FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2012100534> ?p ?o ?g. }

• W2012100534 endingPage "54" @default.
• W2012100534 startingPage "33" @default.
• W2012100534 abstract "The thick Paleocene basaltic lava succession exposed on Disko Island and Nuussuaq Peninsula, central West Greenland, experienced regional metamorphism shortly after volcanism followed by several events of localized hydrothermal alteration. Regional metamorphism resulted in well-developed lower zeolite facies mineral assemblages consisting primarily of mafic phyllosilicates and zeolites. In the upper Paleocene lava formation, the Maligât Formation, alteration is dominated by early mixed dioctahedral–trioctahedral smectite followed by chabazite and thomsonite. This same assemblage persists into the upper portions of the underlying Vaigat Formation. Within the Vaigat Formation, the chabazite–thomsonite assemblage is replaced at depth by an assemblage dominated by mafic phyllosilicates followed by thomsonite + chabazite + analcime + natrolite + gonnardite. Mafic phyllosilicate compositions within the latter zone become systematically more rich in the trioctahedral component with depth; the highest-grade mafic phyllosilicates consist of purely trioctahedral, mixed-layer chlorite–smectite. The mineral assemblage developed in the Vaigat Formation is distinct from similar grade assemblages formed in most large igneous provinces as a consequence of the unusually olivine-rich lava compositions that dominate this formation. The zeolites developed in the Vaigat Formation tend to be more Na-rich and somewhat Si-depleted relative to those that form in feldspar-phyric lavas such as the Maligât Formation. Late hydrothermal alteration led to a wide variety of low-grade metamorphic mineral assemblages largely confined to mineralized veins and their immediate surroundings. The distribution of regional alteration assemblages on Disko and Nuussuaq suggests relatively low geothermal gradients (< 45 °C/km) during metamorphism. The highest regional metamorphic grades occur at the base of the exposed succession on northern Disko, suggesting uplift of this area relative to the rest of the island, consistent with recent seismic data." @default.
• W2012100534 created "2016-06-24" @default.
• W2012100534 creator A5011279084 @default.
• W2012100534 creator A5016317975 @default.
• W2012100534 creator A5018116830 @default.
• W2012100534 creator A5018297108 @default.
• W2012100534 creator A5036818306 @default.
• W2012100534 date "2006-11-01" @default.
• W2012100534 modified "2023-09-27" @default.
• W2012100534 title "Regional very low-grade metamorphism of basaltic lavas, Disko–Nuussuaq region, West Greenland" @default.
• W2012100534 cites W1555133190 @default.
• W2012100534 cites W1556705733 @default.
• W2012100534 cites W1817585669 @default.
• W2012100534 cites W1821151640 @default.
• W2012100534 cites W1964719915 @default.
• W2012100534 cites W1966093554 @default.
• W2012100534 cites W1967419716 @default.
• W2012100534 cites W1976712317 @default.
• W2012100534 cites W1979695954 @default.
• W2012100534 cites W1980046202 @default.
• W2012100534 cites W1981737804 @default.
• W2012100534 cites W1991701391 @default.
• W2012100534 cites W1993490397 @default.
• W2012100534 cites W1995698173 @default.
• W2012100534 cites W1996832287 @default.
• W2012100534 cites W1997534357 @default.
• W2012100534 cites W1998239973 @default.
• W2012100534 cites W2007448272 @default.
• W2012100534 cites W2014449817 @default.
• W2012100534 cites W2020976223 @default.
• W2012100534 cites W2023412179 @default.
• W2012100534 cites W2024975374 @default.
• W2012100534 cites W2033497000 @default.
• W2012100534 cites W2036017971 @default.
• W2012100534 cites W2037637153 @default.
• W2012100534 cites W2046414884 @default.
• W2012100534 cites W2046829014 @default.
• W2012100534 cites W2048449294 @default.
• W2012100534 cites W2056797624 @default.
• W2012100534 cites W2063105478 @default.
• W2012100534 cites W2079045061 @default.
• W2012100534 cites W2085591215 @default.
• W2012100534 cites W2087171801 @default.
• W2012100534 cites W2103517719 @default.
• W2012100534 cites W2107131671 @default.
• W2012100534 cites W2112744199 @default.
• W2012100534 cites W2114051980 @default.
• W2012100534 cites W2121477286 @default.
• W2012100534 cites W2130680196 @default.
• W2012100534 cites W2133632700 @default.
• W2012100534 cites W2149021721 @default.
• W2012100534 cites W2168019960 @default.
• W2012100534 cites W2261443321 @default.
• W2012100534 cites W2269800663 @default.
• W2012100534 cites W2313146119 @default.
• W2012100534 cites W2326381477 @default.
• W2012100534 cites W2339309276 @default.
• W2012100534 cites W2407782081 @default.
• W2012100534 cites W2410477729 @default.
• W2012100534 cites W2473243627 @default.
• W2012100534 cites W2497774030 @default.
• W2012100534 cites W3018581654 @default.
• W2012100534 cites W3030412547 @default.
• W2012100534 cites W3143483768 @default.
• W2012100534 cites W3166027785 @default.
• W2012100534 cites W3166046691 @default.
• W2012100534 cites W3168308530 @default.
• W2012100534 cites W3169990835 @default.
• W2012100534 cites W3170192967 @default.
• W2012100534 cites W3171022581 @default.
• W2012100534 cites W3171322788 @default.
• W2012100534 cites W3171677205 @default.
• W2012100534 cites W3171996629 @default.
• W2012100534 cites W606557605 @default.
• W2012100534 doi "https://doi.org/10.1016/j.lithos.2006.03.028" @default.
• W2012100534 hasPublicationYear "2006" @default.
• W2012100534 type Work @default.
• W2012100534 sameAs 2012100534 @default.
• W2012100534 citedByCount "33" @default.
• W2012100534 countsByYear W20121005342012 @default.
• W2012100534 countsByYear W20121005342013 @default.
• W2012100534 countsByYear W20121005342014 @default.
• W2012100534 countsByYear W20121005342015 @default.
• W2012100534 countsByYear W20121005342017 @default.
• W2012100534 countsByYear W20121005342018 @default.
• W2012100534 countsByYear W20121005342019 @default.
• W2012100534 countsByYear W20121005342020 @default.
• W2012100534 countsByYear W20121005342021 @default.
• W2012100534 countsByYear W20121005342022 @default.
• W2012100534 crossrefType "journal-article" @default.
• W2012100534 hasAuthorship W2012100534A5011279084 @default.
• W2012100534 hasAuthorship W2012100534A5016317975 @default.
• W2012100534 hasAuthorship W2012100534A5018116830 @default.
• W2012100534 hasAuthorship W2012100534A5018297108 @default.
• W2012100534 hasAuthorship W2012100534A5036818306 @default.
• W2012100534 hasConcept C112764850 @default.
• W2012100534 hasConcept C127313418 @default.
• W2012100534 hasConcept C151730666 @default.

• next