A decade-long rifting episode that began in the Krafla
volcanic system, north Iceland, in 1975 caused
substantial, regional, postevent anelastic deformation.
This was modeled as viscous relaxation in an
elastic/viscoelastic structure by Hofton and Foulger
[1996]. The results from modeling the
deformation detected in north Iceland have far-reaching
implications both for local and regional processes and
for the fundamental behavior of deformation around
spreading plate boundaries in general. Tilt in the
vicinity of the Krafla volcano fits the model well
after 1988/1989 which suggests that the
volcano magma chamber stopped inflating/deflating in 1988. A
viscosity of 0.8 x 10 Pa s was required to match the
local tilt data, less than that predicted for north Iceland
as a whole. Vertical motion measured using the Global
Positioning System (GPS) 1987-1992
around the ice cap Vatnajökull is inconsistent with isostatic
uplift. Using the elastic-viscoelastic model to predict
motion in other regions of Iceland suggests that the
deformation effects of the Krafla episode are significant
in many parts of Iceland and should be taken into account
when modeling deformation there. Though
not an realistic plate boundary model, interesting
complexities of the elastic-viscoelastic model are
highlighted by deformation modeling of an infinitely long
dike. This predicts that the amount of horizontal
displacement close to the dike may exceed the amount of
initial dike opening early in the spreading cycle. A
more realistic approximation to the plate boundary in
north Iceland, involving five overlapping
segments that experience dike emplacements at discrete
intervals, suggests that the width of the zone within which
transient, time-dependent deformation occurs may be several
hundred kilometers wide, considerably wider than the
neovolcanic zone. A kinematic approach to describing
plate motions is not appropriate close to spreading plate
boundaries and elsewhere where the viscosity of the Earth is low.
AGU Index Terms: 1206 Crustal Movements-interplate; Mineralogy, Petrology, and Rock Chemistry; 8150 Plate boundary-general; 8158 Plate motions-present and recent; 0000 Mineralogy, Petrology, and Rock Chemistry
Keywords/Free Terms: Spreading plate boundary, anelastic
JGR-Solid Earth 96JB02465
Vol. 101
, No. B11
, p. 25,423