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Recent Trends of Active Fault Investigation

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(1) , 35, 6 , 589-595, 2002 Econ. Environ. Geol., 35(6), 589-595, 2002.   . *.  

(2)   Recent Trends of Active Fault Investigation Mihn-Soo Oh* Korea Institute of Science and Technology Information Technology & Patent Information Analysis Dept. 52, Eoeun-Dong, Yuseong-Gu, Daejeon 305-806, Korea. .  . !M+ †B+ kl Gm1UV h") *+ uUV ƒ”• –- *U—V IJ f" ˜ %$ Bq uUV, Œf p$ Q de Ž _! *Q+ ™$g “šlIJ(capable fault)”!M+ †B' 2†+ AMj *Q. fault)”.   1915   (Alfred Wegener)  “ !"#”$ %&' () *+ 20, -. /01 234 “5.67(the theory of the plate tectonics)”! #0) *+ -.  89: !;+ & -5(<=)>! ?@&A BCD E 5 FGH$+ IJ! K>B-) !' L M -N! OPQ. IJ!R IS(fracture) TUV IS9$ WX  YZ *+ F[ IJ!M H\Q. IJ]  1UV ^+ _41UV `a -V . +b, c IJ! de4 f" $ LMg h"_ IJ i h"_ IJUV . j Q. h"_ IJ!R kl Gm1UV YZ(no)  BA) *&A %p$ YZ Bq IJ: rQ. h_IJ!M) ` s de!9g -N: tO + u] vw), I- IJ YZ Bq “”x “f"yz”' {| 5} ~UV ) *Q. €9$ ih"_ IJ!R -1 ‚UV ƒp „$ IJ †! Bq uUV IJ P_ !‡ ˆ ! YZ  BA- ‰] IJ: rQ. 2 BŠ IJ! h_IJUV 50‹ˆMj !+ IJf"! Œf p$ BD Ž_! * U, ^ V 4` -N OP! [‘’Q+ “ !Q. €4! !”$ LMg+ “h_IJ(active .   h_IJ 62/›†] œIž# „(Ÿ  ) ¡] {.6¢ £ .6 #G ¤N #G ~ #, ¥ 3# ¦ §¨¢ ©  £ H-ª  H- «„_ W$ h†‹+ V ¬UV+ ­® ž#¢$  H-ª «„_ W$ 1 †¯ u!Q. -K [° AM+ kl h_IJ Z±j ²£ ³! 0´c #‹B *- ‰ Eµ$ ž# H -ª$  ¶1 «_ W B‘f  ·K vwM ž#¢ ¤N #G ¸|  ¹! ¶1UV !;B  z º+ »!Q. a—V !a µ' ”¼ Z`g+ IJ  h_`H,  ½­, YZ¶ ¦ ˆ Avg+ IJ  ¾¿ £$  ´ À ¸|, !$ ¸ |  µ' ”¼ Z`g+ h_IJ 62/› †! ªX‹BÁK Q. . .  .   

(3) Â, Ã, ÄAQ, Å, ÆÇ ¦ ÈÉÊ £ ªN $g+ 1980 ËHÌ Í 14 - UV h_ . *Corresponding author: [email protected]. 589.

