FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2043669844> ?p ?o ?g. }

• W2043669844 endingPage "328" @default.
• W2043669844 startingPage "294" @default.
• W2043669844 abstract "Previous rock magnetic investigations of oceanic basement samples have been mainly restricted by single drill holes or dredge collections. In this study, we present new and published data on the rock magnetic properties of igneous rock samples recovered during seven Ocean Drilling Program (ODP) legs in the Atlantic, Pacific, and the southern Indian oceans. The recovered igneous rocks from these legs are mainly basaltic flows (both submarine and subaerial), diabase sills, and serpentinized peridotites with approximate ages of 140,000 years, 10–12, 34, 69, 100–108, and 110–121 Ma, which offers an opportunity to investigate magnetic properties and mineral changes attending alteration of basement rocks over a wide range of ages from variable tectonic settings. Titanomagnetite and titanomaghemite are commonly present in igneous rock samples of the Ontong Java Plateau, the Kerguelen Plateau/Broken Ridge, the eastern Equatorial Pacific, the middle Atlantic ridge (Trans-Atlantic Geotraverse area), and the Newfoundland-Iberia rifted margins. For basaltic rock samples, three general groups (A, B, and C, respectively) can be divided in terms of rock magnetic properties. Samples from group A have a single phase of Ti-poor titanomagnetite with Curie temperatures ranging between 480 and 580 °C and exhibit a strong Verwey transition in the vicinity of 110 K. Basalts from this group are most likely good paleomagnetic recorders and probably have preserved original and stable magnetic remanences. Group B is mainly observed in pillow lavas and is characterized by a Curie temperature of 260–280 °C, which is typical of low-temperature oxidized titanomaghemite or titanium rich titanomagnetite. The low-temperature curves for group B do not show the Verwey transition. Group C has more than one Curie temperature, which suggests the presence of multiple magnetic phases. The thermomagnetic signature indicates the inversion of titanomaghemite to a strongly magnetized magnetite, as shown by the irreversible cooling curves. For the serpentinized peridotites recovered from both sides of the Newfoundland-Iberia rifted margins, results from low-temperature measurements show that (titano)magnetites are present in the dark-colored peridotites, with a strong Verwey transition in the vicinity of 110 K, and with field- and frequency-dependent susceptibility curves that resemble those of synthetic TM0. In contrast to the magnetic properties observed from the dark-colored peridotites, the low-temperature curves for the yellow-brown-colored peridotites did not show any Verwey transition. Thermomagnetic analysis also failed to show evidence for titanomagnetites. The remanent magnetization is carried by a thermally unstable mineral that breaks down at about 420 °C, probably maghemite. The magnetic signatures of the serpentinized peridotites recovered from both sides of the Newfoundland-Iberia rift appear not in conflict with the notion that conjugate margins will have generally similar crustal structure and evolution history. Our rock magnetic data indicate that the differences in the rock magnetic properties of basaltic rocks are mainly a function of mineralogy and alteration. There is no apparent coincidence between the age of the rocks and the degree of low-temperature alteration, as suggested by the presence of nearly unoxidized titanomagnetite in the Cretaceous aged basalts and by an examination of Curie temperature versus sample age that does not unambiguously show a positive relationship between the degree of low-temperature oxidation and crust ages." @default.
• W2043669844 created "2016-06-24" @default.
• W2043669844 creator A5032082605 @default.
• W2043669844 creator A5038416930 @default.
• W2043669844 creator A5047415607 @default.
• W2043669844 creator A5048135366 @default.
• W2043669844 creator A5048329245 @default.
• W2043669844 creator A5056391726 @default.
• W2043669844 creator A5058114925 @default.
• W2043669844 creator A5060907895 @default.
• W2043669844 creator A5061295464 @default.
• W2043669844 creator A5077329887 @default.
• W2043669844 date "2006-07-01" @default.
• W2043669844 modified "2023-10-03" @default.
• W2043669844 title "Unraveling the magnetic carriers of igneous cores from the Atlantic, Pacific, and the southern Indian oceans with rock magnetic characterization" @default.
• W2043669844 cites W1964114137 @default.
• W2043669844 cites W1964687583 @default.
• W2043669844 cites W1968333494 @default.
