The AND-2A drillcore (Antarctic Drilling Program-ANDRILL) was successfully completed in late 2007 on the Antarctic continental margin (Southern McMurdo Sound, Ross Sea) with the aim of tracking ice proximal to shallow marine environmental fluctuations and to document the 20-Ma evolution of the Erebus Volcanic Province. Lava clasts and tephra layers from the AND-2A drillcore were investigated from a petrographic and stratigraphic point of view and analyzed by the Ar-40-Ar-39 laser technique in order to constrain the age model of the core and to gain information on the style and nature of sediment deposition in the Victoria Land Basin since Early Miocene. Ten out of 17 samples yielded statistically robust Ar-40-Ar-39 ages, indicating that the AND-2A drillcore recovered a parts per thousand currency sign230 m of Middle Miocene (similar to 128-358 m below sea floor, similar to 11.5-16.0 Ma) and > 780 m of Early Miocene (similar to 358-1093 m below sea floor, similar to 16.0-20.1 Ma). Results also highlight a nearly continuous stratigraphic record from at least 358 m below sea floor down hole, characterized by a mean sedimentation rate of similar to 19 cm/ka, possible oscillations of no more than a few hundreds of ka and a break within similar to 17.5-18.1 Ma. Comparison with available data from volcanic deposits on land, suggests that volcanic rocks within the AND-2A core were supplied from the south, possibly with source areas closer to the drill site for the upper core levels, and from 358 m below sea floor down hole, with the "proto-Mount Morning" as the main source.
40Ar–39Ar dating of volcanogenic products from the AND-2A core (ANDRILL Southern McMurdo Sound Project, Antarctica): correlations with the Erebus Volcanic Province and implications for the age model of the core
BRACCIALI, LAURA;ROCCHI, SERGIO
2010-01-01
Abstract
The AND-2A drillcore (Antarctic Drilling Program-ANDRILL) was successfully completed in late 2007 on the Antarctic continental margin (Southern McMurdo Sound, Ross Sea) with the aim of tracking ice proximal to shallow marine environmental fluctuations and to document the 20-Ma evolution of the Erebus Volcanic Province. Lava clasts and tephra layers from the AND-2A drillcore were investigated from a petrographic and stratigraphic point of view and analyzed by the Ar-40-Ar-39 laser technique in order to constrain the age model of the core and to gain information on the style and nature of sediment deposition in the Victoria Land Basin since Early Miocene. Ten out of 17 samples yielded statistically robust Ar-40-Ar-39 ages, indicating that the AND-2A drillcore recovered a parts per thousand currency sign230 m of Middle Miocene (similar to 128-358 m below sea floor, similar to 11.5-16.0 Ma) and > 780 m of Early Miocene (similar to 358-1093 m below sea floor, similar to 16.0-20.1 Ma). Results also highlight a nearly continuous stratigraphic record from at least 358 m below sea floor down hole, characterized by a mean sedimentation rate of similar to 19 cm/ka, possible oscillations of no more than a few hundreds of ka and a break within similar to 17.5-18.1 Ma. Comparison with available data from volcanic deposits on land, suggests that volcanic rocks within the AND-2A core were supplied from the south, possibly with source areas closer to the drill site for the upper core levels, and from 358 m below sea floor down hole, with the "proto-Mount Morning" as the main source.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
