FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966074920> ?p ?o ?g. }

• W1966074920 endingPage "175" @default.
• W1966074920 startingPage "160" @default.
• W1966074920 abstract "In fold-and-thrust belts, shortening is mainly accommodated by thrust faults which are preferential zones for recrystallisation and mass transfer. This study focuses on a detachment fault related to the emplacement of the Monte Perdido thrust unit in the southern Pyrenees. The studied fault zone consists of a 10 m thick intensively foliated phyllonite developed within the Millaris marls, of Eocene age. The lithological homogeneity of the hanging wall and footwall allows us to compare the Millaris marls outside the fault zone with the highly deformed marls located in the fault zone and to quantify the chemical, mineralogical and volumetric changes related to deformation processes along the fault. The Millaris marls are composed of detrital quartz, illite, chlorite, minor albite and pyrite, in a micritic calcite matrix. In the fault zone, the cleavage planes are marked by clay minerals and calcite ± chlorite veins attest to fluid–mineral interactions during deformation. The mineral proportions in all samples from both the fault zone and Millaris marls have been quantified by two methods: (1) X-ray diffraction and Rietveld refinement, and (2) bulk chemical analyses as well as microprobe analyses to calculate modal composition. The excellent agreement between the results of these two methods allows us to estimate mineralogical variations using a modification of the Gresens' equation. During fault activation, up to 45 wt% of calcite was lost while the amounts of quartz and chlorite remained unchanged. Illite content remained constant to slightly enriched. The mineralogical variations were coupled with a significant volume loss (up to 45%) mostly due to the dissolution of micritic calcite grains. Deformation was accompanied by pressure solution and phyllosilicates recrystallisation. These processes accommodated slip along the fault. They required fluids as catalyst, but they did not necessitate major chemical transfers." @default.
• W1966074920 created "2016-06-24" @default.
• W1966074920 creator A5040897705 @default.
• W1966074920 creator A5048692707 @default.
• W1966074920 creator A5050535558 @default.
• W1966074920 creator A5053087570 @default.
• W1966074920 creator A5075166773 @default.
• W1966074920 creator A5077535919 @default.
• W1966074920 creator A5077815004 @default.
• W1966074920 date "2014-08-01" @default.
• W1966074920 modified "2023-10-05" @default.
• W1966074920 title "Quantification of mass transfers and mineralogical transformations in a thrust fault (Monte Perdido thrust unit, southern Pyrenees, Spain)" @default.
• W1966074920 cites W1538545315 @default.
• W1966074920 cites W1647725950 @default.
• W1966074920 cites W1821151640 @default.
• W1966074920 cites W1963987887 @default.
• W1966074920 cites W1969465780 @default.
• W1966074920 cites W1972755934 @default.
• W1966074920 cites W1973518565 @default.
• W1966074920 cites W1977156689 @default.
• W1966074920 cites W1978878856 @default.
• W1966074920 cites W1984019431 @default.
• W1966074920 cites W1985521055 @default.
• W1966074920 cites W1993664081 @default.
• W1966074920 cites W1994253014 @default.
• W1966074920 cites W1998622803 @default.
• W1966074920 cites W2006115899 @default.
• W1966074920 cites W2008632542 @default.
• W1966074920 cites W2009619843 @default.
• W1966074920 cites W2011737275 @default.
• W1966074920 cites W2011859305 @default.
• W1966074920 cites W2013447206 @default.
• W1966074920 cites W2015923183 @default.
• W1966074920 cites W2016260972 @default.
• W1966074920 cites W2017083513 @default.
• W1966074920 cites W2020487117 @default.
• W1966074920 cites W2025346274 @default.
• W1966074920 cites W2027736655 @default.
• W1966074920 cites W2031249760 @default.
• W1966074920 cites W2031384515 @default.
• W1966074920 cites W2033047492 @default.
• W1966074920 cites W2052917991 @default.
• W1966074920 cites W2056301165 @default.
• W1966074920 cites W2059877826 @default.
• W1966074920 cites W2062263455 @default.
• W1966074920 cites W2063342502 @default.
• W1966074920 cites W2066130477 @default.
• W1966074920 cites W2073815295 @default.
• W1966074920 cites W2075618665 @default.
• W1966074920 cites W2075935676 @default.
• W1966074920 cites W2085385901 @default.
• W1966074920 cites W2085471924 @default.
• W1966074920 cites W2112769390 @default.
• W1966074920 cites W2120399724 @default.
• W1966074920 cites W2122338764 @default.
• W1966074920 cites W2126024272 @default.
• W1966074920 cites W2133155865 @default.
• W1966074920 cites W2133314518 @default.
• W1966074920 cites W2138849924 @default.
• W1966074920 cites W2140408185 @default.
• W1966074920 cites W2152195282 @default.
• W1966074920 cites W2165253121 @default.
• W1966074920 cites W2165658645 @default.
• W1966074920 doi "https://doi.org/10.1016/j.marpetgeo.2013.12.016" @default.
• W1966074920 hasPublicationYear "2014" @default.
• W1966074920 type Work @default.
• W1966074920 sameAs 1966074920 @default.
• W1966074920 citedByCount "17" @default.
• W1966074920 countsByYear W19660749202015 @default.
• W1966074920 countsByYear W19660749202016 @default.
• W1966074920 countsByYear W19660749202017 @default.
• W1966074920 countsByYear W19660749202018 @default.
• W1966074920 countsByYear W19660749202019 @default.
• W1966074920 countsByYear W19660749202021 @default.
• W1966074920 countsByYear W19660749202022 @default.
• W1966074920 countsByYear W19660749202023 @default.
• W1966074920 crossrefType "journal-article" @default.
• W1966074920 hasAuthorship W1966074920A5040897705 @default.
• W1966074920 hasAuthorship W1966074920A5048692707 @default.
• W1966074920 hasAuthorship W1966074920A5050535558 @default.
• W1966074920 hasAuthorship W1966074920A5053087570 @default.
• W1966074920 hasAuthorship W1966074920A5075166773 @default.
• W1966074920 hasAuthorship W1966074920A5077535919 @default.
• W1966074920 hasAuthorship W1966074920A5077815004 @default.
• W1966074920 hasBestOaLocation W19660749204 @default.
• W1966074920 hasConcept C109007969 @default.
• W1966074920 hasConcept C110041135 @default.
• W1966074920 hasConcept C114793014 @default.
• W1966074920 hasConcept C127313418 @default.
• W1966074920 hasConcept C151730666 @default.
• W1966074920 hasConcept C165205528 @default.
• W1966074920 hasConcept C17409809 @default.
• W1966074920 hasConcept C175551986 @default.
• W1966074920 hasConcept C192194790 @default.
• W1966074920 hasConcept C199289684 @default.
• W1966074920 hasConcept C2777844515 @default.
• W1966074920 hasConcept C2779429093 @default.
• W1966074920 hasConcept C2779870107 @default.

• next