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Australia: The Land Where Time Began |
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The Earliest
Evolved Crust on Earth Generated in Setting like Iceland It is not certain how the earliest continental
crust was formed on Earth at a time when it probably had a surface of
oceanic crust. The authors1 suggest the first continental
crust may have formed in a setting such as an oceanic island where
mantle upwelling generates magmas that crystallise to form new crust.
The character of Iceland, of the oceanic plateaux, is closest to
continental crust as it is anomalously thick (Allen et
al., 2002) and contains a
relatively high proportion of rocks (Jakobsson,
Jonasson et al. 2008) that are
sialic (silica-rich). Therefore, Iceland has been considered to be a
suitable analogue for the earliest continental crust to be generated
(Kroner, 1982). According to the authors1 the sialic rocks
from Iceland has a geochemical signature
(Carmichael, 1964; Muehlenbachs, Anderson & Sigvaldason, 1974;
Nicholson et al., 1991; Bindeman et
al., 2012) that is distinct
from that of the typical
Archaean rocks that have been found so far that date from about
3.9-2.5 Ga (Martin, Martin & Sigmarsson, 2008). Reimink et
al. report in this paper the
discovery of a tonalitic gneiss rock unit that is exceptionally well
preserved that dates to 4.02 Ga within the Acasta Gneiss Complex in
Canada. It was shown by geochemical analysis that iron enrichment,
negative Europium anomalies, patterns of unfractionated
rare-earth-elements, and magmatic zircons with low oxygen isotope
ratios. These geochemical characteristics are not like typical igneous
rocks from the Archaean, rather, they are strikingly similar to the
sialic rocks from Iceland, which implies that the formation of this
ancient rock unit was formed by magmatic processes at a shallow level
that include the assimilation of rocks that had previously been altered
by surface waters. Direct evidence for the earliest continental crust of
the Earth being formed in a tectonic setting comparable to that of
Iceland of the present has been provided by the data obtained by the
authors1.
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| Author: M.H.Monroe Email: admin@austhrutime.com Sources & Further reading | ||||||||||||||