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(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
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(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
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(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
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(Table 3) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
This dataset has no description
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(Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB ...
This dataset has no description
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(Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB ...
This dataset has no description
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(Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB ...
This dataset has no description
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(Table 2) Magnetic properties and oxidation state of titanomagnetite in MORB ...
This dataset has no description
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(Appendix A1) Magnetic hysteresis parameters for samples collected across pol...
Sediment depth (m) is composite depth (mcd) after St. John et al. (2004, doi:10.1016/j.margeo.2004.09.004) -
(Table 1) Magnetic properties for individual samples from ODP Hole 136-843B
We present rock magnetic data on 10 samples recovered from ODP Hole 843B. The 95-m.y.-old basalts have moderately high magnetization values, and Curie temperature measurements... -
(Table 2) Petrophysical, petrological, and geochemical characteristics of ODP...
Ocean Drilling Program Hole 990A penetrated 131 m of subaerially emplaced Paleocene flood basalts on the Southeast Greenland margin with a recovery of 74%. Shipboard P-wave... -
(Table T2) Rock magnetic parameters of ODP Leg 180 sites
Rock magnetic measurements were performed on sediments above 20 meters below seafloor (mbsf) (general) and above 2.5 mbsf (detailed) at Sites 1109, 1110, and 1115 (Ocean... -
(Table T1) Magnetic properties of MORB from ODP Leg 187 sites
The core samples of mid-ocean-ridge basalts (including Indian and Pacific type) recovered from the Southeast Indian Ridge (SEIR) area near the Australian Antarctic Discordance... -
(Table T1) Paleomagnetic characterization of ODP Hole 198-1213B basalts
Paleomagnetic measurements were made on 52 samples from the igneous section of Ocean Drilling Program Hole 1213B for the purpose of determining paleoinclination and polarity and... -
Magnetic and petrographic properties of ODP Site 120-747 (Table 1)
Carbonate sediments from the Kerguelen Plateau (ODP Leg 120) of Eocene to Pliocene age were investigated with rock magnetic, petrographic and geochemical methods to determine... -
Magnetic properties of the oceanic igneous rocks (Table 1)
Hysteresis measurements have been carried out on a suite of ocean-floor basalts with ages ranging from Quaternary to Cretaceous. Approximately linear, yet separate,... -
(Table 1) Magnetic hysteresis parameters for samples from ODP Hole 197-1203A
The signal/noise ratio (defined as the ratio of the total Ms to the Ms of the AGFM P1-type probe) is larger than five for all data points -
Hysteresis in the deformation of layered crystal structures
The aim of this proposal is to study the origin of the hysteresis effect in many layered crystal structures, in particular MAX-phases, such as Ti2AlC. This effect has been... -
Unemployment persistence: does the size of the shock matter? (replication data)
One of the stylized facts of unemployment is that shifts in its mean rate between decades and half-decades account for most of its variance. In this paper, we use a statistical... -
Small-system modelling of real wages, inflation, unemployment and output per ...
The relationships between real wages, output per capita, inflation and unemployment in Italy between 1970 and 1994 are modelled using a cointegrated vector autoregression. There...