FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2889100013> ?p ?o ?g. }

• W2889100013 endingPage "511" @default.
• W2889100013 startingPage "461" @default.
• W2889100013 abstract "The diverging plate boundaries in North Iceland and its shelf display a complex tectonic at the Kolbeinsey Ridge (K-R), the Northern Rift Zone (NRZ), and the Tj?rnes Fracture Zone containing the Grímsey Oblique Rift (GOR), the Húsavík-Flatey Fault (HFF), and the Dalvík Lineament (DL). While active deformation is well-known, the structural pattern is sporadically mapped and a comprehensive account of the upper Tertiary-present deformation is not fully at hand. To address the gaps, this paper provides new regional tectonic maps with continuous coverage, and detailed analyses of the deformation. Faults, open fractures, prominent joints and volcanic edifices were identified on Multibeam/Single beam, Spot 5, and Digital Elevation Model, and subjected to multidisciplinary structural analysis and correlation with selected data. Some of the results are: 1) Six sets constitute the structural pattern. The N-S rift-parallel normal faults are 1/3, and the shear fractures of the transform zone and the oblique rift 2/3 of the fracture population. The en échelon arrangements above deep-seated shear zones indicate dextral slip on WNW to NW, and sinistral slip on NNE to ENE faults, conformable with earthquake data. 2) During the polyphase tectonic, the six sets led to basin and horst formation, block compartmentalisation, rotation, horsetail splay, rhomb-graben in relay zone of strike-slips, and volcanism. 3) Listric faults are absent and the steeply-dipping faults are antithetic, synthetic, or form extensional flower structures above 4 km depth. The Plio-pleistocene/present syn-sedimentary deformation caused a deep half graben in the Eyjafjarearáll Basin (Ey), fault growth, rollover, and sediment onlaps, with some of the faults still active. 4) The plate boundaries of K-R/Ey, GOR/?xarfjreur/NRZ, and DL delimit a major microplate labelled here as Grímsey-Tj?rnes-Dalvík. 5) The WNW earthquake cluster in GOR corresponds either to a blind horsetail splay fault or to initiation of a transform segment parallel to the HFF. The described tectonic-sedimentary-magmatic deformation is relevant to other diverging plate boundaries where similar sets control the hydrocarbon and geothermal resources." @default.
• W2889100013 created "2018-09-07" @default.
• W2889100013 creator A5044271719 @default.
• W2889100013 creator A5089972104 @default.
• W2889100013 date "2018-01-01" @default.
• W2889100013 modified "2023-09-26" @default.
• W2889100013 title "Structures and Styles of Deformation in Rift, Ridge, Transform Zone, Oblique Rift and a Microplate Offshore/Onshore North Iceland" @default.
• W2889100013 cites W1518103483 @default.
• W2889100013 cites W1518419654 @default.
• W2889100013 cites W1560714783 @default.
• W2889100013 cites W1578715279 @default.
• W2889100013 cites W1589361213 @default.
• W2889100013 cites W1667447052 @default.
• W2889100013 cites W1964197584 @default.
• W2889100013 cites W1965078451 @default.
• W2889100013 cites W1968895964 @default.
• W2889100013 cites W1968999833 @default.
• W2889100013 cites W1969112599 @default.
• W2889100013 cites W1970334697 @default.
• W2889100013 cites W1974493245 @default.
• W2889100013 cites W1974610448 @default.
• W2889100013 cites W1975445336 @default.
• W2889100013 cites W1975777283 @default.
• W2889100013 cites W1978185779 @default.
• W2889100013 cites W1980679023 @default.
• W2889100013 cites W1982779071 @default.
• W2889100013 cites W1983777910 @default.
• W2889100013 cites W1983879726 @default.
• W2889100013 cites W1986982663 @default.
• W2889100013 cites W1987019383 @default.
• W2889100013 cites W1990536791 @default.
• W2889100013 cites W1993192562 @default.
• W2889100013 cites W1993588061 @default.
• W2889100013 cites W1995809323 @default.
• W2889100013 cites W1996186259 @default.
• W2889100013 cites W1996831697 @default.
• W2889100013 cites W1998188289 @default.
• W2889100013 cites W1998557806 @default.
• W2889100013 cites W1999089294 @default.
• W2889100013 cites W2002453184 @default.
• W2889100013 cites W2005292640 @default.
• W2889100013 cites W2006644501 @default.
• W2889100013 cites W2006745337 @default.
• W2889100013 cites W2011055448 @default.
• W2889100013 cites W2014144720 @default.
• W2889100013 cites W2014864243 @default.
• W2889100013 cites W2022648729 @default.
• W2889100013 cites W2024793243 @default.
• W2889100013 cites W2027523108 @default.
• W2889100013 cites W2030745437 @default.
• W2889100013 cites W2033502571 @default.
• W2889100013 cites W2034049221 @default.
• W2889100013 cites W2034896492 @default.
• W2889100013 cites W2040925008 @default.
• W2889100013 cites W2041540137 @default.
• W2889100013 cites W2042727696 @default.
• W2889100013 cites W2044592077 @default.
• W2889100013 cites W2046491190 @default.
• W2889100013 cites W2048542403 @default.
• W2889100013 cites W2051046669 @default.
• W2889100013 cites W2051397440 @default.
• W2889100013 cites W2053596635 @default.
• W2889100013 cites W2054451772 @default.
• W2889100013 cites W2055127223 @default.
• W2889100013 cites W2055566826 @default.
• W2889100013 cites W2056551438 @default.
• W2889100013 cites W2058656414 @default.
• W2889100013 cites W2060329206 @default.
• W2889100013 cites W2060589231 @default.
• W2889100013 cites W2062250537 @default.
• W2889100013 cites W2062664646 @default.
• W2889100013 cites W2064970633 @default.
• W2889100013 cites W2067009614 @default.
• W2889100013 cites W2067689144 @default.
• W2889100013 cites W2067969260 @default.
• W2889100013 cites W2068161390 @default.
• W2889100013 cites W2068772241 @default.
• W2889100013 cites W2069570241 @default.
• W2889100013 cites W2070023059 @default.
• W2889100013 cites W2071600331 @default.
• W2889100013 cites W2074318293 @default.
• W2889100013 cites W2076380260 @default.
• W2889100013 cites W2077028606 @default.
• W2889100013 cites W2077098086 @default.
• W2889100013 cites W2077308142 @default.
• W2889100013 cites W2077953409 @default.
• W2889100013 cites W2078005590 @default.
• W2889100013 cites W2079653280 @default.
• W2889100013 cites W2080282388 @default.
• W2889100013 cites W2080828102 @default.
• W2889100013 cites W2083142278 @default.
• W2889100013 cites W2084818844 @default.
• W2889100013 cites W2088688465 @default.
• W2889100013 cites W2089857088 @default.
• W2889100013 cites W2092885778 @default.
• W2889100013 cites W2093951728 @default.
• W2889100013 cites W2099226273 @default.
• W2889100013 cites W2100719803 @default.

• next