Please use this identifier to cite or link to this item:
https://hdl.handle.net/2440/13767
Citations | ||
Scopus | Web of Science® | Altmetric |
---|---|---|
?
|
?
|
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Alias, G. | - |
dc.contributor.author | Sandiford, M. | - |
dc.contributor.author | Hand, M. | - |
dc.contributor.author | Worley, B. | - |
dc.date.issued | 2002 | - |
dc.identifier.citation | Journal of Metamorphic Geology, 2002; 20(3):351-363 | - |
dc.identifier.issn | 0263-4929 | - |
dc.identifier.issn | 1525-1314 | - |
dc.identifier.uri | http://hdl.handle.net/2440/13767 | - |
dc.description | The definitive version is available at www.blackwell-synergy.com | - |
dc.description.abstract | Porphyroblastic schists in the thermal aureole of the Victor Harbor Granite at Petrel Cove, in the southern Adelaide Fold Belt, South Australia, preserve a record of sequential cordierite, andalusite, staurolite, fibrolite, chlorite and muscovite growth (along with biotite+plagioclase+quartz+ilmenite) during progressive deformation. A P–T pseudo-section appropriate to biotite-saturated assemblages in KFMASH shows that the sequence of mineral reactions records increasing pressure of at least 1 kbar (from c. 3 to c. 4 kbar) during cooling from around 580 °C. Heating at pressures below c. 3 kbar is inferred for growth of early formed cordierite porphyroblasts, and is attributed in part to the thermal effects of granite emplacement, while the pressure increase is attributed to tectonic burial accruing from ongoing deformation. The 'anticlockwise' P–T path is consistent with convergent deformation being focussed as a consequence of heating, as to be expected for a lithospheric rheology that is strongly temperature dependent. | - |
dc.description.statementofresponsibility | G Alias, M Sandiford, M Hand, B Worley | - |
dc.language.iso | en | - |
dc.publisher | Blackwell Science Inc | - |
dc.source.uri | http://www.blackwell-synergy.com/doi/abs/10.1046/j.1525-1314.2002.00373.x | - |
dc.title | The P-T record of synchronous magmatism, metamorphism and deformation at Petrel Cove, southern Adelaide Fold Belt | - |
dc.type | Journal article | - |
dc.identifier.doi | 10.1046/j.1525-1314.2002.00373.x | - |
pubs.publication-status | Published | - |
dc.identifier.orcid | Hand, M. [0000-0003-3743-9706] | - |
Appears in Collections: | Aurora harvest 7 Environment Institute publications Geology & Geophysics publications |
Files in This Item:
There are no files associated with this item.
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.