FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W162590092> ?p ?o ?g. }

• W162590092 abstract "At the request of the Bureau of Land Management, the U.S. Geological Survey assessed the Lake Valley Area of Critical Environmental Concern (ACEC), which includes the historic Lake Valley townsite and silver-manganese mining district, for undiscovered mineral resources. The Lake Valley ACEC is along the southeastern margin of the Black Range of western Sierra County, New Mexico. The Black Range contains eleven mining districts from which silver, lead, zinc, manganese, copper, gold, and tin have been recovered. As part of the study, an area of over 75 square mi (195 square km) in the area of the Lake Valley ACEC was mapped to understand ore controls and to assess mineral-resource potential. Lake Valley mining district is in Mississippian Lake Valley Formation carbonate rocks, but much of the surrounding terrane consists of volcanic rocks on the southeastern edge of the Emory cauldron which formed about 34.9 Ma. Volcanic rocks are part of the Mogollon-Datil volcanic province which include flows, breccias, ash-flow tuffs, and intrusive rhyolites. The Lake Valley mining district is located about 20 mi (32 km) south of the Late Cretaceous Laramide copper-gold porphyry intrusion at Hillsboro. It is also located at the western boundary of the Rio Grande rift basin.The Lake Valey fault is the major structural feature of the study area. Geological and geophysical data suggest the fault is composed of two segments: a southern, northwest-striking segment that may have a pre-Tertiary history and a northerly-striking segment that is part of the Emory cauldron ring fracture. The mining district is bounded by the southern, northwest-striking segment of the fault which may have up to 800 ft (240m) of normal offset. Deposit types identified in the Black Range, and for which we assess mineral potential, are Laramide porphyry, Laramide skarns, Laramide veins, gold placer, carbonate-hosted, volcanic-epithermal, and rhyolite tin; no Rio Grande Rift baritefluorite-galena deposits are known, but they are included in the assessment. The most likely deposits to be discovered in the Lake Valley district are carbonate-hosted silver-manganese deposits. These deposits could be deposited by hydrothermal fluids or be related to intrusion of Oligocene rhyolite or Laramide porphyry. An aeromagnetic high south of the district probably reflects a small felsic intrusion of unknown age. We assess the Lake Valley ACEC as having low to moderate potential for undiscovered carbonate-hosted deposits associated with volcanic rocks or Laramide porphyry plutons, and low potential for gold placer and rhyolite tin deposits." @default.
• W162590092 created "2016-06-24" @default.
• W162590092 creator A5002426575 @default.
• W162590092 creator A5008826233 @default.
• W162590092 creator A5015381102 @default.
• W162590092 creator A5017153831 @default.
• W162590092 creator A5045816458 @default.
• W162590092 creator A5057093301 @default.
• W162590092 creator A5066089927 @default.
• W162590092 creator A5077932061 @default.
• W162590092 date "1998-01-01" @default.
• W162590092 modified "2023-09-23" @default.
• W162590092 title "Geology and mineral resources of the Lake Valley area, Sierra County, New Mexico" @default.
• W162590092 doi "https://doi.org/10.3133/ofr98347" @default.
• W162590092 hasPublicationYear "1998" @default.
• W162590092 type Work @default.
• W162590092 sameAs 162590092 @default.
• W162590092 citedByCount "0" @default.
• W162590092 crossrefType "journal-article" @default.
• W162590092 hasAuthorship W162590092A5002426575 @default.
• W162590092 hasAuthorship W162590092A5008826233 @default.
• W162590092 hasAuthorship W162590092A5015381102 @default.
• W162590092 hasAuthorship W162590092A5017153831 @default.
• W162590092 hasAuthorship W162590092A5045816458 @default.
• W162590092 hasAuthorship W162590092A5057093301 @default.
• W162590092 hasAuthorship W162590092A5066089927 @default.
• W162590092 hasAuthorship W162590092A5077932061 @default.
• W162590092 hasBestOaLocation W1625900921 @default.
• W162590092 hasConcept C109007969 @default.
• W162590092 hasConcept C114793014 @default.
• W162590092 hasConcept C120806208 @default.
• W162590092 hasConcept C126457475 @default.
• W162590092 hasConcept C127313418 @default.
• W162590092 hasConcept C150999391 @default.
• W162590092 hasConcept C151730666 @default.
• W162590092 hasConcept C16674752 @default.
• W162590092 hasConcept C17409809 @default.
• W162590092 hasConcept C175551986 @default.
• W162590092 hasConcept C192241223 @default.
• W162590092 hasConcept C2778471503 @default.
• W162590092 hasConcept C2778697265 @default.
• W162590092 hasConcept C2778703903 @default.
• W162590092 hasConcept C77928131 @default.
• W162590092 hasConceptScore W162590092C109007969 @default.
• W162590092 hasConceptScore W162590092C114793014 @default.
• W162590092 hasConceptScore W162590092C120806208 @default.
• W162590092 hasConceptScore W162590092C126457475 @default.
• W162590092 hasConceptScore W162590092C127313418 @default.
• W162590092 hasConceptScore W162590092C150999391 @default.
• W162590092 hasConceptScore W162590092C151730666 @default.
• W162590092 hasConceptScore W162590092C16674752 @default.
• W162590092 hasConceptScore W162590092C17409809 @default.
• W162590092 hasConceptScore W162590092C175551986 @default.
• W162590092 hasConceptScore W162590092C192241223 @default.
• W162590092 hasConceptScore W162590092C2778471503 @default.
• W162590092 hasConceptScore W162590092C2778697265 @default.
• W162590092 hasConceptScore W162590092C2778703903 @default.
• W162590092 hasConceptScore W162590092C77928131 @default.
• W162590092 hasLocation W1625900921 @default.
• W162590092 hasOpenAccess W162590092 @default.
• W162590092 hasPrimaryLocation W1625900921 @default.
• W162590092 hasRelatedWork W1976643371 @default.
• W162590092 hasRelatedWork W1980940883 @default.
• W162590092 hasRelatedWork W2037281132 @default.
• W162590092 hasRelatedWork W2050976523 @default.
• W162590092 hasRelatedWork W2119395571 @default.
• W162590092 hasRelatedWork W2133440777 @default.
• W162590092 hasRelatedWork W2350943903 @default.
• W162590092 hasRelatedWork W2394037060 @default.
• W162590092 hasRelatedWork W2911773734 @default.
• W162590092 hasRelatedWork W3197450162 @default.
• W162590092 isParatext "false" @default.
• W162590092 isRetracted "false" @default.
• W162590092 magId "162590092" @default.
• W162590092 workType "article" @default.