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(22) BV: 0.1≤S<1, CV: S<0.1D EZ[. \S, ]^_, `a, ef gh4 ij. b(., cd] *!k  # g: ;l(mno 5p 2000-8B) *k 1997 35,000 !"# %p3 50,000 !"# %pD J7hqU(, !k rHD 35,000 !"# %p3 h5 &j.. €9$ ö æFÆ.ø+ )P 4 <V ,(Holocene, -1UV ˜%,)‚$ YZ *  IJ: ~UV ) *U, [°AM+ Âö Ù½Z yø ~: L7)(H ) 2000-8Æ, 2000 6 23) *Q. ö Ù.(IAEA)ø+ h_IJ 5}~ UV Û )P 4$ !"! *+ F[, Þ -8þ S! *+ -=1 ­Ó: N F[, > IJ: LM G-Nh"! *+ F[ ¦ ? Q\ šlIJ Ï ÷’ F[ £: ~UV ) *Q. Ã] h_IJ 5}~UV )P 4$ h " 1! *+ IJUV A³] 1≤S(W@YZmj mm/year), B³] 0.1≤S<1 ¦ C³] S<0.1 £ IJ f" W@YZmj' ¶1UV ) *Q.  A$ , ÊZÊ, !»°, BAQ ¦ ÈÉÊ £ ] h_IJ 5}~: }jV ½- ‰) *Q. .  . )h_IJ: ´ !” Z`g+ 4  C1J$  C1æF · Jg62, GPS(Global Positioning System)' !† DGM(Digital Geological Mapping) ^+ DFM(Digital Fracture Mapping) £$  )IJj _, IJ ¾(segment)¿$ .  62, ”«I. 62, )IJ$  )N1 Ô: 1† ”, )- , ) IJ )›Ù 62 ¦ )IJ ÏÖÕ: Z -N¿1 Ï./ £$ ”g TD’ _ 1 · ¶1 -À' ¸|V Q. !>  { E- {| : S&9 vpx ¡Q.         IJ h"_ `H' 5I+ {| ~ { A+  ˜% IJ h"x  Y=mj ' Fv¤+ u!Q. IJ h"+ IJ$ ” P_’ ¢: UV ` e1UV  h" ' ´4+ u! ˜ª Ô!-K, G Ô: 1†• z º: F[+ ‚14 ÔUV tò• zj *Q. H, Q\ 4 IJ$ ”g ¾I‹& A IJ: I) *+ J Ï' Õ` Fv K zj *Q. )IJ ÏÕ$g {| ™] IJh" ÷L’ 1D À¢: MN` Ž `a - Ô$  ÏÖÕ ¼' ´4),  ´ 4’ ÏÖÕ À$ ` -1 ÷O¤†  ë_: 9P W+ u!Q. )IJ ÏÖÕ: Z -N¿1 Ô] Q ӏ, ûû Ô}V ÏÖÕ$ !†‹+  À¢! Q7, ^ û Ô}V ÏÕ Í .

