A distant magmatic source for Cretaceous karst bauxites of Southern Apennines (Italy), revealed through SHRIMP zircon age dating
dc.contributor.author | Boni, Maria | |
dc.contributor.author | Reddy, Steven | |
dc.contributor.author | Mondillo, Nicola | |
dc.contributor.author | Balassone, Giuseppina | |
dc.contributor.author | Taylor, Rich | |
dc.date.accessioned | 2017-01-30T12:38:39Z | |
dc.date.available | 2017-01-30T12:38:39Z | |
dc.date.created | 2013-03-07T20:00:35Z | |
dc.date.issued | 2012 | |
dc.identifier.citation | Boni, Maria and Reddy, Steven and Mondillo, Nicola and Balassone, Giuseppina and Taylor, Rich. 2012. A distant magmatic source for Cretaceous karst bauxites of Southern Apennines (Italy), revealed through SHRIMP zircon age dating. Terra Nova 24 (4): pp. 326-332. | |
dc.identifier.uri | http://hdl.handle.net/20.500.11937/23683 | |
dc.identifier.doi | 10.1111/j.1365-3121.2012.01068.x | |
dc.description.abstract |
Karst bauxites occur at a Late Cretaceous hiatus on a Bahamian-type platform in Southern Apennines, Italy. In contrast to the well-defined stratigraphic context, their origin remains controversial. Detrital zircon grains preserve textures and Th/U ratios consistent with crystallization from a melt, occasionally around older cores. U-Pb isotopic data, collected using SHRIMP II, record several age populations. The youngest (~90 Ma) falls into the age interval of bauxite formation as defined by stratigraphic criteria. The zircons must therefore be derived from a contemporary Cretaceous volcanic source. The older zircons may be interpreted as xenocrysts associated with the Cretaceous magmas or derived from different sources. Because the bauxite occurs on a isolated carbonate platform, the grains must come from far away sources, most probably transported by wind. The age, palaeogeography and inferred Cretaceous wind pattern are consistent with a prevailing origin from the Dinaric and Carpatho-Balkan orogenic belts, with its Cretaceous bimodal volcanism. | |
dc.publisher | Blackwell Publishing Ltd | |
dc.title | A distant magmatic source for Cretaceous karst bauxites of Southern Apennines (Italy), revealed through SHRIMP zircon age dating | |
dc.type | Journal Article | |
dcterms.source.volume | 24 | |
dcterms.source.number | 4 | |
dcterms.source.startPage | 326 | |
dcterms.source.endPage | 332 | |
dcterms.source.issn | 0954-4879 | |
dcterms.source.title | Terra Nova | |
curtin.department | ||
curtin.accessStatus | Fulltext not available |