66 datasets found

Pelagic sedimentation during the Early Cretaceous at Site 603 produced alternations of laminated marly limestone and bioturbated limestone--a facies typical of the "Blake-Bahama...

From the upper 300 m of CRP-2/2A, twenty-six samples of diamicts and deformation structures have been thin sectioned. These have been analysed for texture, structure, diagenesis...

Five samples of diamicts from different levels of the Miocene part of the CRP-1 core have been thin sectioned. Observations in the thin sections relate to texture, diagenesis,...

Laboratory: Leibniz Labor, University of Kiel, Germany

This dataset contains the processed and raw data belonging to the organic geochemical analyses on cysts of the dinoflagellate Thalassiphora pelagica in sample 18H 17W 55-57 cm...

We present the rock magnetic and paleomagnetic data set from Site U1553 (including Holes A, B & E) recovered during IODP Expedition 378 in the southern Campbell Plateau...

Comparative pore water-sediment studies are crucial to trace biogeochemical and early diagenetic interactions between mineral and fluid phases. They are commonly conducted in...

We simulate the lithification process in the laboratory by consolidating mixtures of halite and shale powders with halite-saturated brine. We quantify lithification by: (1)...

Similar glacial-interglacial δ15N variations in two MIS 13-10 sediment sequences in the western North Atlantic Ocean

This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,...

This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,...

This Firt Order Reversal Curve was measured using the LakeShore Model 8600 vibrating sample magnetometer at the paleomagnetic laboratory of the Institute of Geomechanics,...

These First Order Reversal Curves were measured with a Princeton Measurement Corporation (PMC) Micromag M2900 alternating gradient force magnetometer at the Paleo- and Rock-...

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...

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 magnetic cycling provides complementary information on mineral magnetic properties. We used the Quantum Design MPMS-XL7 Magnetic Property Measurement System at...

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...

Measurements of acquisition of isothermal remanent magnetization (IRM) were conducted on a uniformly distributed subset of 65 discrete samples. We applied 22-step IRM...

Detailed alternating field (AF) demagnetization of Natural Remanent Magnetization (NRM) were conducted on discrete samples of IODP Site U1553. Thermal demagnetization were only...

AF demagnetization data of NRM were analyzed using anchored Principal Component Analysis (PCA) to obtain the Characteristic Remanent Magnetization (ChRM). Each sample was...