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Australia: The Land Where Time Began |
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Subduction – A
record of Spontaneous Initiation in the Izu-Bonin-Mariana Arc According to Arculus et
al. the subduction of
tectonic plates is poorly understood. If it is push from a distant
mid-ocean ridge or pull of a subducted plate it is expected there would
be compression and uplift of the overlying plate. Contrasting with this,
spontaneous initiation of subduction which is driven by the subsidence
of dense lithosphere along faults that are adjacent to the buoyant
lithosphere would result in extension and magmatism. Arculus et
al. say it typical for
younger deposits to obscure the record in the rocks of the initiation of
subduction with the result that the evaluation of these possibilities
has proven to be elusive. In this paper Arculus et
al. present the results of
their analysis of the igneous characteristic of igneous basement rocks
and overlying sediments, which had been sampled from the Amami Sankaku
Basin in the northwest Philippine Sea. The uppermost of the basement
rocks, which cover a widespread area, have been supplied by dykes. They
are similar in composition and age, being constrained by the sediments
which overlie them, to the basalts in the Izu-Bonin-Mariana forearc
which are 52-48 million years old. It is indicated by the geochemical
characteristics of the basement lavas there was a component of subducted
lithosphere involved in their genesis, and the mantle source rocks from
which the lavas were derived were more melt-depleted than those which
were tapped at mid-ocean ridges. Arculus et
al. propose that the
abasement lavas were formed during the inception of subduction of
Izu-Bonin-Mariana in a mode that is consistent with the spontaneous
initiation of subduction.
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| Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading | ||||||||||||||