FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019440852> ?p ?o ?g. }

• W2019440852 endingPage "123" @default.
• W2019440852 startingPage "108" @default.
• W2019440852 abstract "Abstract Fabric patterns of strongly serpentinized peridotite were determined using eigenvector analysis and eigenvalue classification of lattice preferred orientation of olivine and orthopyroxene. This approach has been applied to a rootless fold-shaped body of mylonitized spinel to garnet peridotite surrounded by fine-grained and partially retrogressed ky–kfs granulite. The EBSD data show either axial [0 1 0] or [1 0 0](0 k l) pattern, both characteristic for ‘dry’ slip systems. The former pattern occurs predominantly along the inner margin and southern limb while the latter is mainly developed in the hinge of the fold shaped body. Foliations and lineations deciphered from the LPO data suggest that the [1 0 0](0 k l) pattern reflects constrictional deformation (prolate strain ellipsoid) in the hinge of the peridotite fold while the axial [0 1 0] pattern reflects pure flattening (oblate strain ellipsoid) inherited from the period of emplacement of the peridotite sheet in the crust. Similarity in finite strain pattern of peridotite and surrounding granulites indicates their common thermal and mechanical evolution during folding. The petrology and structural data result in a model of burial of peridotite below thickened crustal root, its exhumation and folding. The burial stage is associated with prograde metamorphism resulting in a coarse-grained microstructure and development of spinel and garnet zones. The emplacement of peridotite into lower crustal granulites occurred along a shear zone associated with grain size reduction in both peridotite and granulite and rapid cooling of mylonitized peridotite to the ambient temperatures of lower crust. Further ascent to mid-crustal levels occurred within the vertical granulite channel. Final fold shape of the peridotite developed during subsequent indentation of the weak vertically anisotropic crust by the adjacent continental promontory. The degree of mechanical coupling between folded peridotite and granulite in mid-crustal levels is estimated using comparison of studied microstructures with experimental data." @default.
• W2019440852 created "2016-06-24" @default.
• W2019440852 creator A5053029204 @default.
• W2019440852 creator A5074843514 @default.
• W2019440852 creator A5076698197 @default.
• W2019440852 date "2012-05-01" @default.
• W2019440852 modified "2023-10-05" @default.
• W2019440852 title "Ductile deformation and rheology of sub-continental mantle in a hot collisional orogeny: Example from the Bohemian Massif" @default.
• W2019440852 cites W1497317178 @default.
• W2019440852 cites W1532765746 @default.
• W2019440852 cites W1533979261 @default.
• W2019440852 cites W1543257786 @default.
• W2019440852 cites W1666099996 @default.
• W2019440852 cites W1771565016 @default.
• W2019440852 cites W1962482944 @default.
• W2019440852 cites W1965152929 @default.
• W2019440852 cites W1967928062 @default.
• W2019440852 cites W1973990596 @default.
• W2019440852 cites W1974467019 @default.
• W2019440852 cites W1976274418 @default.
• W2019440852 cites W1980092680 @default.
• W2019440852 cites W1983472035 @default.
• W2019440852 cites W1986161369 @default.
• W2019440852 cites W1990390248 @default.
• W2019440852 cites W1992902717 @default.
• W2019440852 cites W1995115331 @default.
• W2019440852 cites W1995498098 @default.
• W2019440852 cites W1998107551 @default.
• W2019440852 cites W1998691409 @default.
• W2019440852 cites W1999850681 @default.
• W2019440852 cites W2000033909 @default.
• W2019440852 cites W2005516122 @default.
• W2019440852 cites W2008412316 @default.
• W2019440852 cites W2012428364 @default.
• W2019440852 cites W2012471105 @default.
• W2019440852 cites W2016865743 @default.
• W2019440852 cites W2017550611 @default.
• W2019440852 cites W2017588800 @default.
• W2019440852 cites W2017658532 @default.
• W2019440852 cites W2024019540 @default.
• W2019440852 cites W2030487011 @default.
• W2019440852 cites W2031458587 @default.
• W2019440852 cites W2032972683 @default.
• W2019440852 cites W2033791808 @default.
• W2019440852 cites W2036293114 @default.
• W2019440852 cites W2038328635 @default.
• W2019440852 cites W2040663618 @default.
• W2019440852 cites W2041514871 @default.
• W2019440852 cites W2043910621 @default.
• W2019440852 cites W2044210226 @default.
• W2019440852 cites W2048455922 @default.
• W2019440852 cites W2050198702 @default.
• W2019440852 cites W2052847541 @default.
• W2019440852 cites W2055858362 @default.
• W2019440852 cites W2057633554 @default.
• W2019440852 cites W2058060723 @default.
• W2019440852 cites W2058982328 @default.
• W2019440852 cites W2060883068 @default.
• W2019440852 cites W2061740219 @default.
• W2019440852 cites W2062018184 @default.
• W2019440852 cites W2063628199 @default.
• W2019440852 cites W2064588212 @default.
• W2019440852 cites W2065051607 @default.
• W2019440852 cites W2068164597 @default.
• W2019440852 cites W2068269169 @default.
• W2019440852 cites W2068684490 @default.
• W2019440852 cites W2068986987 @default.
• W2019440852 cites W2069125613 @default.
• W2019440852 cites W2069498568 @default.
• W2019440852 cites W2074784970 @default.
• W2019440852 cites W2075910962 @default.
• W2019440852 cites W2078021476 @default.
• W2019440852 cites W2079309154 @default.
• W2019440852 cites W2080394669 @default.
• W2019440852 cites W2082148657 @default.
• W2019440852 cites W2084439549 @default.
• W2019440852 cites W2093770479 @default.
• W2019440852 cites W2093936359 @default.
• W2019440852 cites W2094231314 @default.
• W2019440852 cites W2103597088 @default.
• W2019440852 cites W2110083414 @default.
• W2019440852 cites W2110605561 @default.
• W2019440852 cites W2116414338 @default.
• W2019440852 cites W2116519903 @default.
• W2019440852 cites W2120697819 @default.
• W2019440852 cites W2130031398 @default.
• W2019440852 cites W2132697546 @default.
• W2019440852 cites W2133100925 @default.
• W2019440852 cites W2133517299 @default.
• W2019440852 cites W2134261798 @default.
• W2019440852 cites W2137471179 @default.
• W2019440852 cites W2139829082 @default.
• W2019440852 cites W2144152811 @default.
• W2019440852 cites W2148940495 @default.
• W2019440852 cites W2153654932 @default.
• W2019440852 cites W2163699960 @default.
• W2019440852 cites W2166287006 @default.
• W2019440852 cites W2168943758 @default.

• next