Undersøgelsesmetoder Flashcards
Grain size distribution
Is it clay, silt, sand or gravel.
Longer the travel the finer and more mixed material.
Short distance will give more local material
Erratic boulders and indicator clasts
Fine gravel and coarse sand (?)
Give the same answer as indicator clasts.
300 grains categorised
Not much material needed - statistically useful
Upper part of till more weathered
Clast morphology
The roundness
Indicator of how it was transported.
Compared to similar types of clasts
Heavy minerals
(Relative age - how easily they weather )
Source area - Composition
Clay minerals
Only made by chemical weathering.
Origin and movement - best short transportation
(Clays can transform into other - indicate age)
Geochemistry
Hard rock
Signature geochemistry
Micromorphology
Microstructures - deformations ect.
Determine the environment
Different environments can give same structures
Magnetic susceptibility
Good for matching tills over long distances.
Magnetic alignment with the direction of the transport (elongated) - easy to measure like this
Also in boreholes
Geophysical investigations
Type of lithology.
(seismic profiles - TEM, borehole profiles - gamma and resistivity)