• 検索結果がありません。

十和田火山,噴火エピソードE及びG噴出物の放射性炭素年代

N/A
N/A
Protected

Academic year: 2021

シェア "十和田火山,噴火エピソードE及びG噴出物の放射性炭素年代"

Copied!
7
0
0

読み込み中.... (全文を見る)

全文

(1)ῒ῔  /-  (,**2)  0  +3-ῌ+33 . ΐ ῕.  

(2) E  G  N. ½. ,**2  , 8 +2 9 ,**2  ++ 8 +. 9. Radiocarbon Ages of the Eruptive Products from the Eruptive Episodes E and G, Towada Volcano, Northeast Japan Takashi KUDO῍ Towada volcano is an active volcano located at the northern part of the Northeast Japan arc. I carried out AMS radiocarbon dating of two soil samples taken from directly below the tephra layers derived from the eruptive episodes E and G at Towada volcano. The obtained +.C ages were 2++*-* BP (PLD-23+-) for the eruptive episode E (Nambu Pumice) and 331*-/ BP (PLD-23+.) for the eruptive episode G (Shingo Pumice). On the basis of the calibrated +.C ages and the stratigraphic relations, the most suitable ages of eruptive episodes E, F, G and Ninokura Scoria were estimated to be approximately 3.,, +*.,, ++ and ++.1ῌ+/./ cal kyr BP, respectively. These results enabled more detailed and reliable chronology of eruptive history during the post-caldera stage of Towada volcano. Key words : Towada volcano, eruptive episode E, eruptive episode G, AMS +.C dating, eruptive history. +ῌ ῐ ῎ ῑ ῏. :;.<

(3) =>?@A +.C . :;.BCDE>FG H ++ km.

(4) ."/ (+300) 0123 (+303) 45 (+31*). I

(5) J@A;.KLA M + :;.I. 67 (+31.) 4 (+310) / (+32-) Hayakawa.  

(6) // ka 

(7)  (//ῌ. (+32/) NEDO (+320) N23 (,**-) >OPQ R. +/ ka) <

(8) +/ kaST I - IUVWX>. YZQ[\ G3G ]Z^I W_` I;. aYZQbA (Hayakawa, +32/) :;.I;c. defWg>h^Z\iIKLj <

(9) kI. lmn Hayakawa (+32/) >Oj ;op Jq@. ;rJ!@A>":KLP\ s]KN . t#JEuGQ + vI ;defWg $>wYZ. x% (,**1)  sZyK +.C z& RI=J. {F3^ A B C u| }~lnJ'bQ()YZ. €> *‚,+ƒ (AMS) ,>OA +. C -.. QbA :;./I;.u0„GQ;I1 . J†‡b ˆ;defWg>bQsI‰2KŠi3. 456biII <

(10) K‹7‹Œ. 8u9:YZAJ;qG\ G3G ;defW. IŽK <1= ;Jj > GQ‘j Hayakawa,. g E u F >bQ ’<“‡A”?z@AuYZ •. +32/ ; Nx% ,**1 ;.–—I˜™šJ›B@. \‡ +.C IœCzDyZQb\. [žA‡;.I + KLAuŸ A ¡EI;JF. y\ :;.<

(11) >‘¢AžA‡;I. -@A\£> ¤¥I;GHJK[A¦¢§¨>I. + uGQ ;defWg G z©ª^ZA ]I;. «GQ‘ @AzLA sIKi;>?@A-.  JIKU¬­|>LYZA<

(12) ® I:.  ;I1 45¯° šJMA\£IžA‡±N. O=>U¬­|;zO UVWX3^ sI<I‹7. W_u‡A G\zPQ ²P‡hj4³5K¨´‡. {Iµ¶ J·¸KQ1=>¹º;z»]AU.  W_IœCu38‡;I;qzDyZA. VWX¼I¤R >1 GQbA y\ ]I;JE.  -*/ῌ2/01  !" +ῌ+ῌ+ # 1 $%&'()*+,- )*. AIST, Institute of Geology and Geoinformation, Geological Survey of Japan, Central 1, Higashi. +ῌ+ῌ+, Tsukuba, Ibaraki -*/ῌ2/01 Corresponding author : Takashi Kudo e-mail : kudo-taka@aist.go.jp.

