FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2029240983> ?p ?o ?g. }

• W2029240983 endingPage "103" @default.
• W2029240983 startingPage "78" @default.
• W2029240983 abstract "Abstract Structural analysis defines a multiphase Sveconorwegian tectonic evolution for the boundary zone between the Kongsberg and Telemark lithotectonic units in S Norway, referred to as the Kongsberg-Telemark Boundary Zone (KTBZ). This large-scale weakness zone developed predominantly within and at the margin of a c. 110 km long granitic belt, the intrusion of which is dated between 1170 ± 11 and 1146 ± 5 Ma by U–Pb SIMS zircon geochronology. The oldest KTBZ ductile fabric formed during the Sveconorwegian orogenic cycle (c. 1140–900 Ma) as a penetrative top-to-the-W shear fabric, which was subsequently reactivated selectively by sinistral transpression that formed characteristic mylonitic shear zones within the granitic belt. Later folding affected the area at the northern end of the Kongsberg lithotectonic unit. Analysis of the subregional foliation trajectories unravels the occurrence of a large-scale fold structure, the “Norefjell-Honefoss Fold”. All these structures are in turn cut by late-Sveconorwegian, E-dipping shear zones and normal faults, which accommodated a distinct phase of exhumation of the Telemark lithotectonic unit in the footwall of the KTBZ. This extensional detachment widens toward the north, where it might have controlled the emplacement of the late-orogenic Fla granite. Since late Sveconorwegian times, the KTBZ was repeatedly reactivated in a brittle fashion forming complex fault patterns, extensive quartz vein networks and leading to the generation of the so-called “Store Rivningsbreksje”, a 100 km long brittle fault zone that follows the trend of the KTBZ and that locally juxtaposes blocks with different ductile precursor histories. The newly established deformation history helps to refine existing models for the orogenic evolution of the central Sveconorwegian orogen. The characterization of the Norefjell-Honefoss fold structure provides a new perspective on Sveconorwegian geometries and fabrics in the area. The reactivation history established for the KTBZ helps to better understand the dynamics of long-lived weakness zones of Precambrian origin in general." @default.
• W2029240983 created "2016-06-24" @default.
• W2029240983 creator A5027905765 @default.
• W2029240983 creator A5041868142 @default.
• W2029240983 creator A5077610855 @default.
• W2029240983 creator A5083019417 @default.
• W2029240983 creator A5088226401 @default.
• W2029240983 date "2015-08-01" @default.
• W2029240983 modified "2023-10-03" @default.
• W2029240983 title "Multiple reactivation and strain localization along a Proterozoic orogen-scale deformation zone: The Kongsberg-Telemark boundary in southern Norway revisited" @default.
• W2029240983 cites W115532391 @default.
• W2029240983 cites W1538382845 @default.
• W2029240983 cites W1566043238 @default.
• W2029240983 cites W1582566143 @default.
• W2029240983 cites W1961302952 @default.
• W2029240983 cites W1966989464 @default.
• W2029240983 cites W1969755548 @default.
• W2029240983 cites W1971080266 @default.
• W2029240983 cites W1974810094 @default.
• W2029240983 cites W1977603915 @default.
• W2029240983 cites W1977883297 @default.
• W2029240983 cites W1979106839 @default.
• W2029240983 cites W1980025301 @default.
• W2029240983 cites W1986976616 @default.
• W2029240983 cites W1987657517 @default.
• W2029240983 cites W1992338695 @default.
• W2029240983 cites W2001753780 @default.
• W2029240983 cites W2003578564 @default.
• W2029240983 cites W2005348715 @default.
• W2029240983 cites W2005918852 @default.
• W2029240983 cites W2006575382 @default.
• W2029240983 cites W2009908156 @default.
• W2029240983 cites W2011343588 @default.
• W2029240983 cites W2016243171 @default.
• W2029240983 cites W2017395625 @default.
• W2029240983 cites W2018723058 @default.
• W2029240983 cites W2019152704 @default.
• W2029240983 cites W2019907634 @default.
• W2029240983 cites W2024055416 @default.
• W2029240983 cites W2025552690 @default.
• W2029240983 cites W2027209394 @default.
• W2029240983 cites W2027721230 @default.
• W2029240983 cites W2028001269 @default.
• W2029240983 cites W2029074756 @default.
• W2029240983 cites W2031395330 @default.
• W2029240983 cites W2031413961 @default.
• W2029240983 cites W2033121619 @default.
• W2029240983 cites W2033494237 @default.
• W2029240983 cites W2035608336 @default.
• W2029240983 cites W2039872199 @default.
• W2029240983 cites W2041404152 @default.
• W2029240983 cites W2042071294 @default.
• W2029240983 cites W2042767874 @default.
• W2029240983 cites W2044368575 @default.
• W2029240983 cites W2045368485 @default.
• W2029240983 cites W2045668709 @default.
• W2029240983 cites W2047775483 @default.
• W2029240983 cites W2048240400 @default.
• W2029240983 cites W2048979765 @default.
• W2029240983 cites W2053485431 @default.
• W2029240983 cites W2057665303 @default.
• W2029240983 cites W2059304029 @default.
• W2029240983 cites W2061512750 @default.
• W2029240983 cites W2061573838 @default.
• W2029240983 cites W2063330441 @default.
• W2029240983 cites W2065157015 @default.
• W2029240983 cites W2065568524 @default.
• W2029240983 cites W2069186880 @default.
• W2029240983 cites W2075133310 @default.
• W2029240983 cites W2076603812 @default.
• W2029240983 cites W2083326010 @default.
• W2029240983 cites W2083605721 @default.
• W2029240983 cites W2087980462 @default.
• W2029240983 cites W2092877638 @default.
• W2029240983 cites W2096801474 @default.
• W2029240983 cites W2099367338 @default.
• W2029240983 cites W2107542043 @default.
• W2029240983 cites W2109599465 @default.
• W2029240983 cites W2113807312 @default.
• W2029240983 cites W2125098024 @default.
• W2029240983 cites W2136898319 @default.
• W2029240983 cites W2137729850 @default.
• W2029240983 cites W2142339071 @default.
• W2029240983 cites W2151199734 @default.
• W2029240983 cites W2152495027 @default.
• W2029240983 cites W2155128667 @default.
• W2029240983 cites W2158077899 @default.
• W2029240983 cites W2168298006 @default.
• W2029240983 cites W2171827043 @default.
• W2029240983 cites W2764747535 @default.
• W2029240983 cites W3205771575 @default.
• W2029240983 doi "https://doi.org/10.1016/j.precamres.2015.03.009" @default.
• W2029240983 hasPublicationYear "2015" @default.
• W2029240983 type Work @default.
• W2029240983 sameAs 2029240983 @default.
• W2029240983 citedByCount "19" @default.
• W2029240983 countsByYear W20292409832015 @default.
• W2029240983 countsByYear W20292409832016 @default.

• next