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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 124 (1996), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An unconstrained 3-D micromagnetic model for magnetite grains with resolutions up to 23 × 23 × 63 is presented. The model has been used to investigate the magnetic domain states of submicron parallelepipeds with various elongations. The method of fast Fourier transformation (FFT) has been implemented in three dimensions to accelerate the computation of the magnetostatic energy and its gradient, assuming constant magnetization for each subcube of the model. A 3-D implementation of the exchange energy and its gradient, using a five-point formula to approximate the Laplace operator, was chosen. Special attention has been paid to single-domain (SD) or flower states and pseudo-single-domain (PSD) configurations. A circular configuration, called vortex state, has been found to have the lowest energy of various PSD states. As a local energy minimum (LEM), the free energy of the vortex state is compared to that of a single-domain state. A comparison of these energies is used to determine a lower and an upper threshold size for the SD to PSD transition. In the interval between these two threshold sizes both configurations, SD and PSD, coexist. Above the upper threshold size we found metastable double-vortex configurations which seem to represent three-domain structures with closure domains.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2023-04-28
    Description: Obtaining reliable information from even the most challenging paleomagnetic recorders, such as the oldest igneous rocks and meteorites, is paramount to open new windows into Earth's history. Currently, such information is acquired by simultaneously sensing millions of particles in small samples or single crystals using SQUID magnetometers. The obtained rock-magnetic signal is a statistical ensemble of grains potentially differing in reliability as paleomagnetic recorder due to variations in physical dimensions, chemistry and magnetic behavior. Here we go beyond bulk magnetic measurements and combine computed tomography and scanning magnetometry to uniquely invert for the magnetic moments of individual grains. This enables us to select and consider contributions of subsets of grains as a function of particle-specific selection criteria and avoid contributions that arise from particles that are altered, or contain unreliable magnetic carriers. This new, non-destructive, method unlocks information from complex paleomagnetic recorders that until now goes obscured.
    Type: Dataset
    Format: application/zip, 18.3 MBytes
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  • 3
    Publication Date: 2023-06-27
    Keywords: 151-911A; AGE; Calculated; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Ice rafted debris; Joides Resolution; Leg151; North Greenland Sea
    Type: Dataset
    Format: text/tab-separated-values, 406 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-04-28
    Description: There are six datasets in this contribution, all presented in the manuscript 'Micromagnetic Tomography for paleomagnetism and rock-magnetism'. The first dataset was measured with a Magnetic Tunneling Junction (MTJ) scanner using a synthetic sample after a pulsed magnetization of 1 Tesla was applied perpendicular to the surface of the sample (file names: mtj_synth_XXX). The second dataset was measured on a Quantum Diamond Microscope (QDM) using the same synthetic sample with a pulsed magnetization of 1 Tesla perpendicular to its surface (file names: qdm_synth_XXX). The four other datasets are regions on a volcanic sample that was not treated magnetically and measured with a QDM (file names: qdm_volc_areaY_XXX). For each of these datasets the following files are available: XXX_cuboids.txt contains a list of grains defined by groups of cuboids. xi, eta, and zeta define the midpoint of each cuboid that has sides 2a, 2b, and 2c, in the x, y, and z direction respectively, all dimensions are given in micrometers; the last column specifies the grain to which the cuboid belongs (particle index). XXX_BzUpGrid.txt contains the results of the magnetic surface scan of the sample in Tesla, with increasing x-coordinates in the horizontal direction, and increasing y coordinates in the vertical direction. The step size for the data-sets are as follows (all in micrometer and in both directions): mtj_synth 10 micrometer; qdm_synth 6.0 micrometer; qdm_volc 1.2 micrometer. XXX_magnetizations.txt contains the results of the magnetic inversions, i.e. the magnetizations per grain in A/m. The first column is the particle index, then the magnetizations in the x (mx), y (my), and z (mz) directions.