(13) 7. 194. 8. Fig. +. Topographic map of Towada volcano showing the sampling site for +.C dating. A part of + : ,/,*** topographic map “Heraidake” published by the Geographical Survey Institute is used.  + +. C  /0 %1 . !"#$%&' ()*+ ,  / , +  -.. 9:;:<=>

(14) ?'@ABC DEFG@ 2H. 2IJKLM .* N ,1  . 3 O +.+ N ,  ,/. 4P3 +333 ; H4QR3 ,**15 S>TG3 . 5 L"#S 2 +5 AALUVWXYZB)[\. ]^_`a G %bc9d. '@ABU3 . @e\f /.1 m ghi\>jkEF 2 ,53 hl. mnop%qr'@hLCst>u@ . v3 ]^_`a C w xy 2z{3 +32-53 . 3 ]^_`a G o`|U7 4}6. ]^_`a D῍~\ (Hayakawa, +32/)3 ]^. (,**1) > DS +.C  + $€Lu3 v. _`a D ~\ 27 4}63 ,**153 ]^. <‚%ƒ&'@S„9Uo`|%

(15) '. _`a E xy (Hayakawa, +32/)3 ]^_`. >uTS. a F †~ (Hayakawa, +32/)3 ]^_`a. ‡ˆ3 ]^_`a E B G 9‰G3 XYZŠW) [ AMS. +.. C . %+”•%S LU. .  .

(16) . . G ‹Œxy (Hayakawa, +32/) vŽ‘’“ (Hayakawa, +32/) >„FS  9–S)[. —F˜™%š93 ]^_`a E, F, G, . !UxyŠWvŽ‹ŒxyŠW\› "#. ‘’“%œ3 žŸ%+T. S 2 ,5 !"# 9U3 —ŠhXYZ>). S S3 ¡¢poZ£9@m9. [ !

(17) ¤!¥¦L§!"#EFGAB%¨©. $§%N

(18) ?9ªGC«'@. 9GcG@ "#EFS)[! , $9ªG3 AMS &9v@ +.C. ,ῌ ῎ΐ῍῏ῐῑῒ. .  . !U´'3 µ¶·‹Œ¸. /(.  %+TS  U¬­•®¯°±4Z²9³ )S !U¹FCº»BG¼ῌ“p¢’ῌ¼½.

(19) R S T   E UV G W

(20) $ XYZ[2. 195. \]^_ `abDcdefNO-  gh 8 9:;% <= >?@AB CD>E AMS : NEC i +./S DH _PcdO- 01- +.C j. Kk_P lm no$p],-8. +.. C 2. qWO- C 2/ Libby $rs //02 _ +.. PqWO t +3/* u0v,-. BP *wO- cdxo$  ypK . +.. C  2ῌ 2ypz{. IntCal*. (Reimer et al., ,**.) yp|}~A CALIB /.*.+ (Stuiver and Reimer, +33-) _- ^€ . * yp$ +.C 2/ BPῌkyr BP yp 2K‚ƒ„2/ cal BPῌcal kyr BP NwM -     -ῌ+ 

(21) E.   E $ †‡ˆ$‰u0 2++* -* BP (PLD-23+-) $2/Š01-  + ‹1J. *  E KLM2/NOP   † Œ$Z  u0  01- 20**  ,/* BP GaK-,0+- : FGHI +31* 2-1*+1* BP (GaK-+*0/* : Hayakawa,+32/) ŠŽ,- ^€ ‹10 _1‘m=.. ’*cd“1-$*Ž” lm p ^“1 P_^_ •–01-2/  —$2/˜” /**-** ™jš_xoN^,- -ῌ, 

