FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4384156946> ?p ?o ?g. }

• W4384156946 endingPage "104916" @default.
• W4384156946 startingPage "104916" @default.
• W4384156946 abstract "Stylolites form by the transportation and precipitation of dissolved materials in pore fluids due to concentration gradients that develop in rocks under stress. This is a coupled chemical-hydraulic-mechanical (CHM) process, resulting from the interplay between chemical dissolution, pore fluid flow and stress during stylolite growth. Although the CHM feedbacks that develop around stylolite seams lead to porosity compartmentalization, the dynamic processes controlling porosity evolution during stylolite growth remain unknown. Here, thrust-induced stylolites in micritic limestones of the Eilean Dubh Formation that crop out in the footwall of the Caledonian Ullapool/Moine Thrust in NW Scotland are used to investigate the dynamic processes controlling stylolite growth. Stylolite microstructures observed in detail, using a backscatter electron image mosaic (102,600 × 18,239 pixels; 0.17μm/pixels), both reveal stylolite seams (core zones) surrounded by zones of increased-porosity (damage zones) and suggest a four stage self-organization process for stylolite growth and evolution. In the first stage, stress concentration in the micritic matrix led to the partial dissolution of the matrix, forming new pores adjacent to pyrites grains. In the second stage, the new pores facilitated local dissolution, which in turn promoted their growth, establishing a positive feedback loop between texture and solubility that enlarged the local porous zone by self-organization. In the third stage, the porous zones facilitated the influx of externally derived fluids and differentiated into core zones, with syn-kinematic precipitation of secondary pyrites and clay minerals, and damage zones, with ongoing dissolution. In the fourth stage, the porous zones propagated perpendicular to the shortening direction and became interlinked, forming mature stylolites with a core zone in the centre surrounded on both sides by damage zones with high porosities. The fluid flux along the stylolites during their formation was likely controlled by episodic movements along the Ullapool Thrust." @default.
• W4384156946 created "2023-07-14" @default.
• W4384156946 creator A5004948928 @default.
• W4384156946 creator A5017129277 @default.
• W4384156946 creator A5063631483 @default.
• W4384156946 creator A5070068895 @default.
• W4384156946 date "2023-08-01" @default.
• W4384156946 modified "2023-09-25" @default.
• W4384156946 title "Synkinematic evolution of stylolite porosity" @default.
• W4384156946 cites W1978080283 @default.
• W4384156946 cites W1978729931 @default.
• W4384156946 cites W1986329089 @default.
• W4384156946 cites W1986537648 @default.
• W4384156946 cites W1989075842 @default.
• W4384156946 cites W2004261667 @default.
• W4384156946 cites W2006254758 @default.
• W4384156946 cites W2014324861 @default.
• W4384156946 cites W2015399809 @default.
• W4384156946 cites W2036766392 @default.
• W4384156946 cites W2040687069 @default.
• W4384156946 cites W2047420577 @default.
• W4384156946 cites W2052757568 @default.
• W4384156946 cites W2052967611 @default.
• W4384156946 cites W2053200498 @default.
• W4384156946 cites W2053997518 @default.
• W4384156946 cites W2056884399 @default.
• W4384156946 cites W2057299550 @default.
• W4384156946 cites W2061719363 @default.
• W4384156946 cites W2066130477 @default.
• W4384156946 cites W2069003345 @default.
• W4384156946 cites W2072742339 @default.
• W4384156946 cites W2094884720 @default.
• W4384156946 cites W2096586520 @default.
• W4384156946 cites W2115191099 @default.
• W4384156946 cites W2122068331 @default.
• W4384156946 cites W2146572212 @default.
• W4384156946 cites W2146953701 @default.
• W4384156946 cites W2148440657 @default.
• W4384156946 cites W2150829150 @default.
• W4384156946 cites W2157522005 @default.
• W4384156946 cites W2167279371 @default.
• W4384156946 cites W2170076374 @default.
• W4384156946 cites W2171838921 @default.
• W4384156946 cites W2330248125 @default.
• W4384156946 cites W2601810315 @default.
• W4384156946 cites W2766692997 @default.
• W4384156946 cites W2803107964 @default.
• W4384156946 cites W2888186169 @default.
• W4384156946 cites W2891319009 @default.
• W4384156946 cites W2965249361 @default.
• W4384156946 cites W3008330838 @default.
• W4384156946 cites W4205647993 @default.
• W4384156946 doi "https://doi.org/10.1016/j.jsg.2023.104916" @default.
• W4384156946 hasPublicationYear "2023" @default.
• W4384156946 type Work @default.
• W4384156946 citedByCount "0" @default.
• W4384156946 crossrefType "journal-article" @default.
• W4384156946 hasAuthorship W4384156946A5004948928 @default.
• W4384156946 hasAuthorship W4384156946A5017129277 @default.
• W4384156946 hasAuthorship W4384156946A5063631483 @default.
• W4384156946 hasAuthorship W4384156946A5070068895 @default.
• W4384156946 hasConcept C107054158 @default.
• W4384156946 hasConcept C121332964 @default.
• W4384156946 hasConcept C127313418 @default.
• W4384156946 hasConcept C130452526 @default.
• W4384156946 hasConcept C133916931 @default.
• W4384156946 hasConcept C147789679 @default.
• W4384156946 hasConcept C153294291 @default.
• W4384156946 hasConcept C174178034 @default.
• W4384156946 hasConcept C185592680 @default.
• W4384156946 hasConcept C187320778 @default.
• W4384156946 hasConcept C199289684 @default.
• W4384156946 hasConcept C6648577 @default.
• W4384156946 hasConcept C88380143 @default.
• W4384156946 hasConceptScore W4384156946C107054158 @default.
• W4384156946 hasConceptScore W4384156946C121332964 @default.
• W4384156946 hasConceptScore W4384156946C127313418 @default.
• W4384156946 hasConceptScore W4384156946C130452526 @default.
• W4384156946 hasConceptScore W4384156946C133916931 @default.
• W4384156946 hasConceptScore W4384156946C147789679 @default.
• W4384156946 hasConceptScore W4384156946C153294291 @default.
• W4384156946 hasConceptScore W4384156946C174178034 @default.
• W4384156946 hasConceptScore W4384156946C185592680 @default.
• W4384156946 hasConceptScore W4384156946C187320778 @default.
• W4384156946 hasConceptScore W4384156946C199289684 @default.
• W4384156946 hasConceptScore W4384156946C6648577 @default.
• W4384156946 hasConceptScore W4384156946C88380143 @default.
• W4384156946 hasLocation W43841569461 @default.
• W4384156946 hasOpenAccess W4384156946 @default.
• W4384156946 hasPrimaryLocation W43841569461 @default.
• W4384156946 hasRelatedWork W1990484035 @default.
• W4384156946 hasRelatedWork W2007169218 @default.
• W4384156946 hasRelatedWork W2007434786 @default.
• W4384156946 hasRelatedWork W2020487117 @default.
• W4384156946 hasRelatedWork W2054045083 @default.
• W4384156946 hasRelatedWork W2139902873 @default.
• W4384156946 hasRelatedWork W2170102073 @default.
• W4384156946 hasRelatedWork W2946830180 @default.

• next