A detailed tephrochronological study was carried out on the deep-sea core collected from Site 963A in the Sicily Channel during ODP Leg 160. The chronology of the succession is provided by an age–depth model based on isotope stratigraphy and quantitative eco-biostratigraphy. Major, trace and rare earth element content was obtained on single glass grains through electron probe micro-analysis and laser ablation–inductively coupled plasma mass spectrometry techniques from six well-preserved tephra layers, characterized by a discrete thickness found along the succession. These deposits were correlated with the volcanic activity of Pantelleria and dated at 42.5, 127.5, 128.1, 129.1, 188.7 and 197.7 ka. This detailed chemical characterization of...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ 18 O) anal...
Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptoteph...
A detailed tephrostratigraphy supported by accelerator mass spectrometry (AMS) 14C dating and isotop...
A detailed tephrochronological study was carried out on the deep-sea core collected from Site 963A i...
A detailed tephrochronological study was carried out on the deep-sea core collected from Site 963A i...
We present a major, trace and rare earth element characterization of single glass shards from fiftee...
Tephra layers from six deep-sea cores, recovered between the Ionian and the Aegean Seas, and coverin...
Distal tephrochronology relies on the synchronous dispersal and deposition of volcanic ash or tephra...
Isochronous tephra layers provide the potential for the precise correlation of environmental records...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ18O) analys...
Major, minor and trace element analysis of volcanic glass in proximal and distal (< 2 mm) tephra dep...
none3noA detailed chemical investigation of volcanic glass fragments from volcaniclastic strata (6 t...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ 18 O) anal...
Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptoteph...
A detailed tephrostratigraphy supported by accelerator mass spectrometry (AMS) 14C dating and isotop...
A detailed tephrochronological study was carried out on the deep-sea core collected from Site 963A i...
A detailed tephrochronological study was carried out on the deep-sea core collected from Site 963A i...
We present a major, trace and rare earth element characterization of single glass shards from fiftee...
Tephra layers from six deep-sea cores, recovered between the Ionian and the Aegean Seas, and coverin...
Distal tephrochronology relies on the synchronous dispersal and deposition of volcanic ash or tephra...
Isochronous tephra layers provide the potential for the precise correlation of environmental records...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ18O) analys...
Major, minor and trace element analysis of volcanic glass in proximal and distal (< 2 mm) tephra dep...
none3noA detailed chemical investigation of volcanic glass fragments from volcaniclastic strata (6 t...
International audienceA detailed tephrostratigraphic study supported by stable isotope (δ 18 O) anal...
Five cores from the southern Tyrrhenian and Ionian seas were studied for their tephra and cryptoteph...
A detailed tephrostratigraphy supported by accelerator mass spectrometry (AMS) 14C dating and isotop...