(22) G.   G $›œ †‡ˆ$‰u0 331* -/ BP (PLD-23+.) $2/Š01-  + ‹1J. *  G KLM2/NOP  Q   (,**1) K˜,P›œ †‡ˆ$‰u001 - 3--*-/ BP (PLD-0-11) ŠŽ,- •–01- 2/ —$2/˜” 0** žŸ _xoN^,Š 2/N¡¢L£$¤¥^ ¦ !§01^_ . . Q  (,**1)  R S T8¨4©As$ ª Kk_P «¬4K˜M­$® #*¯°"N#±“1M2²O- ‹‹* • –01-2/_P   E, F, G € ˜V$$³«C´3$2µ¶%M .ῌ+ 

(23) E Fig. ,. Geological columnar section at the sampling site. Numerals in rectangles are +.C date. Alphabets represent the name of eruptive episodes. Words in parentheses represent the name of eruptive units.  ,  !"#$"%&' ()*+,-. / 01- +.C 2/ 34567     

(24) . Q  (,**1)   E $2NO P Hayakawa (+32/) K˜M 2-1*+1* BP $2/ O- ­OP ‹$$ d +-C /Z$·¸ /*ŽM,/(Stuiver and Polach, +311) N¹dOP yp]^_   E $2€€˜­ 3.. cal kyr BP NO- OuO ‹$2/ º»Š&y. ¼F½„ lm pŠ^“1P_^_-§ ˜”.

(25) !. 196 Table +.. ". Results of AMS+.C dating..  + AMS +.C . #$%& &' +.C ()*+. ,-./012 -3 !. -4 56 AMS 73789:-;. <  (,**1) 78=>>?@ . A B-#-- C.  

(26)   . 78D /**

(27) -** E3. ! <  (,**1) @ FGH)I E J7K G. L:@ B#MNO@POQ. . & W#X@Y$Z @[%&\Z. ]^D8 JJ7W +* cal kyr BP  56 E  G. _` - Wab@'OZ  L. -c(L78 c& F ]^. d@ eDfghi)j@*+&. D8, E F J7K G klRST-mn.  73 op-O@! <  (,**1) -. 561t 2. RSTU!,V" F . / qr/0OfV()*s]^D  F @ +*.+

(28) +*.. cal kyr BP 1t@2 +*., cal kyr. -34OZ _`  56 . BP 3 L@! <  (,**1) ]^8u. @JJ7W 3.* cal kyr BP  + OZ8 5l1t. v

(29) 3. @JJ7W 3., cal kyr BP  . .ῌ-  G. !  <  (,**1) @ FGH)I G . .ῌ,  F. . ! <  (,**1) @ FGH)I F =>.  3--* -/ BP (PLD-0-11) w# 6s JJ. >?,x!,s 2++* -* BP (PLD-0-13) . 7W +*.0 cal kyr BP  y& 56. 7z  s! <  (,**1) @ {x. @ 331* -/ BP  C  78D 0**  u|}. RSTRSTU!,V~ L. 3 5l€ h@ yOZ . - F @E2‚. & :-„ #X@Y$Z _` -.   ƒ". s3 L@ 56  {B89 †‡. Wab@'OZ  op-O@ 5l1t.  FGH)I E ,xy:J8 F . 2 -34OZ _`  56. @E2‚. . ˆ! <  (,**1) . ‰Š2  -3 ! <  (,**1) 7 =. @JJ7W ++.. cal kyr BP  + OZ. 8 5l1t@JJ7W ++ cal kyr BP  . >>?@ E;‹./Ds. .ῌ.