(23) . 592. Z Q7Q. 4.1.1. [MQ iW=G Õ(U-Th-Pb. series :. CHIME method). [MQ iW=G Õ] ­(R)§T (S)§T 2! °, T£! BA ‹9 §T UVÒ ! ˆ ! ­§T UVÒ V t-‹- ‰ Eµ $ Ô2_ W=» vW Ô2_ iW= » ’ Q. H, U Th] `a - X¢ YY 2! ZGz$ *Bg -K [\ ã! *’Q. L Mg YY P_, ] ¦ X¢! ]‹+ $ g U UVGS$ m+ Th] ­§T4 U + Q\ ZiÒV YY ^] X¢¤V !" ’Q.  ¼ !„$+ 1! U Th 2! h"j i 1$g _BA ’Q. !a iW=» + G(system) Q ¨`G' t-9 ‚! -A 9g Ô2Ž W=: !;+ ÔaUV NX‹B, ?  ‚! ü79 ­§T §T h"j iÒ] p V 1V bQ. ! E b$ 2°+ ‚, H h "j iÒ! ‚$ LMg Y¿+  iÒ] § T €.$ LMg 8MNQ. !a °' !†9 1c ­§T §T: ª` Ô2Ž iW= ÷G Á’ 23 OP ' Õ• z *Q. V ->] )C1J {$ dt‹B *+ Æ, ò"¢ ^+ IJ9 Ԕ$ dt’ "Z – €.' !†` ÏÖÕ: zX, ‚ “Fþ ÏÔ2Ž Õ” ! !†‹B ƒQ, ef Pj [z “S!¿ ¶ ”(Thermal ionization mass spectrometry) ùOV Õ Ï ƒã ÍZ' gU, ˜%$+ “Qh] tj¼D iMjY ¶ ”(Multiple collector inductively coupled plasma mass spectrometry) ùOV Q k 7) ‚l À ñm! Ž ‹Q. ! Ô$  ÏÕ! Ž ÏÖÍZ+ € 1UV €. 510Z !¤ ‚! Eµ$  §T €.$ LMg z 100K ÍZ )6 j' n+ ÏÖ ¼' o: z *Q. 4.1.2. ESR(Electron Spin Resonance, „ ¹ 0) Õ „¹0] BŠ ¢ m$ 1’ Ô2Ž$  p Ó: Õ+ T Ô2Ž ¾ÏÖ Õ!Q. Zeller(1968) ©qUV - ¾Ï ÖÕ$ ! Ô: j !p, 1982 HÌ+ Ãr 1UV ÏÕ$ !†‹),  ‡ Ikeya(1993)$ 238. 230. 238. 238. 230. ” ˆs O„‹U, )6j' Ç+ ÏÖÕ ÍZ + 200K 400K  „!Q. IJ™Ð(fault clay)$g ° Å:   ¢V + UV, ¾ÏÖÕ$ ¸|  ] Å m$ 0l+ `a - ESR signals(the E', OHC, Al and Ti signals amongst others) ,  IJh" { „IY= †$ ”g 0(zero)! ’Q + u!Q. IJh" !‡$ ESR signal>] -A‚ ‚$ it` ESR signal , ™™ u+ u$ Ë' () *Q. ÏÕ ¼ë V IJh"   Î' A vwQ+ ™ ÏÖÕ  ¢(Å): x M N• z *Q+ ™: -) *Q. ESR ÏÖÕ Ô] 4 C1¢! º+ ¿J -á!A Y_J -á$ O8+ IJi-' !†` IJ h"' ¼+b y] Ô!j Q. ^ ƒp’ IJh" ESR z] ˜‡ IJ h" {$ ºB-+ Fa! * Eµ$ ! ÔUV + ÇBN À ˜‡ IJh" K: ¼ ’Q. 4.1.3. OSL(Optically Stimulated Lumine-scence) Õ  1996HÌ Ãr1UV ÏÖÕ$ !†‹   OSL ÏÕ ¼ë+ C1J$ dt’ Å,   ¦ {B| £ X¢! }~: à Y- ' -+ uUV, f€ "«!A C1-$g ? c }~: €v OSL )Æ 0(zero)UV ’ Qq  Z C1J$ ” }~! ‘-) q !‡ ÇY$ * + U, Th, K £ ÏÔ2_ –VHÌ €] Ô2 Ž$ ” ‚’ 1ª¶(equivalent dose): Õ ) ' ςª¶Ò(annual dose rate)V Aƒ „! OSL Ï ’Q. a—V OSL Ï+ Å!A , ^+ {B| £: åd C1J C1' -Q(Aitken, 1998;  † £, 2000; ,‡@ £, 2001;  †, 2002). OSL ÏÕ À )6j *+ ÕG + 50K „!Q. 4.1.4.. 14. C AMS(Accelerating Mass Spectro-metry,. m¶ ) Õ [Ç "Z – {$g C(carbon)] 4 Ï Õ$  ˆ! !†‹+ Ô2_ –Vg 5,730 €.' -) N(nitr-gen)UV UV, ‰–' d t+ ­® À ¢ ÏÖ Õ! ŽQ. )6 j *+ ÏÖÕ ÍZ+ z 100 ¤5$g 5~6K 14. 14.