    Keywords: File content; File name; File size; HW03; MIMATOM; North Pacific Ocean, western part; paleomagnetism; Paleomagnetism and rock-magnetism by Micro-Magnetic Tomography; ROCK; rock-magnetism; Rock sample; Sample method; Sample type; scanning magnetometry; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 5
    Publication Date: 2023-06-27
    Description: The complete sediment series recovered during METEOR Cruise M 41/3 with the gravity corer were subject to laboratory geophysical studies. Shipboard measurements on the segmented cores routinely comprised three basic physical parameters: - compressional (p-) wave velocity vp, - electric resistivity Rs (as a measure of density and porosity), and, - magnetic volume susceptibility K. These properties are cIosely related to lithology and grain size of the sediments and provide high-resolution core logs (spacing 1 cm for p-wave velocity, 2 cm for eIectric resistivity and magnetic volume susceptibility) available prior to all other detailed investigations. In addition, oriented samples for subsequent shore-based rock and paleomagnetic studies were taken at routine intervals of 5 cm.
    Keywords: 06MT41_3; Angola Basin; Brazil Basin; GeoB; GeoB5110-4; GeoB5112-4; GeoB5115-1; GeoB5116-2; GeoB5117-1; GeoB5120-2; GeoB5121-1; GeoB5130-2; GeoB5131-1; GeoB5132-3; GeoB5133-1; GeoB5134-2; GeoB5135-2; GeoB5136-1; GeoB5137-2; GeoB5138-1; GeoB5139-2; GeoB5140-1; GeoB5142-1; Geosciences, University of Bremen; Gravity corer (Kiel type); M41/3; Meteor (1986); Northwestern Vema Channel; SL
    Type: Dataset
    Format: application/zip, 38 datasets
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Grøsfjeld, Kari; De Schepper, Stijn; Fabian, Karl; Husum, Katrine; Baranwal, Soma; Andreassen, Karin; Knies, Jochen (2014): Dating and palaeoenvironmental reconstruction of the sediments around the Miocene/Pliocene boundary in Yermak Plateau ODP Hole 911A using marine palynology. Palaeogeography, Palaeoclimatology, Palaeoecology, 414, 382-402, https://doi.org/10.1016/j.palaeo.2014.08.028
    Publication Date: 2024-01-09
    Description: The late Neogene evolution of the Arctic to Subarctic region is poorly understood due to few available records and poor age control. At the margin of the Arctic Ocean, Yermak Plateau Ocean Drilling Program (ODP) Hole 911A is strategically located for establishing a stratigraphic framework for the Arctic. Here we present dinoflagellate cyst and acritarch data from 24 stratigraphic levels in the lower part (474.26-505.64 metres below the seafloor (mbsf)) of ODP Hole 911A. The marine palynomorphs indicate a latest Miocene to earliest Pliocene age (between 5.8 and 5.0 Ma) for the base of the hole based on the co-occurrence of the dinoflagellate cyst Barssidinium evangelineae and acritarch Lavradosphaera crista. Our age estimate for the sediments can possibly be further refined to 5.0-5.33 Ma based on the presence of Achomosphaera andalousiensis suttonensis, which apparently has a range restricted to the Pliocene. An age close to the Miocene/Pliocene boundary agrees with the planktonic foraminifer data. Together with recently available magnetostratigraphic data, the base of the hole is likely to be placed at ~5.2 Ma. This new chronostratigraphy is a first step towards a better understanding of the late Neogene palaeoenvironment for the Yermak Plateau and also for the wider Arctic to Subarctic region. The terrestrial and fresh water palynomorphs were most likely redistributed and/or displaced from the shelf towards deeper parts of the basin during contourite deposition under the influence of the West Spitsbergen Current. The in situ marine dinoflagellate cyst assemblage contains a mixture of cool water and thermophilic taxa, indicating sea-ice free, cool-temperate, warmer than present conditions at the Yermak Plateau. Rivers were likely the source for the freshwater influence.