(30) . 01-Z  Œ q)Ž@ =>. <Ž‘’@=“”xŽ‘’f ”x>?. >?f•–>—˜™~-š?› {B. fœOZ8 L@^@žAŸ (T¡–. !,-W¢BC&D£¤¥ ]¦N{ f§.  FGH)I L ,›s¨48 FGH)I. E!,-©ª2 «¬OZ  W­ ®¯}!. G  Hayakawa, +32/ ;   ,**-. ,f@E;‹O./ °±1-Z  /0mn. ! <  (,**1) @ FGH)I L J7K G . c&²3L³ ! <  (,**1) -Y$. 78 <Ž‘’ ´pµJJ7W +/ῌ++. ƒ+/0O@ fV / cm =>>?-¶rE. cal kyr BP · 56 FGH)I G . F¸!,GQH`3 ¹r-+& L. -c(D ' Horiuchi et al. (,**1) . L@ {º7ˆ»¼½ŽO=>>?,x!. 78 FGH)I L  AMS +.C -7zL.

(31)    :;<=> E ? G @ABCD. 197. %4 &'()*EF#6GHI"J KL1 Horiuchi et al. (,**1) .  :;<=> L  M NOPQRQS , EF#6 +.. C T"JK# U5V5WX / . 4  ". +/./ cal kyr BP %01 7. . !Y Z[\ NEG51QS4"451 G\]^  "_06#$%#$`5$ 7 "a b$% &'()*@+cd. U +/./ cal kyr BP %K$ e% &'()*% G fghi,E. ,ῌ+. cm &jklmnb$ .   ,**1 E-G ,&jOP!

(32) EF#6 . opq'`51 % / rs()kt= u4 U *.*, cmῌ%vPG45$ 7OP !

(33) " #$% &'()*% G +,,-. +**ῌ 1** ,%w@`5$ &jklxyE^*z06#. $r='"2+06W{+,,-"a 0  :; <=> G " ++ cal kyr BP %b$% &'() *@+|d.U ++.1 cal kyr BP %K$ } |^  &'()*  @+.U +/./ῌ ++.1 cal kyr BP %K$ / 

(34)  . ,\q'01 " #601 .

(35)  " - E_b ~1 €E. :;<=>E‚$ ƒ„ ,-` †€E  "%L1" . E_b }c\.

(36)   ‡.EF#6ˆ‰$%%GE ŠE% GK‹ //

(37) 0zEF#6Œ,b$ K 1 2KŒ,.  (,**1) \GJKL1l 77 \.q'`51EŽR ^0Œ,b$  \. +/./ cal kyr BP E‘7L1  :; <=> L E^ ’nv45$  “”l ”•`51 (Hayakawa, +32/)

(38)  –3 .U4

(39) 4—˜`51 (Hayakawa, +32/) ™– 3. šE›5œž œŸ ŸE$$¡6K'(). Fig. -. Chronology of eruptive history during the post-caldera stage of Towada volcano. Ages : *, Machida et al. (+32+) and Hayakawa and Koyama (+332) ; **, Kudo and Sasaki (,**1) ; ***, Kudo et al. (,**-) ; ****, this paper ; *****, Horiuchi et al. (,**1).  - 

(40)      : *   (+32+)  (+332) ; **   (,**1) ; ***   (,**-) ; ****  ; ***** Horiuchi et al. (,**1).. * ¢@ &'()* 

(41) £K$7 œ    @E$•k ”•\ 89 Ž‚45$ Hayakawa, +32/ ; Hunter and Blake, +33/ ; 89 ,**- ,**. 7e:–3. U ++.1 cal kyr BP. ~\.

