RADIOCARBON DATING OF THE LAST VOLCANIC ERUPTIONS OF CIOMADUL VOLCANO, SOUTHEAST CARPATHIANS, EASTERN-CENTRAL EUROPE

被引:46
作者
Harangi, Sz [1 ]
Molnar, M. [2 ]
Vinkler, A. P. [1 ]
Kiss, B. [1 ]
Jull, A. J. T. [3 ]
Leonard, A. G. [3 ]
机构
[1] Eotvos Lorand Univ, Dept Petrol & Geochem, H-1117 Budapest, Hungary
[2] MTA ATOMKI, Hertelendi Ede Lab Environm Studies, Debrecen, Hungary
[3] Univ Arizona, NSF Arizona AMS Lab, Tucson, AZ 85721 USA
关键词
PANNONIAN REGION; QUATERNARY VOLCANISM; NEOGENE; CHARCOAL; SPECTROSCOPY; C-14; CONTAMINATION; REFLECTANCE; YELLOWSTONE; MOUNTAINS;
D O I
10.1017/S0033822200046580
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This paper provides new accelerator mass spectrometry (AMS) radiocarbon age data for the last volcanic events in the Carpathian-Pannonian region of eastern-central Europe. The eruption ages were determined on charcoal fragments collected from pumiceous pyroclastic flow deposits at 2 localities of the Ciomadul Volcano. Two charcoal samples from the southeastern margin of the volcano (Bixad locality) set the date of the last volcanic eruption to 27,200 +/- 260 yr BP (29,500 +/- 260 cal BC). On the other hand, our data show that the Tusnad pyroclastic flow deposit, previously considered as representing the youngest volcanic rock of the region, erupted at similar to 39,000 yr BP (similar to 41,300 cal BC). Thus, a period of dormancy more than 10,000 yr long might have elapsed between the 2 volcanic events. The different ages of the Tusnad and Bixad pyroclastic flow deposits are confirmed also by the geochemical data. The bulk pumices, groundmass glass, and the composition of the main mineral phases (plagioclase and amphibole) suggest eruption of slightly different magmas. Considering also the assumed long volcanic history (similar to 600 ka) of the Ciomadul, these data suggest that further detailed studies are necessary on this seemingly inactive volcano in order to evaluate the possible renewal of volcanic activity in the future.
引用
收藏
页码:1498 / 1507
页数:10
相关论文
共 36 条
[1]   The use of Raman spectroscopy to monitor the removal of humic substances from charcoal:: Quality control for 14C dating of charcoal [J].
Alon, D ;
Mintz, G ;
Cohen, I ;
Weiner, S ;
Boaretto, E .
RADIOCARBON, 2002, 44 (01) :1-11
[2]  
Carn SA, 2009, T AM GEOPHYS UNION, V90, P205, DOI DOI 10.1029/2009EO240001
[3]   Surface and bulk chemistry of charcoal obtained by vacuum pyrolysis of bark:: influence of feedstock moisture content [J].
Darmstadt, H ;
Pantea, D ;
Sümmchen, L ;
Roland, U ;
Kaliaguine, S ;
Roy, C .
JOURNAL OF ANALYTICAL AND APPLIED PYROLYSIS, 2000, 53 (01) :1-17
[4]  
Gansecki CA, 1998, GEOLOGY, V26, P343, DOI 10.1130/0091-7613(1998)026<0343:NAFTCE>2.3.CO
[5]  
2
[6]   FTIR spectroscopy and reflectance of modern charcoals and fungal decayed woods: implications for studies of inertinite in coals [J].
Guo, Y ;
Bustin, RM .
INTERNATIONAL JOURNAL OF COAL GEOLOGY, 1998, 37 (1-2) :29-53
[7]  
Harangi S., 2001, Acta Geologica Hungarica, V44, P223
[8]  
Harangi S, 2007, GEOL SOC AM SPEC PAP, V418, P67, DOI 10.1130/2007.2418(04)
[9]  
Hatté C, 2001, RADIOCARBON, V43, P177
[10]  
JUVIGNE E, 1994, CR ACAD SCI II, V318, P1233