ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • 129-802A; 24-238; 26-257; 27-261; 28-267; 29-283; 34-320B; 38-336; 49-412A; 52-418A; 54-427; 58-446; 61-462; 63-469; 65-483B; 67-495; 72-516F; 76-534A; 78-543A; 82-562; 82-564; Antarctic Ocean/BASIN; Antarctic Ocean/Tasman Sea; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//BASIN; Indian Ocean//FRACTURE ZONE; Indian Ocean//PLAIN; Joides Resolution; Leg129; Leg24; Leg26; Leg27; Leg28; Leg29; Leg34; Leg38; Leg49; Leg52; Leg54; Leg58; Leg61; Leg63; Leg65; Leg67; Leg72; Leg76; Leg78; Leg78AB; Leg82; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/FRACTURE ZONE; North Atlantic/Norwegian Sea; North Atlantic/RIDGE; North Pacific/ESCARPMENT; North Pacific/Gulf of California/CONT RISE; North Pacific/Philippine Sea/BASIN; North Pacific/TRENCH; North Pacific/TROUGH; North Pacific Ocean; Ocean Drilling Program; ODP; South Atlantic/CONT RISE; South Pacific/BASIN  (1)
  • 24-238; AGE; Coercivity; Curie temperature; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Hysteresis, coercivity of remanence/coercivity; Hysteresis, saturation magnetization/ saturation remanence; Hysteresis, saturation remanence; Indian Ocean//FRACTURE ZONE; Leg24; Natural remanent magnetization, Intensity per unit mass; Sample code/label; vibrating sample magnetometer (microVSM)  (1)
Collection
Keywords
Publisher
Years
  • 1
    Publication Date: 2023-06-27
    Keywords: 24-238; AGE; Coercivity; Curie temperature; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Hysteresis, coercivity of remanence/coercivity; Hysteresis, saturation magnetization/ saturation remanence; Hysteresis, saturation remanence; Indian Ocean//FRACTURE ZONE; Leg24; Natural remanent magnetization, Intensity per unit mass; Sample code/label; vibrating sample magnetometer (microVSM)
    Type: Dataset
    Format: text/tab-separated-values, 13 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Wang, Daming; Van der Voo, Rob; Peacor, Donald R (2005): Why is the remanent magnetic intensity of Cretaceous MORB so much higher than that of mid to late Cenozoic MORB? Geosphere, 1(3), 138-146, https://doi.org/10.1130/GES00024.1
    Publication Date: 2024-01-09
    Description: The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been recognized: maximum as well as average intensities are generally high for very young samples, falling off rather rapidly to less than half the recent values in samples between 10 and 30 Ma, whereupon they slowly rise in the early Tertiary and Cretaceous to values that approach those of the very young samples. NRM intensities measured in this study follow the same trends as those observed in previous publications. In this study, we take a statistical approach and examine whether this pattern can be explained by variations in one or more of all previously proposed mechanisms: chemical composition of the magnetic minerals, abundance of these magnetization carriers, vectorial superposition of parallel or antiparallel components of magnetization, magnetic grain or domain size patterns, low-temperature oxidation to titanomaghemite, or geomagnetic field behavior. We find that the samples do not show any compositional, petrological, rock-magnetic, or paleomagnetic patterns that can explain the trends. Geomagnetic field intensity is the only effect that cannot be directly tested on the same samples, but it shows a similar pattern as our measured NRM intensities. We therefore conclude that the geomagnetic field strength was, on-average, significantly greater during the Cretaceous than during the Oligocene and Miocene.
    Keywords: 129-802A; 24-238; 26-257; 27-261; 28-267; 29-283; 34-320B; 38-336; 49-412A; 52-418A; 54-427; 58-446; 61-462; 63-469; 65-483B; 67-495; 72-516F; 76-534A; 78-543A; 82-562; 82-564; Antarctic Ocean/BASIN; Antarctic Ocean/Tasman Sea; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//BASIN; Indian Ocean//FRACTURE ZONE; Indian Ocean//PLAIN; Joides Resolution; Leg129; Leg24; Leg26; Leg27; Leg28; Leg29; Leg34; Leg38; Leg49; Leg52; Leg54; Leg58; Leg61; Leg63; Leg65; Leg67; Leg72; Leg76; Leg78; Leg78AB; Leg82; North Atlantic/BASIN; North Atlantic/CONT RISE; North Atlantic/FRACTURE ZONE; North Atlantic/Norwegian Sea; North Atlantic/RIDGE; North Pacific/ESCARPMENT; North Pacific/Gulf of California/CONT RISE; North Pacific/Philippine Sea/BASIN; North Pacific/TRENCH; North Pacific/TROUGH; North Pacific Ocean; Ocean Drilling Program; ODP; South Atlantic/CONT RISE; South Pacific/BASIN
    Type: Dataset
    Format: application/zip, 25 datasets
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...