FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2112873932> ?p ?o ?g. }

• W2112873932 endingPage "716" @default.
• W2112873932 startingPage "693" @default.
• W2112873932 abstract "The Atascosa Lookout trachyandesite lava flow is the youngest and most compositionally primitive unit in the middle Tertiary Atascosa–Tumacacori–Cerro Colorado volcanic complex (ATCC). The flow hosts a variety of objects of contrasting origin, including (1) clusters of plagioclase ± chromian diopside, magnesian augite, quartz, hornblende, and orthopyroxene; (2) amoeboid-shaped quartz-bearing enclaves; (3) plagioclase crystals with a concentric interior zone of small melt inclusions (dusty plagioclase); (4) plagioclase crystals with cores filled with large melt inclusions (honeycomb plagioclase); (5) plagioclase glomerocrysts. The groundmass of the trachyandesitic flow is trachydacite. Some crystal clusters, enclaves, and plagioclase glomerocrysts are surrounded by diffuse envelopes of trachydacite higher in K and Mg and lower in Si than the trachydacitic groundmass of the flow. This envelope material is interpreted as foreign magma that engulfed these objects as it invaded their host magma. Both the crystal clusters and plagioclase glomerocrysts may be the remains of cumulate crystal layers, disrupted by influxes of magma into their reservoirs. Crystals in the lava flow originated in at least three distinct magmas and their hybrids. The groundmass of the lava flow preserves evidence for repeated infusion of envelope magma into the system. These influxes fueled the invasion of crystal clusters, plagioclase glomerocrysts, enclaves, and swirls of the envelope magma into the groundmass of the Atascosa Lookout lava flow. Despite the compositional and textural variety apparent in the lava flow, the magmas involved in its development may have been genetically closely related. The collection of features in the lava flow resulted from the development of compositional layers in the magma, accumulation of crystal-rich horizons, disturbance of the system by repeated magma influx, and minor crustal assimilation." @default.
• W2112873932 created "2016-06-24" @default.
• W2112873932 creator A5024663598 @default.
• W2112873932 date "2000-05-01" @default.
• W2112873932 modified "2023-10-01" @default.
• W2112873932 title "Crystal Clusters, Feldspar Glomerocrysts, and Magma Envelopes in the Atascosa Lookout Lava Flow, Southern Arizona, USA: Recorders of Magmatic Events" @default.
• W2112873932 cites W1674284334 @default.
• W2112873932 cites W1952657320 @default.
• W2112873932 cites W1964680110 @default.
• W2112873932 cites W1966895654 @default.
• W2112873932 cites W1967277465 @default.
• W2112873932 cites W1976645689 @default.
• W2112873932 cites W1980974163 @default.
• W2112873932 cites W1989491939 @default.
• W2112873932 cites W1993170289 @default.
• W2112873932 cites W2001823729 @default.
• W2112873932 cites W2002132035 @default.
• W2112873932 cites W2012396908 @default.
• W2112873932 cites W2018262830 @default.
• W2112873932 cites W2021627365 @default.
• W2112873932 cites W2024835978 @default.
• W2112873932 cites W2034904379 @default.
• W2112873932 cites W2035586702 @default.
• W2112873932 cites W2037195508 @default.
• W2112873932 cites W2037262165 @default.
• W2112873932 cites W2039222439 @default.
• W2112873932 cites W2040549377 @default.
• W2112873932 cites W2041681251 @default.
• W2112873932 cites W2044353766 @default.
• W2112873932 cites W2046711380 @default.
• W2112873932 cites W2048152287 @default.
• W2112873932 cites W2056232757 @default.
• W2112873932 cites W2058118596 @default.
• W2112873932 cites W2058367269 @default.
• W2112873932 cites W2060204187 @default.
• W2112873932 cites W2063436373 @default.
• W2112873932 cites W2063478785 @default.
• W2112873932 cites W2072536276 @default.
• W2112873932 cites W2077582088 @default.
• W2112873932 cites W2077938222 @default.
• W2112873932 cites W2080206109 @default.
• W2112873932 cites W2082844473 @default.
• W2112873932 cites W2086393480 @default.
• W2112873932 cites W2092033333 @default.
• W2112873932 cites W2098979332 @default.
• W2112873932 cites W2105068734 @default.
• W2112873932 cites W2108417661 @default.
• W2112873932 cites W2111837677 @default.
• W2112873932 cites W2113174296 @default.
• W2112873932 cites W2116880139 @default.
• W2112873932 cites W2122639532 @default.
• W2112873932 cites W2136565500 @default.
• W2112873932 cites W2155349018 @default.
• W2112873932 cites W2157099954 @default.
• W2112873932 cites W2331859469 @default.
• W2112873932 cites W2345520342 @default.
• W2112873932 cites W2885503471 @default.
• W2112873932 cites W2899699838 @default.
• W2112873932 cites W2899764608 @default.
• W2112873932 doi "https://doi.org/10.1093/petrology/41.5.693" @default.
• W2112873932 hasPublicationYear "2000" @default.
• W2112873932 type Work @default.
• W2112873932 sameAs 2112873932 @default.
• W2112873932 citedByCount "54" @default.
• W2112873932 countsByYear W21128739322012 @default.
• W2112873932 countsByYear W21128739322013 @default.
• W2112873932 countsByYear W21128739322014 @default.
• W2112873932 countsByYear W21128739322015 @default.
• W2112873932 countsByYear W21128739322016 @default.
• W2112873932 countsByYear W21128739322017 @default.
• W2112873932 countsByYear W21128739322018 @default.
• W2112873932 countsByYear W21128739322019 @default.
• W2112873932 countsByYear W21128739322020 @default.
• W2112873932 countsByYear W21128739322021 @default.
• W2112873932 countsByYear W21128739322022 @default.
• W2112873932 countsByYear W21128739322023 @default.
• W2112873932 crossrefType "journal-article" @default.
• W2112873932 hasAuthorship W2112873932A5024663598 @default.
• W2112873932 hasBestOaLocation W21128739321 @default.
• W2112873932 hasConcept C113754120 @default.
• W2112873932 hasConcept C120806208 @default.
• W2112873932 hasConcept C127313418 @default.
• W2112873932 hasConcept C151730666 @default.
• W2112873932 hasConcept C161509811 @default.
• W2112873932 hasConcept C17409809 @default.
• W2112873932 hasConcept C182402614 @default.
• W2112873932 hasConcept C183222429 @default.
• W2112873932 hasConcept C192241223 @default.
• W2112873932 hasConcept C24343810 @default.
• W2112873932 hasConcept C2776283581 @default.
• W2112873932 hasConcept C2779181077 @default.
• W2112873932 hasConcept C2779870107 @default.
• W2112873932 hasConcept C5900021 @default.
• W2112873932 hasConcept C9566828 @default.
• W2112873932 hasConceptScore W2112873932C113754120 @default.
• W2112873932 hasConceptScore W2112873932C120806208 @default.
• W2112873932 hasConceptScore W2112873932C127313418 @default.
• W2112873932 hasConceptScore W2112873932C151730666 @default.

• next