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First order reversal curve (FORC) analysis of IODP sample U1553E-26X-3-W 43/4...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553B-22X-2-W 77/...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553B-5H-2-W 61/6...
This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,... -
First order reversal curve (FORC) analysis of IODP sample U1553E-1H-4-W 114/...
These First Order Reversal Curves were measured with a Princeton Measurement Corporation (PMC) Micromag M2900 alternating gradient force magnetometer at the Paleo- and Rock-... -
Statistical analysis of sedimentary and diagenetic factors for NRM Interpreta...
Five bivariate abundance analyses investigate, to which extent paleomagnetic interpretability (quantified by the quality indices N/R, NP/RP, NPP/RPP, N?/R? and INT), depend on... -
Magnetozone boundaries and assigned geomagnetic chrons of IODP Site 378-U1553...
Using the quality rating of polarity, we identified fifteen magnetozones, labeled as R0, N1, R1, …, N7, R7. The well-defined biostratigraphic frame enabled us to correlate the... -
Low-temperature thermomagnetic measurements of 11 sediment samples from IODP ...
Low-temperature magnetic cycling provides complementary information on mineral magnetic properties. We used the Quantum Design MPMS-XL7 Magnetic Property Measurement System at... -
Endmember analysis of IRM acquisition curves of 65 sediment samples of IODP S...
End-member unmixing using the algorithm of Heslop and Dillon (2007) (doi:10.1111/j.1365-246X.2007.03432.x) was performed on 65 normalized IRM acquisition curves to quantify... -
Isothermal remanent magnetization (IRM) acquisition curves of 65 sediment sam...
Measurements of acquisition of isothermal remanent magnetization (IRM) were conducted on a uniformly distributed subset of 65 discrete samples. We applied 22-step IRM... -
Stepwise NRM demagnetization data of 572 sediment samples from IODP Site 378-...
Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conducted on discrete samples of IODP Site U1553. Thermal demagnetization were only... -
Calcareous nannofossil abundance of IODP Site 378-U1553
999 means cf: taxonomic note: 'cf.' (= 'confer', in Latin: compare) -
d13C and d18O stable isotope records of IODP Site 378-U1553
This dataset has no description
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Organic Carbon Isotopes from bulk sediments recovered from IODP Site 378-U155...
Bulk sediment organic carbon isotopes, and total organic content values from IODP site 378-U1553 (166°11.4801′E, 52°13.4294′S) located on the Campbell Plateau are presented.... -
Late Paleocene - early Eocene calcareous nannofossil relative abundance count...
In this dataset, we show the raw relative abundance count data for calcareous nannofossils observed in sediment samples from International Ocean Discovery Program (IODP)... -
Chromium Reducible Sulfur isotopes from bulk sediments recovered from IODP Si...
Bulk sediment chromium reducible sulfur isotopes (CRS) from IODP site 378-U1553 (166°11.4801′E, 52°13.4294′S) located on the Campbell Plateau are presented. These data were... -
Bulk Carbonate Sulfur Isotopic Composition of Carbonate Associated Sulfate in...
Carbonate associated sulfate sulfur isotope results from IODP Site U1553 (166°11.4801′E, 52°13.4294′S) located on the Campbell Plateau are presented. Pore water and bulk... -
Sulfur and Oxygen Isotopic Composition of Dissolved Sulfate in Interstitial W...
Dissolved sulfate sulfur and oxygen isotope results and carbonate associated sulfate sulfur isotope results from IODP Site U1553 (166°11.4801′E, 52°13.4294′S) located on the...
