FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2042549689> ?p ?o ?g. }

• W2042549689 endingPage "69" @default.
• W2042549689 startingPage "59" @default.
• W2042549689 abstract "Abstract The Uchkoshkon tin deposit is one of the largest deposits in the Sn–W Saryjaz ore district of Eastern Kyrgyzstan. The district coincides spatially with the Saryjaz syntaxis, which is the narrowest portion of the South Tien Shan collisional belt. The syntaxis is distinguished by collisional thrust tectonics and postcollisional A-type granite magmatism of Permian age. The Uchkoshkon deposit is in the exocontact zone of a 260-km 2 , 273–279 Ma, ilmenite series, high heat production, biotite granite pluton. A satellite granite stock (400 × 250 m) and an explosive breccia pipe (450 × 150 m), crosscutting the stock, are the central structural features of the deposit area. The main stock, accompanied by Li–F felsite dykes, controlled early-stage Mo–W and Sn–W greisen–stockwork mineralization that surrounds the apical portion of the stock. The breccia pipe postdates the emplacement of the Li–F felsite dykes and greisen–stockwork mineralization. The pipe is rooted in main pluton and has been traced by a borehole to a depth of 800 m. The breccia was injected by a swarm of tree-like branching dykes with diffuse contours consisting of K- and B-rich rhyolite porphyry cementing the breccia fragments. The main breccia body has been intruded by a much smaller (150 × 100 m) hydrothermal breccia pipe with quartz–tourmaline matrix, which immediately preceded main-stage lode mineralization. The majority of the lodes occur outside the breccia pipe within a zone of pervasive scapolitization that surrounds the main pluton. The main-stage lodes are represented by quartz–tourmaline–cassiterite veins with minor sulfides, which occupy a series of steeply-dipping, near-parallel, north–northeast-trending shear fractures that are related to postcollisional strike-slip tectonics. Where quartz–tourmaline–cassiterite veins crosscut moderately-dipping skarn deposits, the latter are commercially mineralized with cassiterite, nordenskioldine and borosilicate minerals. The formation of both explosive breccia and main-stage lode mineralization was related to the evolution of B- and H 2 O-rich residual magma deep within the main pluton. The suggested formation model of the Uchkoshkon tin deposit is generally applicable to other major Sn- and Sn–W deposits in the Saryjaz ore district." @default.
• W2042549689 created "2016-06-24" @default.
• W2042549689 creator A5021122438 @default.
• W2042549689 creator A5061696152 @default.
• W2042549689 creator A5084266584 @default.
• W2042549689 date "2012-02-01" @default.
• W2042549689 modified "2023-09-27" @default.
• W2042549689 title "Geology and mineralization of the Uchkoshkon tin deposit associated with a breccia pipe, Eastern Kyrgyzstan" @default.
• W2042549689 cites W1990747960 @default.
• W2042549689 cites W1999553949 @default.
• W2042549689 cites W1999862911 @default.
• W2042549689 cites W2009360266 @default.
• W2042549689 cites W2017174306 @default.
• W2042549689 cites W2023328218 @default.
• W2042549689 cites W2043980138 @default.
• W2042549689 cites W2046421632 @default.
• W2042549689 cites W2064802425 @default.
• W2042549689 cites W2073163433 @default.
• W2042549689 cites W2074463495 @default.
• W2042549689 cites W2083073541 @default.
• W2042549689 cites W2123874618 @default.
• W2042549689 cites W2130620795 @default.
• W2042549689 cites W2328584152 @default.
• W2042549689 doi "https://doi.org/10.1016/j.oregeorev.2011.09.001" @default.
• W2042549689 hasPublicationYear "2012" @default.
• W2042549689 type Work @default.
• W2042549689 sameAs 2042549689 @default.
• W2042549689 citedByCount "13" @default.
• W2042549689 countsByYear W20425496892014 @default.
• W2042549689 countsByYear W20425496892015 @default.
• W2042549689 countsByYear W20425496892018 @default.
• W2042549689 countsByYear W20425496892019 @default.
• W2042549689 countsByYear W20425496892021 @default.
• W2042549689 countsByYear W20425496892022 @default.
• W2042549689 countsByYear W20425496892023 @default.
• W2042549689 crossrefType "journal-article" @default.
• W2042549689 hasAuthorship W2042549689A5021122438 @default.
• W2042549689 hasAuthorship W2042549689A5061696152 @default.
• W2042549689 hasAuthorship W2042549689A5084266584 @default.
• W2042549689 hasConcept C111696902 @default.
• W2042549689 hasConcept C127313418 @default.
• W2042549689 hasConcept C159390177 @default.
• W2042549689 hasConcept C159750122 @default.
• W2042549689 hasConcept C16674752 @default.
• W2042549689 hasConcept C17409809 @default.
• W2042549689 hasConcept C191897082 @default.
• W2042549689 hasConcept C192562407 @default.
• W2042549689 hasConcept C525849907 @default.
• W2042549689 hasConcept C62074269 @default.
• W2042549689 hasConceptScore W2042549689C111696902 @default.
• W2042549689 hasConceptScore W2042549689C127313418 @default.
• W2042549689 hasConceptScore W2042549689C159390177 @default.
• W2042549689 hasConceptScore W2042549689C159750122 @default.
• W2042549689 hasConceptScore W2042549689C16674752 @default.
• W2042549689 hasConceptScore W2042549689C17409809 @default.
• W2042549689 hasConceptScore W2042549689C191897082 @default.
• W2042549689 hasConceptScore W2042549689C192562407 @default.
• W2042549689 hasConceptScore W2042549689C525849907 @default.
• W2042549689 hasConceptScore W2042549689C62074269 @default.
• W2042549689 hasLocation W20425496891 @default.
• W2042549689 hasOpenAccess W2042549689 @default.
• W2042549689 hasPrimaryLocation W20425496891 @default.
• W2042549689 hasRelatedWork W2042549689 @default.
• W2042549689 hasRelatedWork W2063950367 @default.
• W2042549689 hasRelatedWork W2107033963 @default.
• W2042549689 hasRelatedWork W2153085275 @default.
• W2042549689 hasRelatedWork W2166567858 @default.
• W2042549689 hasRelatedWork W2352710904 @default.
• W2042549689 hasRelatedWork W2782398914 @default.
• W2042549689 hasRelatedWork W2996184140 @default.
• W2042549689 hasRelatedWork W3009025095 @default.
• W2042549689 hasRelatedWork W53892999 @default.
• W2042549689 hasVolume "44" @default.
• W2042549689 isParatext "false" @default.
• W2042549689 isRetracted "false" @default.
• W2042549689 magId "2042549689" @default.
• W2042549689 workType "article" @default.