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http://uninews.unimelb.edu.au/articleid_287.html
Evidence of faulting, buckling and uplift can be clearly seen in the young sediment record from this region. The team obtained an age for the various faults and folds by using a combination of fossils and radioactive isotope dating methods.
The findings confirm that the young mountain building and earthquake activity began around 10 million years ago and continues to the present day.
"This young faulting and folding has had very important economic effects for Australia. The giant oil and gas fields of the Gippsland Basin are largely trapped in young geological deformations produced by the seismic activity.
Faulting, however, can also rupture the reservoirs and cause leakage.
Evidence of faulting, buckling and uplift can be clearly seen in the young sediment record from this region. The team obtained an age for the various faults and folds by using a combination of fossils and radioactive isotope dating methods.
The findings confirm that the young mountain building and earthquake activity began around 10 million years ago and continues to the present day.
"This young faulting and folding has had very important economic effects for Australia. The giant oil and gas fields of the Gippsland Basin are largely trapped in young geological deformations produced by the seismic activity.
QUOTE
http://www2b.abc.net.au/science/k2/stn/arc...pic1505220.shtm
ARC Professorial Fellow, Mike Sandiford, from the University of Melbourne’s School of Earth Sciences was recently awarded ARC funding for research aimed at understanding the forces that
drive the motion of the Earth’s tectonic plates and the distribution of stresses in the Earth’s crust that give rise to great earthquakes such as the magnitude 9 Boxing Day Sumatran quake.
Professor Sandiford says the research shows that as much as 10 per cent of the huge amounts of energy being created at plate connection points at Sumatra and Java are being transferred back
into our plate and causing major stresses.
“This is enough stress to contribute to mild earthquake activity in the central regions of the plate, such as in the Australian continent or central Indian Ocean, and provides us with clues as to why our plate has been slowly breaking up, he says.
“The Indian Ocean quakes are, in effect, leading to the active rupture of the Indo-Australian plate into separate Indian and Australian plates. This new research provides us with important
information about the stresses that are driving this drawn out tectonic plate divorce.
ARC Professorial Fellow, Mike Sandiford, from the University of Melbourne’s School of Earth Sciences was recently awarded ARC funding for research aimed at understanding the forces that
drive the motion of the Earth’s tectonic plates and the distribution of stresses in the Earth’s crust that give rise to great earthquakes such as the magnitude 9 Boxing Day Sumatran quake.
Professor Sandiford says the research shows that as much as 10 per cent of the huge amounts of energy being created at plate connection points at Sumatra and Java are being transferred back
into our plate and causing major stresses.
“This is enough stress to contribute to mild earthquake activity in the central regions of the plate, such as in the Australian continent or central Indian Ocean, and provides us with clues as to why our plate has been slowly breaking up, he says.
“The Indian Ocean quakes are, in effect, leading to the active rupture of the Indo-Australian plate into separate Indian and Australian plates. This new research provides us with important
information about the stresses that are driving this drawn out tectonic plate divorce.
http://www.swissinfo.org/eng/international...00000&ty=ti
September 12, 2007 - 4:25 PM
Big earthquake hits Indonesia
JAKARTA (Reuters) - A powerful earthquake of 8.2 magnitude struck Indonesia's Sumatra region on Wednesday, triggering tsunami warnings in the Indian Ocean, sparking panic in coastal areas across Southeast Asia and causing at least two deaths.
Indonesia issued two tsunami warnings, one after the first quake, and the second after a smaller tremor a few hours later in the same area.