K-Ar ages determined for post-caldera volcanic products from Aso volcano, central Kyushu, Japan

被引:21
|
作者
Miyoshi, Masaya [1 ]
Sumino, Hirochika [2 ]
Miyabuchi, Yasuo [3 ]
Shinmura, Taro [4 ]
Mori, Yasushi [5 ]
Hasenaka, Toshiaki [6 ]
Furukawa, Kuniyuki [7 ]
Uno, Koji [8 ]
Nagao, Keisuke [2 ]
机构
[1] Univ Tokyo, Earthquake Res Inst, Bunkyo Ku, Tokyo 1130032, Japan
[2] Univ Tokyo, Grad Sch Sci, Geochem Res Ctr, Bunkyo Ku, Tokyo 1130033, Japan
[3] Kumamoto Univ, Fac Educ, Kumamoto 8608555, Japan
[4] Kumamoto Gakuen Univ, Fac Econ, Kumamoto 8628680, Japan
[5] Kitakyushu Museum Nat Hist & Human Hist, Kitakyushu, Fukuoka 8050071, Japan
[6] Kumamoto Univ, Grad Sch Sci & Technol, Kumamoto 8608555, Japan
[7] Aichi Gakuin Univ, Fac Business Adm, Nakamura Ku, Nagoya, Aichi 4538777, Japan
[8] Okayama Univ, Grad Sch Educ, Kita Ku, Okayama 7008530, Japan
关键词
K-Ar dating; Sensitivity method; Post-caldera volcanism; Aso volcano; LONG VALLEY; CONSTRAINTS; MAGMAS; ROCKS;
D O I
10.1016/j.jvolgeores.2012.04.003
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We determined the K-Ar ages for post-caldera lavas from Aso volcano in central Kyushu, Japan using the unspiked sensitivity method. The following three peaks of highly-frequent volcanism are recognized in the post-caldera stage: 70-50 ka, 40-20 ka and later than 10 ka. The two peaks of 70-50 ka and 40-20 ka are characterized by activities of compositionally diverse magmas from basalt to rhyolite. The volumes of silicic magmas are significantly larger than those of basalt magmas in these peaks. On the other hand, the peak later than 10 ka is characterized by predominantly basaltic eruptions without silicic magma activities. The active center of the silicic magma production (=crustal assimilation of injected basalt) had presumably migrated northeastward from the southwestern part of the caldera between the peaks of 70-50 ka and 40-20 ka. The predominant basaltic activity in the peak later than 10 ka represents that the production rate of silicic magma decreased, and does not indicate the accumulation of voluminous silicic magma beneath the recent Aso caldera. (C) 2012 Elsevier B.V. All rights reserved.
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页码:64 / 73
页数:10
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