期刊
BULLETIN OF VOLCANOLOGY
卷 77, 期 9, 页码 -出版社
SPRINGER
DOI: 10.1007/s00445-015-0960-9
关键词
Samalas 1257 AD; Plinian eruption; Caldera-forming eruption; Phreatomagmatic eruption; Eruptive dynamics; Trace element analysis
资金
- NERC grant [NE/I013210/1]
- Institut National des Sciences de l'Univers-Centre National de la Recherche Scientifique programme, CT3-ALEA
- project ECRin
- project INSU-CNRS Artemis
- Natural Environment Research Council [NE/I013210/1] Funding Source: researchfish
- NERC [NE/I013210/1] Funding Source: UKRI
The 1257 A.D. caldera-forming eruption of Samalas (Lombok, Indonesia) was recently associated with the largest sulphate spike of the last 2 ky recorded in polar ice cores. It is suspected to have impacted climate both locally and at a global scale. Extensive fieldwork coupled with sedimentological, geochemical and physical analyses of eruptive products enabled us to provide new constraints on the stratigraphy and eruptive dynamics. This four-phase continuous eruption produced a total of 33-40 km(3) dense rock equivalent (DRE) of deposits, consisting of (i) 7-9 km(3) DRE of pumiceous plinian fall products, (ii) 16 km(3) DRE of pyroclastic density current deposits (PDC) and (iii) 8-9 km(3) DRE of co-PDC ash that settled over the surrounding islands and was identified as far as 660 km from the source on the flanks of Merapi volcano (Central Java). Widespread accretionary lapilli-rich deposits provide evidence of the occurrence of a violent phreatomagmatic phase during the eruption. With a peak mass eruption rate of 4.6x10(8)kg/s, a maximum plume height of 43 km and a dispersal index of 110,500 km(2), the 1257 A.D. eruption stands as the most powerful eruption of the last millennium. Eruption dynamics are consistent with an efficient dispersal of sulphur-rich aerosols across the globe. Remarkable reproducibility of trace element analysis on a few milligrammes of pumiceous tephra provides unequivocal evidence for the geochemical correlation of 1257 A.D. proximal reference products with distal tephra identified on surrounding islands. Hence, we identify and characterise a new prominent inter-regional chronostratigraphic tephra marker.
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