(42) \/06#1%2345$  . &'()*@}¤. Ÿ Ÿ¥•l¦§¦. -2** ,¡#1%2345$  - 7+. ¨š©E0zb$%%GE Hunter and Blake, +33/ ; 8. E. ªK%G ++ p N l«;+,,¬\. 9 +333 ; 8­® ,**1  2¯l^<. /01%23456#$7%4 89 ,**-. 6EK^ °)±=¯ %Ÿ Ÿ²³´ lµ¶. U -/* ,¬\ l/06#1%·`5. b$‹EKL1 (Hayakawa, +32/) ~¸ ++ cal kyr BP. $ ¹ºE.U5}|/

(43) \ l/06#1%=. E G   l‘7L1

(44)  +*., cal kyr BP E F, 3., cal. »`56^    ,**1 +/./ῌ++.1 cal kyr. kyr BP E E, 2., cal kyr BP E D, 1./ cal kyr BP E D῍ 0.+. BP E. -/* }c>¼6?#+,,¬\ l½/. cal kyr BP E C  l‘7L1 7+. 1**ῌ+.**.

(45) ). 198.  0 .    *+,'- E ./ G 012345 AMS +.C 678 "  *+,'- E 9 :; 2++*

(46) -* BP,  *+,'- G <9 :; 331*

(47) -/ BP  =:!" >?:!"6@  *+ ,'- E F G (ABC6DEF  G678" HIJ KLMN ! O "#. !P  ; H!Q!RH E : 3.,. cal kyr BP, F : +*., cal kyr BP, G : ++ cal kyr BP, (. ABC : ++.1ῌ+/./ cal kyr BP O8" >? Fig. .. Temporal variations of repose time before eruption during the post-caldera stage of Towada volcano.  .     . IJRS  RS$T U%=V&OS '() '*+, WX=RS-Y8" > Z!:'[ 6@  '*+,  \. ]^]/0_ O`a345bc61d    e2f(0gOH_ 3h6i-F5 4j"4. 4,_kL ='*F5S (ABC O5lmO _k;-:6F  +,;. n7F54  - R/ . .  op61dq"S rstuvwx.

(48). C  ; 8 -.** _y"5l96. z{ :|;};<=~:€>4"454. 6‚ƒL ,.1 cal kyr BP  B  ='*F H.  %„ †.?‡ˆ;} ‰@o  ŠA‹ŒBC.  8 +1** _6‚ƒLDE 3+/  A . FŽ GH R/IJŠA‹; K>6GL. =‘Z8"  - C ’O5lmO _k;. mMLN“A”•–64"4" ZZ—F5O. :6F  +,;n7F54R˜™. š›œPFMžm.  . . QR9WX6˜O ) {: (,**1) =ŸS F"R OON _k=6F  ' *+,=]2mWX=^d:!  . 7šON _: C 5; OON _k=`6F54  . C ’N _k ;6F54N C-B _=f¤9 64"d H!’Rij L;š85 4  . Z!; C ’© e2f(0gª:  =q8"ZO6«¬m C  L;­8 . km W ¡®¯'[' q4; =°0 !. "On !54 (Hayakawa, +32/) Z!=o]^ ]±²³´µ6p™ e2f(0g ¶6N":F "V&q=q FF >OZ·H3h6rm ;¸8544 > P *+,'-st 6DEF"ML  '*+,  \. ]^]/ 0_ `a345bc674    e2f(0gOH_ 3h 345i-F54j"4Ob™54.    T?U V (+32-)  WX01YZ[ \ ,/0   ,2 ,0-ῌ,1-. Hayakawa, Y. (+32/) Pyroclastic geology of Towada volcano. Bull. Earthq. Res. Inst. 0*, /*1ῌ/3,. T?U Vabc (+332) =K¡6; ƒL +* d  e¢4L‘Z8"3H £=# Ogh  .- .*-ῌ.*1. k¢l¥?¦§ (+300) +*** f(¨m'  !"# 

(49) $%&'( no. +.* +*ῌ ,2. Horiuchi, K., Sonoda, S., Matsuzaki, H. and Ohyama, M. (,**1) Radiocarbon analysis of tree rings from a +/./-cal kyr BP pyroclastically buried forest : a pilot study. Radiocarbon, .3, ++,-ῌ++-,. Hunter, A.G. and Blake, S. (+33/) Petrogenetic evolution of a transitional tholeiitic  calc-alkaline series : Towada volcano, Japan. Jour. Petrol., -0, +/13ῌ0*/. ) {:| (,**1)   su¹v, U%

(50) º ++0 0/-ῌ00-. ) ŒB CWwxV (,**-) yz» ¼ M½ 0*** _ e2U

(51) $º +*3 +/+ῌ+0/..

