ML17037A662: Difference between revisions
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| number = ML17037A662 | | number = ML17037A662 | ||
| issue date = 02/06/2017 | | issue date = 02/06/2017 | ||
| title = | | title = Structural Comparison of Fault Zone in Boring Series T-3, Plate 5-11 | ||
| author name = | | author name = | ||
| author affiliation = Dames & Moore, Niagara Mohawk Power Corp | | author affiliation = Dames & Moore, Niagara Mohawk Power Corp | ||
Line 15: | Line 15: | ||
=Text= | =Text= | ||
{{#Wiki_filter:T-3- | {{#Wiki_filter:T-3-5 T-3-6 T-3-7 T-3-8 T-3-9 T-3-6 EXPLANATION OF SY NELS: | ||
( EL 249.7 ) /9 (EL 234 5) 34 (EL. 223.4) 45 (EL 2114) 57 (EL 1717) 96'EL 1051) /6'2 | |||
<<C CL 0 ~ JT 57 DIP OF LITHOLOGIC GRAPH BEDDING PLANE T 3 IO BDRING FAULT FRACTURE NUMBER STRUCTURAL GRAPH (NORMAL) | |||
FOLD 20 4 T 35 ee /63 Z 0 | |||
OMB JT 34 I- T 60 DIP SLIP SLICKENSIDES (ON A 60 PLANE) | |||
A ~ 60 STRIKE SLIP SLICKENSIDES (ON A 50 PLANE) | |||
Z 0 5 60 OBLIQUE SLIP SLICKENSIDES (ON A 60 PLANE) 0 2/ '5 55 98 1$ M G GROOVES T 3o T M-CALCITE MINERALIZATION CD WHI TE 37 4e 99 I- /65 IAI WHITE, DEFORMED I<< Z 0 JT-IKA JT- 'le 00 Z 0I- PINK T Zo 0 0 PINK, DEFORMED MI 0 SULFIDE MINERALIZATION 6/ os /00 (GALENA, SPHALERITE, PYRITE, CHALCOPYRITE, PYRRHOTITE) 0 DEFORMED KI 0 | |||
/0/ Ol) /67 Ul 62 ZONE OF LIMONITE ALTERATION O | |||
0 TO Z | |||
J T 3o 0 0 Gl JT-47 0 Ke T 3o | |||
*33, 5/ 63 T 5 /02 <<f /ee C) 5 6 JT-IZB MINERAL SAMPLE FOR 05 LABORATORY STUDY C) 5 0 4-61 J7-4'5 52 OM /03 DE /69 045JT KA i 07 | |||
<<t CL 0 lg 27 35 53 'T 73 | |||
/04 /70 ~ JT-IZC STRATIGRAPHIC EXPLANATION: | |||
4 D N BRFCK. A C K E<<55) 5 25 T T 50 3 A SANDSTONE | |||
, o) 4 ~ JT 28 /05 I- (3o, o) p Z OW SILTSTONE AND GRAYWACKE NORMAL 3 036 ~I JT-SOA, ZK SHALE T 5 29 I- 55 /06 /72 T 5o IK T 35 5o 0 3o ~ JT 35 I | |||
O Io 0 BROKEN ROCK AHD CORE LOSS T5o 0 3O 1 56 <<E | |||
/73 T 5<< | |||
BRECCIA AND GOUGE (L | |||
U. 0LL 57 /oe /74 | |||
~ JT 115 Tc5 BW a | |||
CL 32 47 58 T 55 70 /09 /75 IAI p 0 T 35 Je 59 7/ //0 /76 'T So OS, T eo 0 MJ OSG 60 5 Zo 72 /77 T75 04 0 T Fo 0 I- Z | |||
<<C 50 73 //2 /re IL 0U T Ro | |||
//3 /79 g SE 5/ 74 CD W- 0 Mo O. | |||
REVERSE DR ' | |||
F LD | |||
//4 /80 37 CO 0 | |||
T IO | |||
+ 75 Jl DM | |||
~ <<5 445 0 Z 535 CI R <<e ~ JT'- 35 0 Ol (0 3/ol UJ I-0 I FA 7 Z <<C U | |||
<<I 0 53 76 //5 /e/ 0 Z | |||
'7 0 | |||
0 | |||