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(25)  593  ¸z14 j. ‹, `$ ò` ÏÕ !Q. P¢Î Šv*+ "«] UV$  C .– À+  ¼ ”$ ÷3! ’Q. ”«I.$  ÏÕUV+ Û ¾Ï Õ + ‹N$ ”g @=: !; ‹-K, aA P¢ Î Œ) A9 ‰– l ‹N {I‹—V C T , Þ Ï Õ, ¦ > -= i £! j+ ‚! Fd$ LMg UV ’Q. À ¤ *Q. ¾Ï Õ] -N¿1 Ï. Ô$g –ù $ ²+ C Tj' kl Š) *+ t2 T ² u i% ‹9 Y-UV C: ‹N ‡  u {$g CHIME Ô, OSL Ô, ¦ C F’ ‚, H P¢Î Œ] ‡ F’ ‚: Õ AMS Ô: !†) *Q. • z *’Q. Ï Õ] -=14 — ÐÓ14 ! Ô Õ¼ë+ C1J$ dt’ t¢$ —$ ”g Õ+b, -=1 —UV+ I.  Ô2_ ‰–ÏÕ ¼V, 1UV+ C1 )”« ¾˜] H 29 C1J$ ` I! J C1' e1UV -+ u] vw t ‹—V ‚! Fd$ LMg F2 õK Y ¢! Œ] ' -Q. a—V ! ¼+ C Q. l ‚ d™ Y¿+ I. C1¢ Ð 1J9˜– C1”(C1 ‡ dt’ †¢ ް Ó1 —UV+ ™ÐX¢ Ó X¢6_, ¿ Õ ¼)' -&A ^+ 9˜ C1”(C1 j, ÐÓ¿ †! BA+ J(solum) (™x 1 „ Œ] †¢ ްA v t¢ Õ¼)' - šj, Ò, ph, – Tj(Si, Ca, Mg, K, Q. Na) £: > z *Q. 4.1.5. K-Ar ^+ Ar-Ar Õ -= i]  –Ò: ), ¾ÏÖ J¾ÏÖÕ+ }jV IJh" !‡$ =_ À *+ I. )jVHÌ Q\ )j$ Zë+ ’ IJ™Ð =_' Õ+ UV, J¤ I. ¾ÏÖ: .+ Ô!Q. ! F[ –Ò $ Ô2_ UVV 4” 1’ Ar(argon)Ê Ó: –j' . Z”g+ & ”z9 Y": !” Õ`  J P_Ï' Õ+ Ô!Q. + u! ¸z1!Q. K(potasium)+ -.-û: ._+ 8 –V Ç ˜%  £ ªN$g+ )j Pj' n+ | 6JX¢ Ç._ –!Q. K "Z – {$g GPS' !†` Q ´ -=)j „$ zW ÏÖÕ$ !†‹+ K+ „Î K 0.012%' ã- å „: 8+ ”«/«I. mappingÔUV , K+ Ï1UV Cax ArUV UVQ. !{ o] ¶1 À$  -1 _: ½0) $g 11.2% ArUV UV+ u: %&V ÏÖÕ *Q. : + u!Q.  !"    K-Ar ¦ Ar-Ar ÏÖÕ] !71UV K! dt IJ ¾¿R œIžG, c Ù žG$ ‹B *+ J!A X¢!9 ­( Q Ž-K,  ¶  h]! *), c ˜%$ K>BN J g ¤N #G ›1UV 6.61  (tectonic origin)  F[+    Ar! 99% ! ‹ Eµ 4 h_IJ(active fault): ½-: E$ ¸|V + $ Ô2_   Ar Ó: ´ + u! h_IJ ½­ {  s›UV,  6(œ) ’ [ {|Q. kl öË- Ï. ø$g h_IJ ž!' ÂQ. H Û A h_IJ! ύ‹Q œŸ ¯ EŒ- ž! !&A, Þ œŸ! K-Ar ÏÖÕ: zX) *Q. ‹- ‰ˆMj Q\ IJ gV û÷GV KA&A ^+ gV ¹ ÷G' `Ǐ ‹B Av¡ E$    4 IJ] H ! 3 IJ! l h" u +, V  Zë ¾‹+ uUV ), > h_IJ >V‘, 6.61  `H' ½0‘9, 4$ = ! Q\ IJ$ ” ¾I’ F[$j ¾’ uUV ‚ÇQ. _’ I.(’“, terrace) YZ z€‹BÁQ.   «ÜÝvÊ IJ] ¾ ž! W@ ”«I.+ & ”‚” •æ ÷L‹B AvA+ ”z9 Y" -€ –$ ” =_’ 12km jV ´4‹U, ¤ ӝIJG ¾¿ -=!—V, !' ´ !”Q+ u] ) -Î + 6.61 ½­V v Ú 10km ÂK uUV ) f", 4 ”z9 Y" ‡Y¿ £: ”+b ’  *Q(˜ Z¢ £, 1999). 14. 14. 14. 14. 14. 40. 40. 40. 40. . .  

