FISSION-TRACK DATING OBSIDIANS IN CENTRAL AND NORTHERN ANATOLIA

被引:55
作者
BIGAZZI, G
YEGINGIL, Z
ERCAN, T
ODDONE, M
OZDOGAN, M
机构
[1] Istituto die Geocronologia e Geochimica Isotopica, Pisa, 36 56127, Via Cardinale Maffi
[2] Fen-Edebiyat Fakultesi, Çukurova Üniversitesi, Adana, 01330, Fizik Bölümü
[3] MTA Genel Müdürlüg, Ankara, Jeoloji Etüdleri Dairesi
[4] Dipartimento di Chimical Generale dell'Università, Pavia, 12 27100, Viale Taramelli
[5] Edebiyat Fakültesi, Istanbul Üniversitesi, Istanbul, Prehistorya Bölümü
关键词
FISSION TRACK DATING; CHRONOSTRATIGRAPHY OBSIDIAN; CENTRAL ANATOLIA; NORTHERN ANATOLIA; ACIGOL CALDERA; GOLLU DAGI;
D O I
10.1007/BF00301811
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Twenty obsidian samples from Central and North Anatolia were dated by the fission track method. Split samples analyzed in two different laboratories give consistent results. Data presented refer to three volcanic fields and are summarized as follows: Orta-Sakaeli (Northern Anatolia) obsidians with ages from complex near Ciftlik ages between 1.33-0.98 Ma; Acigol caldera (Central Anatolia) shows three age groups: (1) Eruptions of precaldera (Begazkoy) obsidians with ages 0.18-0.15 Ma; (2) Formation of the large intracaldera dome Kocadag-Taskesiktepe at about 0.08 Ma (uncorrected ''apparent'' age of 0.075 Ma); and (3) Acigol peripheral obsidian domes with plateau ages of 0.020 and 0.019 Ma, and an additional uncorrected age of 0.018 Ma form a distinct age group. This fission track parameters discriminate between the various obsidian sources of prehistoric obsidian artifacts.
引用
收藏
页码:588 / 595
页数:8
相关论文
共 22 条
[1]  
Bigazzi G., Oddone M., Datazione dello standard internazionale apatite del Fish Canyon Tuff, Rendiconti Soc Geol It, 13, pp. 133-134, (1990)
[2]  
Bigazzi G., Bonadonna F.P., Hadler Neto J.C., Contribution to statistics in fission track counting, Nucl Tracks Radiat Meas, 11, pp. 123-136, (1986)
[3]  
Bigazzi G., Dompnier E., Hadler Neto J.C., Poupeau G., Vulliez E., A reactor intercalibration for fission track dating and uranium micromapping, Nucl Tracks Radiat Meas, 15, pp. 755-757, (1988)
[4]  
Dewey J.F., Pitman W.C., Ryan W.B.F., Bonnin J., Plate tectonics and the evolution of the alpine system, Bull Geol Soc Am, 84, pp. 3137-3180, (1973)
[5]  
Ercan T., Yegingli Z., Bigazzi G., The obsidians: definition, characteristics and distribution in Anatolia
[6]  
geochemical features of Central Anatolian obsidians, Jeom Derg (Bulletin of Geomorphology), 17, pp. 71-83, (1989)
[7]  
Ercan T., Tokel S., Akbasli A., Yildirim T., Fisekci A., Selvi Y., Olmez M., Can B., Matsuda J.I., Ui T., Fujitani T., Fujitani T., Notsu K., Origin and evolution of the Cenozoic rocks around Hasan Dagi and Karaca (Central Anatolia), Jeom Derg (Bulletin of Geomorphology), 18, pp. 39-54, (1990)
[8]  
Fornaseri M., Malpieri L., Palmieri A.M., Taddeucci A., Analysis of obsidians from the late chalcolithic levels of Arslantepe (Malatya), Paleorient, 3, pp. 231-246, (1977)
[9]  
Hurford A.J., Green P.F., The zeta age calibration of fissiontrack dating, Isotope Geosci, 1, pp. 285-317, (1983)
[10]  
Innocenti F., Mazzuoli R., Pasquare G., Radicati di Brozolo F., Villari L., The Neogene calcalkaline volcanism of Central Anatolia: geochronological data on Kayseri-Nigde area, Geol Mag, 112, pp. 349-360, (1975)