Table 2 Magnetic susceptibility and density of modelled upper crustal lithologies shown in Fig. 4f

From: Subglacial geology and palaeo flow of Pine Island Glacier from combining glacial erratics with geophysics

Name

Abbreviation in Fig. 4

Magnetic susceptibility (SI)

Density kgm−3

Background/Ice

BG/Ice

0.0000

2670

Volcanic

V1

0.0090

2670

Volcanic

V2

0.0160

2670

Volcanic

V3

0.0260

2800

Volcanic

V4

0.0110

2800

Hudson Mafic intrusion

M. Int 1

0.0015

2900

Hudson Granite

H. Granite

0.0040

2600

PIG Granite

PIG. Granite

0.0070

2600

Mafic intrusion 2

M. Int 2

0.0090

2700