Deformation and metamorphism of the Aileu formation, East Timor
Berry, RF (1979) Deformation and metamorphism of the Aileu formation, East Timor. Honours thesis, Flinders University of South Australia.
A 10 km wide coastal strip of the Aileu Formation was mapped in
detail. This section of the north coast of Timor lies 70 km south of
a recently active island arc and was chosen as a potential type
example of the deformation style in an arc-continent collision zone.
In addition a brief study was made of the petrography and chemistry of
altered igneous rocks from this coastal strip and igneous rocks of a
similar age from other regions in East Timor.
The Aileu Formation is composed of metamorphosed shales,
siltstones and arenites with minor limestones and basites. The metamorphic
grade of this formation is zoned from lower greenschist facies
in the southwest to upper almandine-amphibolite facies in the east.
Five structural phases are recognised. The first generation isa
cleavage or schistosity which predates the single prograde metamorphism.
No folds were found associated with this foliation and its significance
is unknown. The second deformation phase occurred in the Late Miocene.
It syn- and post-dates the prograde metamorphic event, produced tight
folds and transposed the compositional layering and early cleavage on
all scales. The last three deformation phases produced open to gentle
macroscopic folds. Correlations with structural data from other
formations suggest the third and fourth phases occurred in the Late
Miocene and the fifth deformation occurred in the Early Pleistocene.
The major high angle faults, which form the boundaries of the Aileu
Formation, were also active in the Early Pleistocene.
The amphibolites and altered dolerites of the Aileu Formation are
transitional, in composition, between alkaline and tholeiitic basalts.
Permian and Mesozoic basalts and dolerites from other regions in East
Timor include both alkaline and tholeiitic compositions. All these igneous rocks are characteristic of continental rift valleys and ocean
islands. However the associated sedimentary rocks were deposited on a
continental shelf or slope. There is no evidence that the Aileu
Formation or the Permian and Mesozoic formations were not formed on
the Australian continental margin.
The geology of Timor is consistent with its evolution as a rift
valley in the Late Palaeozoic and Early Mesozoic, and a trailing margin
from the Cretaceous to the Early Miocene. Structural data suggests a
Late Miocene arc-continent collision. There has been post-orogenic
uplift and minor additional deformation in the Plio-Pleistocene.
Comparison of Papua New Guinea with Timor suggests that the mobile belt
in arc-continent collisions is characterised by medium pressure metamorphism,
relatively coherent deformation style, and a short history of
orogenic activity. Little evidence of thrusting or imbrication has
been uncovered and their importance as deformation processes in this
environment remains speculative.
|Item Type:||Thesis (Honours)|
|Additional Information:||Copyright the Author - The University is continuing to endeavour to trace the copyright owner(s) and in the meantime this item has been reproduced here in good faith. We would be pleased to hear from the copyright owner(s).|
|Deposited By:||Ms Sue Li|
|Deposited On:||12 Aug 2011 12:42|
|Last Modified:||07 Sep 2012 14:25|
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