TURAM (Interpretasi)

8/17/2019 TURAM (Interpretasi)

1/20

Turam

PRESENTED BY :

MANDALA TU NGG U L S INAG A 135090707111002

HAD I T WIBO WO 135090707111003

M LU TH I S 13509070711100!

"ANELLA #URNIA D135090707111005

$ES I"A I O#TA%IANA 13509070711100&


2/20

TURAMAkuisisi

Processing

Interpretasi


3/20

P'm()'*a+ ,')'r-a+a )a*am .'+'ra.a+

m'/()' /uram Ma'**

#(+)u4/6/a, a+8 /)a4 -(m(8'+ m'm.u+a .a+a+8,/r4' ,a,ara+ /a4 /'r-+88a 2 )m'+, ar/+a .r(.'r/'*'4/r(ma8+'/4 )ar 4';a+a4a+ a+8 /)a4 -(m(8'+

)a.a/ ).'r(*'- -a+a /'8a4 *uru, /'r-a)a.


4/20

S(*u, .'r-/u+8a+ .a)a .'r,amaa+ Ma'**m'+88u+a4a+ .'+)'4a/a+ /'4+4 .'r-/u+8a+ a+8)'*a,4a+ m'*a*u ,@/> I+ m'ru.a4a+ ,ua/u .r(8ram

.'r-/u+8a+ m')a+ 8'*(m;a+8 EM u+/u4 aru, 8ar,a+8 /a4 /'r-+88a .a)a 8'(*(8 ,/ru4/ur )ua )m'+,)'+8a+ ,/r4' .ara**'* /'r-a)a. ara- aru, 8ar, a+8/'*a- )/'/a.4a+ )ar G'(,?'+?' I+?(r.(ra/') (@"am;r)8' Ma,,a?-u,'//,>

#ur6a /uram ).'r(*'- )'+8a+ m'+,.4a+.'+8u4ura+ .'r/ama )a+ 4'mu)a+ m'+8-/u+8 SR)a+ ;')a @a,'


5/20

FSR Vertikal horizontal

Hz1 dan Hz2 adalah besar dari medan magnet vertical pada receiver 1dan 2

φZ1 dan φZ2 adalah fase vertical pada receiver posisi 1 dan posisi 2 secaraberturut-turut


6/20

1FSR !nverse atau kebalikan dari FSR "uantitas ini digunakan untuk receiver #ang $arakn#a $auh darisumber

%#ke vertical dengan overburden


7/20

Kurvaperbandinganunnormal dan

normal

%'r/4a*

H(r(+/a*


8/20

Dyke di bawah permukaan tanah vertikal


9/20

Field Strength Ratio )8am;ar4a+ )a*am ;'+/u44ur6a> R',.(+ m')a+ ma8+'/4 + m'm*4 ;'ra8am+@(rma, )a+/ara+a a)a*a- 4')a*ama+ *a.,a+4(+)u4/(r )a+ ara- strike> $4a /'r)a.a/ a+(ma*

4(+)u4/6/a, ma4a dip )ar *a.,a+ m+'ra* /'r,';u/)a.a/ ).'r-/u+84a+ ,'.'r/ .'+'*a,a+ 8am;ar );aa-+


10/20

Dip dari lapisan mineral dapat diketahuidengan landai/curamnya puncak kurva dari

Field Strength Ratio


11/20

"a,' ,/u)

Galena Hill, ayo ining District,

!ukon "erritory


12/20


13/20

&rosedur 'apanganP'ra*a/a+ a+8 )8u+a4a+ a)a*a- U+/ Turam /.'A>B>E>M 112 )'+8a+ 4(m.(,, 2 4(* -(r(+/a* .'+?ara+8 ).,a-4a+ )'+8a+ ara4 100 4a4 30! m'/'r a+8;'r/u8a, u+/u4 m'r'4am ),/(r, )ar .'ru;a-a+ m')a+

ma8+'/ a+8 );a+84/4a+ (*'- aru, ;(*a4C;a*4 .a)a4a;'* a+8 /'r/a+am .a)a )a'ra- ,ur6' /'r,';u/>P'm;a?aa+ a+8 )*a4u4a+ )'+8a+ .*(/ ara4 )ar .u,a/.'ma+?ar ,';',ar 100 4a4 30! m'/'r>


