023-09-26" @default.
• W2071241185 title "Skarns and Genesis of the Huanggang Fe-Sn Deposit, Inner Mongolia, China" @default.
• W2071241185 cites W1970169451 @default.
• W2071241185 cites W1970267158 @default.
• W2071241185 cites W1970658925 @default.
• W2071241185 cites W1972567498 @default.
• W2071241185 cites W1977870256 @default.
• W2071241185 cites W1996361224 @default.
• W2071241185 cites W2017934677 @default.
• W2071241185 cites W2017938841 @default.
• W2071241185 cites W2023198501 @default.
• W2071241185 cites W2046079925 @default.
• W2071241185 cites W2047660877 @default.
• W2071241185 cites W2052848232 @default.
• W2071241185 cites W2057237118 @default.
• W2071241185 cites W2073149430 @default.
• W2071241185 cites W2075687401 @default.
• W2071241185 cites W2081461486 @default.
• W2071241185 cites W2087362485 @default.
• W2071241185 cites W2106537927 @default.
• W2071241185 cites W2106839923 @default.
• W2071241185 cites W2108018437 @default.
• W2071241185 cites W2114041810 @default.
• W2071241185 cites W2124888361 @default.
• W2071241185 cites W2126991183 @default.
• W2071241185 cites W2148592038 @default.
• W2071241185 cites W2152553509 @default.
• W2071241185 cites W2166184943 @default.
• W2071241185 cites W2261187686 @default.
• W2071241185 cites W4243196258 @default.
• W2071241185 doi "https://doi.org/10.1111/j.1751-3928.2001.tb00108.x" @default.
• W2071241185 hasPublicationYear "2001" @default.
• W2071241185 type Work @default.
• W2071241185 sameAs 2071241185 @default.
• W2071241185 citedByCount "21" @default.
• W2071241185 countsByYear W20712411852012 @default.
• W2071241185 countsByYear W20712411852014 @default.
• W2071241185 countsByYear W20712411852015 @default.
• W2071241185 countsByYear W20712411852016 @default.
• W2071241185 countsByYear W20712411852017 @default.
• W2071241185 countsByYear W20712411852018 @default.
• W2071241185 countsByYear W20712411852019 @default.
• W2071241185 countsByYear W20712411852020 @default.
• W2071241185 countsByYear W20712411852021 @default.
• W2071241185 countsByYear W20712411852022 @default.
• W2071241185 crossrefType "journal-article" @default.
• W2071241185 hasAuthorship W2071241185A5046047064 @default.
• W2071241185 hasAuthorship W2071241185A5059639936 @default.
• W2071241185 hasAuthorship W2071241185A5061498578 @default.
• W2071241185 hasBestOaLocation W20712411851 @default.
• W2071241185 hasConcept C111696902 @default.
• W2071241185 hasConcept C127313418 @default.
• W2071241185 hasConcept C151730666 @default.
• W2071241185 hasConcept C156622251 @default.
• W2071241185 hasConcept C159390177 @default.
• W2071241185 hasConcept C159750122 @default.
• W2071241185 hasConcept C165205528 @default.
• W2071241185 hasConcept C17409809 @default.
• W2071241185 hasConcept C191897082 @default.
• W2071241185 hasConcept C192562407 @default.
• W2071241185 hasConcept C195843664 @default.
• W2071241185 hasConcept C199289684 @default.
• W2071241185 hasConcept C2776152364 @default.
• W2071241185 hasConcept C2776432453 @default.
• W2071241185 hasConcept C2777844515 @default.
• W2071241185 hasConcept C2778357522 @default.
• W2071241185 hasConcept C2779870107 @default.
• W2071241185 hasConcept C4992710 @default.
• W2071241185 hasConcept C7145564 @default.
• W2071241185 hasConceptScore W2071241185C111696902 @default.
• W2071241185 hasConceptScore W2071241185C127313418 @default.
• W2071241185 hasConceptScore W2071241185C151730666 @default.
• W2071241185 hasConceptScore W2071241185C156622251 @default.
• W2071241185 hasConceptScore W2071241185C159390177 @default.
• W2071241185 hasConceptScore W2071241185C159750122 @default.
• W2071241185 hasConceptScore W2071241185C165205528 @default.
• W2071241185 hasConceptScore W2071241185C17409809 @default.
• W2071241185 hasConceptScore W2071241185C191897082 @default.
• W2071241185 hasConceptScore W2071241185C192562407 @default.
• W2071241185 hasConceptScore W2071241185C195843664 @default.
• W2071241185 hasConceptScore W2071241185C199289684 @default.
• W2071241185 hasConceptScore W2071241185C2776152364 @default.
• W2071241185 hasConceptScore W2071241185C2776432453 @default.
• W2071241185 hasConceptScore W2071241185C2777844515 @default.
• W2071241185 hasConceptScore W2071241185C2778357522 @default.
• W2071241185 hasConceptScore W2071241185C2779870107 @default.
• W2071241185 hasConceptScore W2071241185C4992710 @default.
• W2071241185 hasConceptScore W2071241185C7145564 @default.
• W2071241185 hasIssue "4" @default.
• W2071241185 hasLocation W20712411851 @default.
• W2071241185 hasOpenAccess W2071241185 @default.
• W2071241185 hasPrimaryLocation W20712411851 @default.

• next