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(27) 594. . #$ % &  ' 1970 ˀK ÜMj  –L £ ªN$ g6ãj -Nl”' g! Z ÔUV á2-N z G-NzK: !†` h_IJ: W -K K£•K ¼' o- ¤Q. a—V ˜% H  $g+ Ç| #¢ Ï÷’ IJ$  )-N1 À' %&V ` h_IJ$  W' j) *Q. H, - "«$ -N$ ” =_’ `a -1 Àx u&' !†` IJ ¹‚1 IJh" _: ”) *Q. `g [°$ ¸ | IJh" ¹‚1 _UV+ Û IJh" !$ z€’ ­® Y= † Ç_ þÿ, Þ IJJ  Â,.6' !† IJh" Ç_ þÿ, ¦ > Jg1 Àx .6-1 À' !† IJh"  Ç_ þÿ £: > z *Q. . &( !' IJh"$ ”g P_’ IJ9¤$ O8+ I J™Ð(fault clay) ^+ IJi-(fault gouge)$ åd ‹B *+ ™ÐX¢$  )- : '` h_IJ Y- h"' ¼+ Ô/V g, ™ÐX¢ )Ù(high-coercivity) áÙ (reverse polarity) _ ] ¿1 ²(chemical remanent magnetization)Vg IJ Y- h" !‡$ IJ: '+ tÎ$ ” =_‹—V, ¿ 1 ² =_ V IJ h"' - Q. aA ! ¼ë+ Q\ ¾ÏÖ Õ: ! †` : `Á + ¥l! *Q(Hailwood et . al., 1992). .   . -N] IJ f"$ ” OP+ uUVg, N Õ ¦ þÿ: Z”g+ )IJ ´ åx f" _ ¦ h_Ž_ `H' P 5I + u! {|Q. ¤$gj 21,' N¦9g GPS (Trimble XR model, zW&° ƒãG z cm !¤, )j ƒãG Ú 50cm !¤)$  ”«I. mapping Ô!  j‹) *U, À©° ^ Pathfinder Officex MS Office, Fieldmate £ SoftwareV k$g  ‚UV „©°' ) *U—V ¬UV ´ À $  )ã  ¼ ӝ¯ u!, !V 4 ).  IJ -1 ' !† h_IJ 62  ³m O„! „§’Q. h_IJ ×{1 62: '” -.6 À  database .‹), h_IJ ªN W! ´‹` h_IJ ÇY -Nl”' W• z *: u!Q. h_IJ ¶1 62 O„: Z”g+ „ µ4Ù] ¢7 Õ ^+ i h ئ! ¸|Q. aA ¤ k] !a 4Ù i$  Ø ¨Ú` & Ë1 IG$gK 62 /Ï. zX‹) *Q.  401 F1 lq: ©ª zj *+ N h_IJ$  62+ ¼ê « z º+ ³  !Q. aA ¤$g -N Ï.+ Ë 14 IG$ ¥, !' Z”g+ €j ¤$ å+ h_IJ ´ å ¦  =_, f" _ _1 ¶1 À ñm! [ {|—V 6mc X‹BÁ • u!Q. 2,000j$ >Bg9g ªN $g+ -¬Œ­®` ƒ “T!(-=j) -62(Paper Geological Mapping; PGM)Ô”$g9Digital Geological Mapping(DGM):V „æ) *U—V, ƒp „HÌ ¹ Á$g |.) *+ ­® - À zë¿ ¤-+ ¶¿ Œf  ¤$ !; B u!Q. ­® œIž Á, c Ù ž Á$g |. + Ë -€-62 -1 À+ 2y1U VA F1UV, ˆ Avg+ ¤ 51UV ¯.  à À ‹—V, 1 ¦ Ó1UV °R `- º+ ¶14 u!BÁ d: .«Q9 62 Ô: -¬Œ- -=j )$ GIS(Geological Information System)$ 2± zë-=þV  Β DGM 2†] a‡ ­® -À P$ ¸ z1!Q. . ! . ) h_IJ$  Ï./62] 1 ë ·K vwM )j ž¿$ L\ 4. P׿x  = .6¢ ¦ Ù # £ «„: Z”gj ¸| ¥¼ u!Q. h_IJ 62] ­® ž#¢ H- ª ¦ «„_ Wx P ÷L’ !—V  z |+ ²Q. c ž#¢ {$g „x „¿,.