14/20


15/20

#ara4/'r,/4 )ar *a.a+8a+ + )4'/a-u )'+8a+

m'+'m.a/4a+ ,'.a,a+8 4(* .'+'rma SEC77

Sum;'r /'8a+8a+ /'r-u;u+8 )'+8a+ 4a;'* .a)a ,'/a.4(*> B',ar+a )a.a/ )4'/a-u )'+8a+ .'r;a+)+8a+ra,( )a+ ;')a @a,' -a+/ara+ *,/r4 .a)a .'rmu4aa+6'r/4a* ,'/a. 4(*>


16/20

S'?ara r'8(+a* ,/ru4/ur 8'(*(8 .a)a )a'ra- (;,'r6a, +/'r*'/a4 );aa- @(rma, Precambrian a+8 /'r;a8m'+a) /8a 4(m.(+'+ u/ama )ma+a:

U..'r S?-,/ : /'r)r )ar ;a/ua+ m4a ;a/ua+ 4a.ur)a+ 4uar,a>

"'+/ra* uar//', :4uar,/ )'+8a+ ?rC?r ;'rar+a;ru a;uCa;u )a+ .u/-

L('r S?-,/ :/'r)r )ar schist a+8 /';a*

(rma, Precambrian + )4'/a-u m'm*4 strike 4'ara- /murC;ara/ )a+ ). 20(C!0( 4' ,'*a/a+> I+@(rma,8'(*(8 ,a+8a/ .'+/+8 )4'/a-u m'+8+8a/ .a)a +@(rma,,/ru4/ur 8'(*(8 4'mu)a+ )a.a/ )4'/a-u *(4a, *a.,a+m+'ra* /'r4(+,'+/ra,> T'ru/ama )'+8a+ 4'/'r4a/a+

a)a+a .a/a-a+ .a)a )a'ra- ,ur6' ,/u) 4a,u, +>


17/20

T'ra)+a m+'ra* /)a4 *'.a, 4a/a++a )'+8a+ a4/6/a,.'r8'ra4a+ *'m.'+8 )a+ 8u+u+8 a.> "'*a-C?'*a- a4;a/a4/6/a, *'m.'+8 ;um a+8 4'mu)a+ ), (*'- ma/'ra* *a6am'm;'+/u4 dyke )a+ sill> D'm4a+ .a)a ,/u) 4a,u, +

m+'ra*,a, ))u8a ;'ra)a .a)a 4(m.(+'+ Central Quartzites )ma+a /'r)a.a/ ura/ .a/a-a+ a+8 ?'+)'ru+8 ?uram 4' ara-,'*a/a+> #(+,'+/ra, m+'ra* )/'mu4a+ .a)a ,';'*um+aa)a*a- .r/ ,)'r/ ,@a*'r/ )a+ 8a*'+a> Ga*'+a 4aa a4a+

.'ra4 ,'-+88a .a)a *a.(ra+ + )-ara.4a+ a)a a+(ma*4(+)u4/6/a, )ar 8a*'+a .a)a Ga*'+a H** Yu4(+ T'rr/(r>

A+(ma* 4(+)u4/6/a, /'r*-a/ ) ;';'ra.a // 4 (;,'r6a,

a+8 ,'*ua, 3 m* ,'4/ar !2 4*(m'/'r )ar +/'+,/a,*'ma-C,')a+8 a/u .a)a *+' 12!00E )a+ 1200E


18/20


19/20


20/20

"'rma/ @r'4u'+, a+8 ;'4'ra .a)a ma,+8Cma,+8m'/()' EM

Documents

TURAM (Interpretasi)