(52)   

(53)  E  G    (+333)   !"#$% 2 345 6789:; /* 033ῌ1+*.   (,**-)  )CDEFG H?IJ KLM)CDEFG$ NO 45  .2 ,.3ῌ,/2.   (,**.)  )C$PQ PRSTD  .3 -01ῌ-2+. UVWX (,**1)   !"#$Y Z[0 \]^_`RFaGb  45 c. GdGef no. ++ +/3ῌ+1,. g Yh

(54) ij k (+32+) 1lmnop qrst# AB /+ /0,ῌ/03. uh v*+ ,wxyz{|, (+303) }j ~€‚ƒ„ ?1< =>? +.C  (/*) 6@AB ,. ,0.ῌ,00. NEDO Y

(55) †!‡ˆ‰Š‹Œ (+320) ( 0*  Ž6‘’“ˆ‰89 < , ” ‘•–— 6˜™šR ῌ ›œ 6˜ 89  ž8 9Ÿ ¡ 2.p. &'()  ¨©ª  (+31.)   b %2  +. C 1<=>? +.C  (30) 6@AB ,2 33ῌ+**.. 199. &'()  *+ , (+31*) -./0 C   1 <=>? +.C ῍ (0,) 6@AB ,. ,-,ῌ ,--. Reimer, P. J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C. J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, F.G., Manning, S.W., Ramsey, C.B., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J. and Weyhenmeyer, C.E. (,**.) IntCal *. terrestrial radiocarbon age calibration, ,0ῌ* ka BP. Radiocarbon, .0, +*,3ῌ+*/2. Stuiver, M. and Polach, H.A. (+311) Discussion : reporting of +.C data. Radiocarbon, +3, -//ῌ-0-. Stuiver, M. and Reimer, P. J. (+33-) Extended +.C data base and revised CALIB -.* +.C age calibration program. Radiocarbon, -/, ,+/ῌ,-*. *() (+310) ›œ \¢£^¤¥$¦%§ «¬ ­®¯6°±²5\³´p }j~µB¶ · no. +/ +.ῌ+3. +.. ¸¹º »¼½.

(56)

Fig. . Topographic map of Towada volcano showing the sampling site for C dating. A part of : , topographic map “Heraidake” published by the Geographical Survey Institute is used.
Fig. . Geological columnar section at the sampling
Table . Results of AMS C dating.
Fig. . Chronology of eruptive history during the post-caldera stage of Towada volcano

参照

関連したドキュメント

We will give a different proof of a slightly weaker result, and then prove Theorem 7.3 below, which sharpens both results considerably; in both cases f denotes the canonical

(Furthermore, a bound on the number of elementary matrices can be found that depends only on n, and is universal for all fields.) In the case of fields, this can easily be

approah, whih is based on a step by step onstrution of the walks [6, 5℄.. We repeat in Setion 3 the proof

Amount of Remuneration, etc. The Company does not pay to Directors who concurrently serve as Executive Officer the remuneration paid to Directors. Therefore, “Number of Persons”

As a result of the Time Transient Response Analysis utilizing the Design Basis Ground Motion (Ss), the shear strain generated in the seismic wall that remained on and below the

1.1 E+09 2.7 E+07 6.6 E+08 7.6 E+07 - ※2 1.9 E+09. 各建屋滞留⽔の全αの放射性物質量評価[Bq] ※1

敷地からの距離 約48km 火山の形式・タイプ 成層火山..

敷地からの距離 約66km 火山の形式・タイプ 複成火山.. 活動年代