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(29)  595 4 #$L: M4. &?I&, 353 3, p. 179¢ ÷L’ ž#] ¹¹#¢Vg [°Ph P 188.  ÷G' -) *Q. !a #¢ 3 H(2002) PQ# % )%R<. &?I&, 38  «_] Ic {|—V, Q\ BŠ Qj <NO 3 2, p. 279-291. , E<S, TUV, WO, E4, E

(30) F, <X, ªX‹BÁ Q. H ¥, %¶, ”{ ³!¥, ÙO <NO YN , Z[\, Z] (2002) A !GH 4 & „–, ¹I £: 3• E H- «„_ W ªX K 2# ^($ OSL )%. _`-I11a <bI  cdI(ef), gh gA gh%i, ‹BÁ  Eµ$ ! h_IJ ùO‡  z 5 24-25, p. 35-36. |+ ²• u!Q. TUV, E<S, <j, EkO, <NO (2001) Wl m h_IJ 62/Ï.' '” -Nl” › nopqr s 8 ^($ )%R<. `-I &, 103, p. 202-211.  Ç| €.] ¢7 14 -Nl” ©Ž http://www.asahi.com/science/news/ Ù! ¿ ¯ u!Q. http://www.eurekalert.org €j h_IJ åj, -.61 _, -NZ±j http://www.iaea.org/worldatom  ¶1  £! !;B-9 µ1 1 O„ http://www.koreath.net http://www.nrc.gov/NRC/CFR/PART100/part100appa.html ] ¢7 ž# «_ W$ {| ÀV h Aitken, M.J. 1998 An introduction to optical dating. †‹B l”Ô-!$ `• u!Q. Oxford Science Publications, Tokyo, 267p. ˜% ¤$g -m1UV OP+ ½­ 4.0 ! Buhay, W.M. et al. 1988 ESR dating of fault gouge; the effect of grain size. Quaternary Science Reviews, v. 7, p.  -Nh"] €j ˆ ! -N «„- vw, 5 FGH Q+ &°-K ) -Î.6f" Chen,515-522. J.H. and Wasserburg, G.J, (1988) High precision mass spectrometric determinations of U234 and Th230 ! hOQ+ 4†! ´‹B ) h_IJ$  -Application to Quaternary geology. Chemical Geology, 62/Ï. hO NX¯ u!Q. v. 70, 173p. ˜% ¤$g+ Ù {   Ï ¹"Ï Doblas, M. (1998) Slickenside kinematic indicators. Tectonophysics, v. 295, p. 187-197. .2ž æUV ¤ -æF$ 1D h_IJ Haliday, A.N., Lee, D.C., Christensen, J.N., Rehkaemper, 5}~ WÔ ùO ¦ „ H- -N«„_ M., Yi, W., Luo, X., Hall, C.M., Ballentine, C.J., Pettke, T. and Stirling, C. (1998) Applications of multiple col$ Åa: Âë+ -k ½0 £: ›8V hO lector-ICPMS to cosmochemistry, geochemistry, and Ï. NX {$ *U—V, ¬UV 2010F$+ [ paleoceanography. Geochimica et Cosmochimica Acta, p. 919-940. °j [° AýV h_IJ 5}~] ¢7 {. Ikeyav. 62, et al. (1982) Dating of a fault by Electron Spin Res6¢ .6 #G, ^+ œIžH- ª £ ¤N onance on intra fault materials. Science, v. 215, p. 1392$ ¸| ¶1 - À' 1UV ”¼• 1393. Lee, H.K. and Schwarcz, H.P. (1994) Criteria for complete z *: u!Q. zeroing of ESR signals during faulting of the San Gab. . . "#$%  (2000) 

(31) ,      .   2000-8(2000 6 23), 2p. ,  , Okada, A. (1999) !"#$% &' ( ) - *

(32) &+ ,-  ./ 0, &12, 2 3 3. p. 155-168. 45, 67 (1991) 8#$ 9:% ;<=>. & ?, 53, p. 44-48. @A, BCD, E

(33) F (1999) A !GH % 4  #$, &?I&, 35, p. 1-14. @A, E4, E

(34) F, BCD (1999) !" J&K. . riel fault zone, Southern California. Tectonophysics, v. 235, p. 317-337. Muhs, D.R., (2000) Dating marine terraces with relativeage and correlated-age methods. In Noller, J.S., Sower, J.M. and Lettis, W.R.(eds.) Quaternary geochronology: Methods and applications. AGU Reference Shelf 4, American Geophysical Union, p. 434-446. Schwarcz, H.P. and Lee, H.K. (1998) Electron Spin Resonance dating. In Sowers, J., Noller, J. and Lettis, W.J. (eds.) Dating and Earthquakes: review of Quarternary geochronology and its application to paleoseismology. U. S. Nuclear Reg. Comm. NUREG/CR 5562p..  8 19 tu, 2002 12 23 vwx.. 2002.

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