• W2043669844 cites W1969955164 @default.
• W2043669844 cites W1970187426 @default.
• W2043669844 cites W1972988389 @default.
• W2043669844 cites W1973850736 @default.
• W2043669844 cites W1974627420 @default.
• W2043669844 cites W1976302971 @default.
• W2043669844 cites W1977736399 @default.
• W2043669844 cites W1978185779 @default.
• W2043669844 cites W1978935961 @default.
• W2043669844 cites W1980606894 @default.
• W2043669844 cites W1984765308 @default.
• W2043669844 cites W1985654794 @default.
• W2043669844 cites W2003600396 @default.
• W2043669844 cites W2005140146 @default.
• W2043669844 cites W2015895598 @default.
• W2043669844 cites W2018567339 @default.
• W2043669844 cites W2018792686 @default.
• W2043669844 cites W2027678030 @default.
• W2043669844 cites W2031128482 @default.
• W2043669844 cites W2042225110 @default.
• W2043669844 cites W2044343119 @default.
• W2043669844 cites W2047514666 @default.
• W2043669844 cites W2048598973 @default.
• W2043669844 cites W2051492374 @default.
• W2043669844 cites W2052128667 @default.
• W2043669844 cites W2052752441 @default.
• W2043669844 cites W2053062936 @default.
• W2043669844 cites W2053346328 @default.
• W2043669844 cites W2056668951 @default.
• W2043669844 cites W2081970557 @default.
• W2043669844 cites W2083138515 @default.
• W2043669844 cites W2084467958 @default.
• W2043669844 cites W2100977328 @default.
• W2043669844 cites W2102206214 @default.
• W2043669844 cites W2104520163 @default.
• W2043669844 cites W2105671109 @default.
• W2043669844 cites W2131767662 @default.
• W2043669844 cites W2137903293 @default.
• W2043669844 cites W2144031821 @default.
• W2043669844 cites W2157044024 @default.
• W2043669844 cites W2159878679 @default.
• W2043669844 cites W2160346204 @default.
• W2043669844 cites W2171797089 @default.
• W2043669844 cites W2186013783 @default.
• W2043669844 cites W2477029474 @default.
• W2043669844 cites W2482788638 @default.
• W2043669844 cites W2483522701 @default.
• W2043669844 cites W2486428660 @default.
• W2043669844 cites W2486687572 @default.
• W2043669844 cites W2488907713 @default.
• W2043669844 cites W2491004788 @default.
• W2043669844 cites W2494573222 @default.
• W2043669844 cites W2499511080 @default.
• W2043669844 cites W2501264094 @default.
• W2043669844 doi "https://doi.org/10.1016/j.pepi.2005.08.005" @default.
• W2043669844 hasPublicationYear "2006" @default.
• W2043669844 type Work @default.
• W2043669844 sameAs 2043669844 @default.
• W2043669844 citedByCount "14" @default.
• W2043669844 countsByYear W20436698442013 @default.
• W2043669844 countsByYear W20436698442015 @default.
• W2043669844 countsByYear W20436698442016 @default.
• W2043669844 countsByYear W20436698442018 @default.
• W2043669844 countsByYear W20436698442019 @default.
• W2043669844 crossrefType "journal-article" @default.
• W2043669844 hasAuthorship W2043669844A5032082605 @default.
• W2043669844 hasAuthorship W2043669844A5038416930 @default.
• W2043669844 hasAuthorship W2043669844A5047415607 @default.
• W2043669844 hasAuthorship W2043669844A5048135366 @default.
• W2043669844 hasAuthorship W2043669844A5048329245 @default.
• W2043669844 hasAuthorship W2043669844A5056391726 @default.
• W2043669844 hasAuthorship W2043669844A5058114925 @default.
• W2043669844 hasAuthorship W2043669844A5060907895 @default.
• W2043669844 hasAuthorship W2043669844A5061295464 @default.
• W2043669844 hasAuthorship W2043669844A5077329887 @default.
• W2043669844 hasConcept C115260700 @default.
• W2043669844 hasConcept C120806208 @default.
• W2043669844 hasConcept C121332964 @default.
• W2043669844 hasConcept C127313418 @default.
• W2043669844 hasConcept C127413603 @default.

• next