HR: 11:35h
AN: GP22A-06 [Abstracts]
TI: Toward an optimal geomagnetic field intensity determination technique: Testing the IZZI
protocol
AU: * Yu, Y
EM: yjyu@ucsd.edu
AU: Tauxe, L
EM: ltauxe@ucsd.edu
AB:
Paleointensity determinations based on double heating techniques (Aitken, Coe, and Thellier) are generally considered to be
functionally interchangeable, producing equally reliable paleointensity estimates. To investigate this premise, we have
developed a simple mathematical model. We find that both the zero-field first and in-field first methods have a strong
angular dependence on the laboratory field (parallel, orthogonal, and anti-parallel) while the two in-field steps method is
independent of the direction of the laboratory-produced field. Contrary to common practice, each method yields quite
different outcomes if the condition of reciprocity of blocking and unblocking temperatures is not met, even with marginal
(10%) tails of partial thermoremanence.
By far the best approach, however, is to alternatethe infield-zerofield (IZ) steps with zerofield-infield (ZI) steps.
We tested the IZZI method associated with the partial thermoremanent magnetization (pTRM) tail check.
As predicted, the IZZI method shows a strong angular dependence,
resulting from the undemagnetized portions of pTRM tails.
We also tested two fundamental assumptions
embedded in Thellier experiments,
the initial state dependence and
the effect of multi-cycle heat treatment.
We observed that the magnitude of pTRMs
with initial state of thermal demagnetization
was larger than that of pTRMs in Thellier analysis.
A multi-cycle Thellier analysis on coarse-grained magnetites
progressively produces more intense pTRMs
and progressively erases more pTRM tails.
Both pre-history and multi-cycle dependence will
likely to enhance the non-linear features of the Arai plot
for coarse-grained magnetites.
DE: 1512 Environmental magnetism
DE: 1521 Paleointensity
DE: 1527 Paleomagnetism applied to geologic processes
DE: 1540 Rock and mineral magnetism
DE: 1594 Instruments and techniques
SC: Geomagnetism and Paleomagnetism [GP]
MN: 2004 AGU Fall Meeting