FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2052837701> ?p ?o ?g. }

• W2052837701 endingPage "740" @default.
• W2052837701 startingPage "713" @default.
• W2052837701 abstract "Recently available new perspectives on the morphology of the sea–floor near the Mid–Atlantic Ridge reveal the widespread development of dome–like massifs with lineated upper surfaces. In form and dimensions, these features resemble continental metamorphic core complexes developed in regions of large–magnitude extension, and thus may be ‘oceanic core complexes’. Excellent examples of these features occur south of the Kane Transform Fault where high–resolution geological data from side–looking sonar, deeply towed cameras, and manned submersibles are available. The geological data from two different massifs, representing somewhat different types of crustal structure, provide important constraints on the development of these oceanic core complexes. Inferences from these direct geological investigations of oceanic core complexes are a first step toward understanding the processes by which these features form in slow–spread crust. Specific relationships in these massifs and nearby areas suggest that these structures have formed over significant lengths of ridge axis (tens of kilometres) and are not necessarily confined to any specific setting with respect to morphologic segmentation patterns. In some cases they are developed in thick gabbroic crust, but elsewhere have formed in crust composed serpentinite riddled with gabbroic intrusions. Ductile stretching and thinning of these sections is recorded in extensive mylonites and shear zones. Syntectonic gabbroic intrusions are widespread and contradict the notion that the massifs develop during intervals of ‘amagmatic spreading’. Cataclastic fault zones in gabbros and serpentinites developed during uplift, cooling and hydration of the stretched crust and may have been localized as major detachment faults. Sparse diabase dikes and basaltic lavas are the latest magmatic additions to these areas. Numerous joints and steeply dipping, small–offset faults are the youngest observed structures. Across part of the top surface of one massif, small–scale faults appear to bound elongated ridges of fractured basement rocks creating the lineated terrain. Thus, the extensive lineated surfaces nearby need not reflect prolonged displacement along a continuous detachment fault surface. Geological relationships developed in the dome–like massifs along the Kane Transform Fault hint at a complex array of processes involved in the evolution of these features and raise new questions regarding their origin and analogies with continental core complexes." @default.
• W2052837701 created "2016-06-24" @default.
• W2052837701 creator A5051732826 @default.
• W2052837701 date "1999-04-15" @default.
• W2052837701 modified "2023-10-18" @default.
• W2052837701 title "Geological investigation of a lineated massif at the Kane Transform Fault: implications for oceanic core complexes" @default.
• W2052837701 cites W135626895 @default.
• W2052837701 cites W1952657320 @default.
• W2052837701 cites W1963862763 @default.
• W2052837701 cites W1965952060 @default.
• W2052837701 cites W1968824256 @default.
• W2052837701 cites W1969731310 @default.
• W2052837701 cites W1969806692 @default.
• W2052837701 cites W1972167093 @default.
• W2052837701 cites W1972575957 @default.
• W2052837701 cites W1977664265 @default.
• W2052837701 cites W1980578633 @default.
• W2052837701 cites W1983815388 @default.
• W2052837701 cites W1984706520 @default.
• W2052837701 cites W1993588061 @default.
• W2052837701 cites W1994323983 @default.
• W2052837701 cites W2000404423 @default.
• W2052837701 cites W2001008178 @default.
• W2052837701 cites W2001415035 @default.
• W2052837701 cites W2002103876 @default.
• W2052837701 cites W2006712012 @default.
• W2052837701 cites W2007711398 @default.
• W2052837701 cites W2008934623 @default.
• W2052837701 cites W2011401090 @default.
• W2052837701 cites W2016302429 @default.
• W2052837701 cites W2019977269 @default.
• W2052837701 cites W2026194643 @default.
• W2052837701 cites W2027415449 @default.
• W2052837701 cites W2029810342 @default.
• W2052837701 cites W2035316152 @default.
• W2052837701 cites W2037891103 @default.
• W2052837701 cites W2043473102 @default.
• W2052837701 cites W2046098057 @default.
• W2052837701 cites W2046461168 @default.
• W2052837701 cites W2048759555 @default.
• W2052837701 cites W2048903462 @default.
• W2052837701 cites W2050928442 @default.
• W2052837701 cites W2061135565 @default.
• W2052837701 cites W2061191537 @default.
• W2052837701 cites W2065388882 @default.
• W2052837701 cites W2067431079 @default.
• W2052837701 cites W2069801129 @default.
• W2052837701 cites W2072527059 @default.
• W2052837701 cites W2080973789 @default.
• W2052837701 cites W2082990553 @default.
• W2052837701 cites W2090090002 @default.
• W2052837701 cites W2097274806 @default.
• W2052837701 cites W2103223747 @default.
• W2052837701 cites W2116958131 @default.
• W2052837701 cites W2126671525 @default.
• W2052837701 cites W2127136348 @default.
• W2052837701 cites W2138655928 @default.
• W2052837701 cites W2142508626 @default.
• W2052837701 cites W2145803736 @default.
• W2052837701 cites W2153021989 @default.
• W2052837701 cites W2463207926 @default.
• W2052837701 cites W2484302152 @default.
• W2052837701 cites W2501885631 @default.
• W2052837701 cites W4205832970 @default.
• W2052837701 cites W4243259209 @default.
• W2052837701 cites W4251061100 @default.
• W2052837701 cites W4377205393 @default.
• W2052837701 cites W44457397 @default.
• W2052837701 doi "https://doi.org/10.1098/rsta.1999.0350" @default.
• W2052837701 hasPublicationYear "1999" @default.
• W2052837701 type Work @default.
• W2052837701 sameAs 2052837701 @default.
• W2052837701 citedByCount "55" @default.
• W2052837701 countsByYear W20528377012012 @default.
• W2052837701 countsByYear W20528377012013 @default.
• W2052837701 countsByYear W20528377012014 @default.
• W2052837701 countsByYear W20528377012015 @default.
• W2052837701 countsByYear W20528377012016 @default.
• W2052837701 countsByYear W20528377012018 @default.
• W2052837701 countsByYear W20528377012019 @default.
• W2052837701 countsByYear W20528377012020 @default.
• W2052837701 countsByYear W20528377012022 @default.
• W2052837701 countsByYear W20528377012023 @default.
• W2052837701 crossrefType "journal-article" @default.
• W2052837701 hasAuthorship W2052837701A5051732826 @default.
• W2052837701 hasConcept C117485682 @default.
• W2052837701 hasConcept C127313418 @default.
• W2052837701 hasConcept C136137745 @default.
• W2052837701 hasConcept C151730666 @default.
• W2052837701 hasConcept C154200439 @default.
• W2052837701 hasConcept C160776313 @default.
• W2052837701 hasConcept C164421858 @default.
• W2052837701 hasConcept C165205528 @default.
• W2052837701 hasConcept C175551986 @default.
• W2052837701 hasConcept C185339796 @default.
• W2052837701 hasConcept C197737763 @default.
• W2052837701 hasConcept C23295444 @default.
• W2052837701 hasConcept C2776698055 @default.

• next