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Australia: The Land Where Time Began |
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Pacific Ocean
Volcanism Related to Deformation Linked to the Hawaiian-Emperor Bend According to O’Connor et
al. ocean islands, sea mounts
and volcanic ridges are believed to have formed above mantle plumes.
However, many volcanic features on the floor of the Pacific Ocean
(Koppers, 2011) cannot be explained by this mechanism, some of which
might have actually have be caused by cracks in the oceanic crust that
are linked to reorganisation of the plate motions (Koppers, 2011;
Winterer & Sandwell, 1987; Natland & Winterer, 2005).
There is a distinctive bend in the Hawaiian-Emperor volcanic chain that
has been linked to changes in the direction of movement of the Pacific
Plate (Gordon, Cox & Harter, 1978; Sharp & Clague, 2006), movement of
the Hawaiian plume (Tarduno et al., 2003; Steinberger, Southerland
& O’Connell, 2004; Tarduno, 2007), or a combination of both
(O’Connor et al., 2013). O'Connor et
al say that as there is no
independent record that dates precisely tectonic events affecting the
Pacific Plate these links are uncertain. In this paper O'Connor et
al. analyse the geochemical
characteristics of samples of lava that have been collected from the
Musicians Ridges, which are lines of volcanic seamounts that formed
close to the Hawaiian-Emperor bend. They found that the geochemical
signature differs from that of the typical ocean island Basalts, instead
resembling mid-ocean ridge basalts. O'Connor et
al. suggest the seamounts are
not related to mantle plume activity, having formed instead in an
extensional setting, which resulted from deformation of the Pacific
Plate. Dating by 40Ar/39Ar revealed that the
Musicians Ridges formed during time windows which are bracketed by the
time of formation of the Hawaiian-Emperor bend, 53-52 Ma and 48-47 Ma.
The conclusion reached by O'Connor et
al. is that the
Hawaiian-Emperor bend formed as the result of plate-mantle
reorganisation, which was potentially triggered by a series of
subduction events at the margins of the Pacific Plate.
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Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading |