dc.creator |
Mcdougall, Ian |
|
dc.creator |
Maboko, Makenya A. H. |
|
dc.creator |
Symonds, Philip |
|
dc.creator |
McCulloch, Malcolm T. |
|
dc.creator |
Williams, I. S. |
|
dc.creator |
Kudrass, H. R. |
|
dc.date |
2016-05-12T15:22:54Z |
|
dc.date |
2016-05-12T15:22:54Z |
|
dc.date |
1994 |
|
dc.date.accessioned |
2018-03-27T08:57:07Z |
|
dc.date.available |
2018-03-27T08:57:07Z |
|
dc.identifier |
McDougall, I., Maboko, M.A.H., Symonds, P.A., McCulloch, M.T., Williams, I.S. and Kudrass, H.R., 1994. Dampier Ridge, Tasman Sea, as a stranded continental fragment∗. Australian Journal of Earth Sciences, 41(5), pp.395-406. |
|
dc.identifier |
http://hdl.handle.net/20.500.11810/2000 |
|
dc.identifier |
10.1080/08120099408728150 |
|
dc.identifier.uri |
http://hdl.handle.net/20.500.11810/2000 |
|
dc.description |
Full text can be accessed
http://www.tandfonline.com/doi/abs/10.1080/08120099408728150 |
|
dc.description |
Dredging of the Dampier Ridge recovered small fragments of granite, gabbro and sandstone. Dating of the igneous samples by the U-Pb, K-Ar and Rb-Sr methods yielded precise ages mainly in the range 250 to 270 Ma, mid-Permian. An imprecise Sm-Nd mineral age of approximately 310 Ma might reflect slightly earlier emplacement of the gabbro. A granitic fragment has a composition approximating that a manimum melt. Taken together with the Late Palaeozoic emplacement ages and other geochemical and geophysical data, the evidence strongly supports the conclusion that the Dampier Ridge is a continental fragment, formerly part of eastern Australia, with its present location a consequence of continential rifting and opening of the Tasman Basin by sea-floor spreading. |
|
dc.language |
en |
|
dc.publisher |
Taylor and Francis |
|
dc.subject |
Dampier Ridge |
|
dc.subject |
Geochemistry |
|
dc.subject |
Geochronology |
|
dc.subject |
Isotopic dating |
|
dc.subject |
Magmatism |
|
dc.subject |
Tasman Basin |
|
dc.title |
Dampier Ridge, Tasman Sea, as a stranded continental fragment |
|
dc.type |
Journal Article |
|