    Keywords: 151-911A; Achomosphaera andalousiensis andalousiensis; Achomosphaera andalousiensis suttonensis; Acritarcha; Acritarcha, standard error; Acritarcha indeterminata; Acritarcha per unit mass; Amiculosphaera umbraculum; Barssidinium evangelineae; Barssidinium graminosum; Barssidinium pliocenicum; Barssidinium spp.; Bitectatodinium raedwaldii; Bitectatodinium tepikiense; Botryococcus spp.; Brigantedinium spp.; Cymatiosphaera invaginata; Cymatiosphaera spp.; DEPTH, sediment/rock; Dinoflagellate cyst; Dinoflagellate cyst, standard error; Dinoflagellate cyst indeterminata; Dinoflagellate cyst per unit mass; Dinoflagellate cyst reworked; Dinoflagellate cyst reworked, standard error; Dinoflagellate cyst reworked per unit mass; DRILL; Drilling/drill rig; Dry mass; DSDP/ODP/IODP sample designation; Echinidinium euaxum; Filisphaera filifera; Filisphaera microornata; Foraminifera, linings; Habibacysta tectata; Impagidinium aculeatum; Impagidinium pallidum; Impagidinium patulum; Impagidinium sp.; Impagidinium spp.; Invertocysta lacrymosa; Invertocysta tabulata; Joides Resolution; Laboratory code/label; Lavradosphaera crista; Lavradosphaera lucifer; Leg151; Lejeunecysta mariae; Lejeunecysta spp.; Lingulodinium machaerophorum; Lycopodium clavatum, standard deviation; Lycopodium clavatum markers counted; Lycopodium clavatum spores per tablet; Lycopodium tablets; Nematosphaeropsis labyrinthus; North Greenland Sea; Number of taxa; Ocean Drilling Program; ODP; Operculodinium? eirikianum crebrum; Operculodinium? eirikianum eirikianum; Operculodinium centrocarpum; Operculodinium sp.; Pediastrum spp.; Pentapharsodinium dalei; Protoceratium reticulatum; Sample code/label; Selenopemphix dionaeacysta; Spiniferites elongatus; Spiniferites falcipedius; Spiniferites spp.; Sumatradinium sp.; Tasmanites; Trinovantedinium glorianum; Trinovantedinium variabile
    Type: Dataset
    Format: text/tab-separated-values, 1521 data points
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  • 7
    Publication Date: 2024-02-02
    Description: The complete sediment series recovered during METEOR Cruise M38/ 1 with the gravity corer were subject to laboratory geophysical studies. Shipboard measurements on the segmented cores routinely comprised three basic physical parameters: - compressional (p-) wave velocity vp, - electric resistivity Rs (as a measure of density and porosity), and, - magnetic volume susceptibility K. These properties are closely related to lithology and grain size of the sediments and provide high-resolution core logs (spacing 1 cm for p-wave velocity, 2 cm for electric resistivity and magnetic volume susceptibility) available prior to all other detailed investigations. In addition, oriented sampIes for subsequent shore based rock and paleomagnetic studies were taken at typically 5 cm intervals.
    Keywords: GeoB; GeoB4304-3; GeoB4305-3; GeoB4306-2; GeoB4307-3; GeoB4308-4; GeoB4310-2; GeoB4311-2; GeoB4312-2; GeoB4313-2; GeoB4314-1; GeoB4315-2; GeoB4317-2; GeoB4319-13; Geosciences, University of Bremen; Gravity corer (Kiel type); M38/1; Meteor (1986); Midatlantic Ridge; Northern Brasil Basin; SL
    Type: Dataset
    Format: application/zip, 39 datasets
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-02-02
    Description: A large fraction of the sediment series recovered during METEOR Cruise M 46/2 with the gravity corer were subject to laboratory geophysical studies. Shipboard measurements on the segmented cores routinely comprised three basic physical parameters: - compressional (p-) wave velocity vp, electric resistivity Rs (as a measure of density and porosity), and, magnetic volume susceptibility. These properties are closely related to lithology and grain size of the sediments and provide high- resolution core logs (spacing 1 cm for p-wave velocity, 2 cm for electric resistivity and magnetic volume susceptibility) available prior to all other detailed investigations. In addition, oriented samples for subsequent shore based rock and paleo-magnetic studies were taken at typically 5 cm intervals.
    Keywords: Argentine Basin; GeoB; GeoB6201-5; GeoB6202-7; GeoB6203-2; GeoB6204-3; GeoB6205-2; GeoB6205-3; GeoB6206-3; GeoB6207-1; GeoB6208-3; GeoB6209-1; GeoB6210-2; GeoB6211-2; GeoB6212-1; GeoB6213-2; GeoB6214-6; GeoB6216-2; GeoB6217-3; GeoB6218-3; GeoB6219-4; GeoB6220-2; GeoB6221-2; GeoB6222-1; GeoB6223-5; GeoB6224-2; GeoB6225-1; GeoB6227-1; GeoB6229-7; GeoB6230-2; GeoB6231-2; GeoB6232-2; GeoB6233-2; GeoB6234-2; Geosciences, University of Bremen; Gravity corer (Kiel type); M46/2; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 52 datasets
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2015-10-03
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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