Matches in SemOpenAlex for { <https://semopenalex.org/work/W4313390839> ?p ?o ?g. }
Showing items 1 to 73 of
73
with 100 items per page.
- W4313390839 endingPage "11" @default.
- W4313390839 startingPage "1" @default.
- W4313390839 abstract "Typically, granitic intrusions that document the lengthy and intricate history of the magmatic-hydrothermal system are linked to tungsten deposits. Uncertainty persists about the genetic relationship between tungsten mineralization and magmatic-hydrothermal development. The primary tungsten deposit in the Dai Tu region, known as the Nui Phao deposit, has been the subject of a petrographical and microscopic examination. Tungsten mineralization in the Dai Tu area often occurs in association with the formation of skarn and greisen bodies, and it has drawn much attention from geoscientists. Based on microscopic observations, tungsten ores can be divided into three mineralization stages, namely skarnisation, greisenization, and hydrothermal stage. To examine the geochemical features of the tungsten ores, the SEM-EDS and Microscope analytical methods were performed in this study. Research results indicate that the Nui Phao tungsten deposit was formed due to different tectonic and magmatism episodes. Accordingly, the Nui Phao tungsten deposit is relatively complicated with the multi-sources of ore components. Most of the tungsten ore was accumulated in association with the metasomatism between the Ordovician-Silurian carbonate-terrigenous sedimentary rocks of the Phu Ngu formation and the Cretaceous two-mica granite of the Pia Oac complex. The research results indicate that tungsten resources obtained at levels 122 and 333 are about 227.6 thousand tons. Moreover, the hydrothermal alteration and metasomatism in the study area are influenced by at least three metasomatic episodes, including skarnisation, greisenisation, and the late hydrothermal alteration of medium to a low temperature that is genetically related to fluorite-polymetallic mineralization." @default.
- W4313390839 created "2023-01-06" @default.
- W4313390839 creator A5016581890 @default.
- W4313390839 creator A5039685599 @default.
- W4313390839 creator A5055887961 @default.
- W4313390839 creator A5074614412 @default.
- W4313390839 date "2022-12-31" @default.
- W4313390839 modified "2023-10-02" @default.
- W4313390839 title "Mineralogical and geological characteristics of the Nui Phao tungsten deposit and its resource in the Dai Tu area, northeastern Vietnam" @default.
- W4313390839 doi "https://doi.org/10.46326/jmes.2022.63(6).01" @default.
- W4313390839 hasPublicationYear "2022" @default.
- W4313390839 type Work @default.
- W4313390839 citedByCount "0" @default.
- W4313390839 crossrefType "journal-article" @default.
- W4313390839 hasAuthorship W4313390839A5016581890 @default.
- W4313390839 hasAuthorship W4313390839A5039685599 @default.
- W4313390839 hasAuthorship W4313390839A5055887961 @default.
- W4313390839 hasAuthorship W4313390839A5074614412 @default.
- W4313390839 hasBestOaLocation W43133908391 @default.
- W4313390839 hasConcept C111696902 @default.
- W4313390839 hasConcept C127313418 @default.
- W4313390839 hasConcept C151730666 @default.
- W4313390839 hasConcept C156622251 @default.
- W4313390839 hasConcept C159390177 @default.
- W4313390839 hasConcept C159750122 @default.
- W4313390839 hasConcept C167919410 @default.
- W4313390839 hasConcept C17409809 @default.
- W4313390839 hasConcept C191897082 @default.
- W4313390839 hasConcept C192562407 @default.
- W4313390839 hasConcept C195843664 @default.
- W4313390839 hasConcept C2776152364 @default.
- W4313390839 hasConcept C2777980256 @default.
- W4313390839 hasConcept C37282123 @default.
- W4313390839 hasConcept C542268612 @default.
- W4313390839 hasConcept C67236022 @default.
- W4313390839 hasConcept C7145564 @default.
- W4313390839 hasConceptScore W4313390839C111696902 @default.
- W4313390839 hasConceptScore W4313390839C127313418 @default.
- W4313390839 hasConceptScore W4313390839C151730666 @default.
- W4313390839 hasConceptScore W4313390839C156622251 @default.
- W4313390839 hasConceptScore W4313390839C159390177 @default.
- W4313390839 hasConceptScore W4313390839C159750122 @default.
- W4313390839 hasConceptScore W4313390839C167919410 @default.
- W4313390839 hasConceptScore W4313390839C17409809 @default.
- W4313390839 hasConceptScore W4313390839C191897082 @default.
- W4313390839 hasConceptScore W4313390839C192562407 @default.
- W4313390839 hasConceptScore W4313390839C195843664 @default.
- W4313390839 hasConceptScore W4313390839C2776152364 @default.
- W4313390839 hasConceptScore W4313390839C2777980256 @default.
- W4313390839 hasConceptScore W4313390839C37282123 @default.
- W4313390839 hasConceptScore W4313390839C542268612 @default.
- W4313390839 hasConceptScore W4313390839C67236022 @default.
- W4313390839 hasConceptScore W4313390839C7145564 @default.
- W4313390839 hasIssue "6" @default.
- W4313390839 hasLocation W43133908391 @default.
- W4313390839 hasOpenAccess W4313390839 @default.
- W4313390839 hasPrimaryLocation W43133908391 @default.
- W4313390839 hasRelatedWork W150648257 @default.
- W4313390839 hasRelatedWork W2061356723 @default.
- W4313390839 hasRelatedWork W2062141614 @default.
- W4313390839 hasRelatedWork W2089400418 @default.
- W4313390839 hasRelatedWork W231444770 @default.
- W4313390839 hasRelatedWork W2353831719 @default.
- W4313390839 hasRelatedWork W2380821166 @default.
- W4313390839 hasRelatedWork W2385713861 @default.
- W4313390839 hasRelatedWork W2791236146 @default.
- W4313390839 hasRelatedWork W4319984619 @default.
- W4313390839 hasVolume "63" @default.
- W4313390839 isParatext "false" @default.
- W4313390839 isRetracted "false" @default.
- W4313390839 workType "article" @default.