<<n Ii) | |||
Gl Z J | |||
39 I 0 6 5 | |||
77 //6 0 Yl 66 re //7 /e3 G | |||
T 0-s T 15 67 //e /84 OT M 0 T55'D STRUCTURAL COMPARISON 42 68 //9 JT- 0 /85 C) 0 EB JT-IZC OF FAULT ZONE IN T- 5 69 /20 /86 BORING SERIES PLATE 5 II | |||
%AMES S}} |
Latest revision as of 21:30, 4 February 2020
ML17037A662 | |
Person / Time | |
---|---|
Site: | Nine Mile Point ![]() |
Issue date: | 02/06/2017 |
From: | Dames & Moore, Niagara Mohawk Power Corp |
To: | Office of Nuclear Reactor Regulation |
References | |
Download: ML17037A662 (1) | |
Text
T-3-5 T-3-6 T-3-7 T-3-8 T-3-9 T-3-6 EXPLANATION OF SY NELS:
( EL 249.7 ) /9 (EL 234 5) 34 (EL. 223.4) 45 (EL 2114) 57 (EL 1717) 96'EL 1051) /6'2
<<C CL 0 ~ JT 57 DIP OF LITHOLOGIC GRAPH BEDDING PLANE T 3 IO BDRING FAULT FRACTURE NUMBER STRUCTURAL GRAPH (NORMAL)
FOLD 20 4 T 35 ee /63 Z 0
OMB JT 34 I- T 60 DIP SLIP SLICKENSIDES (ON A 60 PLANE)
A ~ 60 STRIKE SLIP SLICKENSIDES (ON A 50 PLANE)
Z 0 5 60 OBLIQUE SLIP SLICKENSIDES (ON A 60 PLANE) 0 2/ '5 55 98 1$ M G GROOVES T 3o T M-CALCITE MINERALIZATION CD WHI TE 37 4e 99 I- /65 IAI WHITE, DEFORMED I<< Z 0 JT-IKA JT- 'le 00 Z 0I- PINK T Zo 0 0 PINK, DEFORMED MI 0 SULFIDE MINERALIZATION 6/ os /00 (GALENA, SPHALERITE, PYRITE, CHALCOPYRITE, PYRRHOTITE) 0 DEFORMED KI 0
/0/ Ol) /67 Ul 62 ZONE OF LIMONITE ALTERATION O
0 TO Z
J T 3o 0 0 Gl JT-47 0 Ke T 3o
- 33, 5/ 63 T 5 /02 <<f /ee C) 5 6 JT-IZB MINERAL SAMPLE FOR 05 LABORATORY STUDY C) 5 0 4-61 J7-4'5 52 OM /03 DE /69 045JT KA i 07
<<t CL 0 lg 27 35 53 'T 73
/04 /70 ~ JT-IZC STRATIGRAPHIC EXPLANATION:
4 D N BRFCK. A C K E<<55) 5 25 T T 50 3 A SANDSTONE
, o) 4 ~ JT 28 /05 I- (3o, o) p Z OW SILTSTONE AND GRAYWACKE NORMAL 3 036 ~I JT-SOA, ZK SHALE T 5 29 I- 55 /06 /72 T 5o IK T 35 5o 0 3o ~ JT 35 I
O Io 0 BROKEN ROCK AHD CORE LOSS T5o 0 3O 1 56 <<E
/73 T 5<<
BRECCIA AND GOUGE (L
U. 0LL 57 /oe /74
~ JT 115 Tc5 BW a
CL 32 47 58 T 55 70 /09 /75 IAI p 0 T 35 Je 59 7/ //0 /76 'T So OS, T eo 0 MJ OSG 60 5 Zo 72 /77 T75 04 0 T Fo 0 I- Z
<<C 50 73 //2 /re IL 0U T Ro
//3 /79 g SE 5/ 74 CD W- 0 Mo O.
REVERSE DR '
F LD
//4 /80 37 CO 0
T IO
+ 75 Jl DM
~ <<5 445 0 Z 535 CI R <<e ~ JT'- 35 0 Ol (0 3/ol UJ I-0 I FA 7 Z <<C U
<<I 0 53 76 //5 /e/ 0 Z
'7 0
0
<<n Ii)
Gl Z J
39 I 0 6 5
77 //6 0 Yl 66 re //7 /e3 G
T 0-s T 15 67 //e /84 OT M 0 T55'D STRUCTURAL COMPARISON 42 68 //9 JT- 0 /85 C) 0 EB JT-IZC OF FAULT ZONE IN T- 5 69 /20 /86 BORING SERIES PLATE 5 II
%AMES S