Dataset - B2FIND

(Table 1) Sedimentology of the Pliocene section of the DSDP Feni Drift Site 9...

Ages younger than 8 Ma based on magnetic reversal stratigraphy using the timescale of Cande and Kent (1995, doi:10.1029/94JB03098), older than 8 Ma determined using the...

Magnetic susceptibility from IODP Hole 333-C0018A

Geocode = [m CSF-A] Top Core depth (below sea floor)

Volumetric low-field magnetic susceptibility measurements of sediments from I...

This dataset contains rock-magnetic measurements obtained from Plio–Pleistocene hemipelagic sediment samples recovered at IODP Site U1463 on the Northwest Shelf of Australia...

Rock and paleomagneitc measurements of PS67/197-1

The core was taken in 2005 during Polarstern cruise ANT-XXII/4 in the central Scotia Sea. Magnetic susceptibility, further paleomagnetic information and other proxies were...

Grain-size distribution and grain-size dependent magnetic susceptibility of s...

Since the weight percentages of (classifiable) IRD particles > 1 mm and (unclassifiable, but separable) IRD particles > 125 µm both largely underestimate the total content...

Rock magnetic properties of petrologically representative IRD particles in se...

In order to determine the bulk magnetic impact of all 22 classified IRD lithologies, the specific petromagnetic properties of each were investigated in detail. In order to...

Unclassified IRD susceptibility and content, porosity and grain density of se...

IRD content is commonly assessed by weighing the detrital particles of the >125µm or > 1mm sieve fractions or by counting the IRD particles of the latter. Here we present...