v h v m v t h tt a t h v t v h t vv v vvª v j h h t h v ª ... · ª paleozoic marine clastics...
TRANSCRIPT
T
H
DV D
DDDD
D D
!
D D
D
DD
##
#
###
#
##
#
#
D DD
#
#
HH
H
H
HHHH !
DD
DD
DD
DD
D
D
DDD
DDD
DDD
DDDD
DDD
D
D DDDDD D
D
DD
DD
D
DD
D
DD
DDD D
D
ª
ª
D
VV
V
VV
VV
V
V
VV
V
J
T
TTT
T
TTT
T
H
HH
H
T
T
!
ª ª DªV
VV
V
V
V
VV
V
D
D
D
H H
H
H
D
D
D
T
TD
DDD
D
#0
#0
#0
#0
#0
k
G
k
kk
k
GG
G
G
GG
k
k
k
kk
kk
k
R
RR R
R
RRRR
R
R
R
RRRR G
G
CC
_
A
A'
SouthFloridaBasin
BahamasBasin
BlakePlateauBasin
ApalachicolaBasin
Bahamas Fracture Zone
Sunniland Fracture Zone Cuba Fracture Zone
3-km
2-km
5-km
3.5-km
8-km
6-km
5.5-km
4.5-km
4-km
1.5-k m
10-km
1-km
12-km
4-km
6-km
4-km
5-km1.5
-km
3-km
2-km
5-km
3.5-km
8-km
6-km
5.5-km4.5-km
4-km
1.5-km
10-km
1-km
12-km
1.5
-km
6-km
4-km
5-km
4-km
Pre-Cretaceous Surface andTypes of Basement Terrane
Figure 2.5.1-212
LEGEND
File path: S:\11100\11151.001\figures\2_5_1_figures\LNP_FSAR_FIG02_05_01_212.mxd; Date: [06/09/2008]; User: [sbozkurt]
Progress Energy Florida
Rev 0
Levy Nuclear PlantUnits 1 and 2Part 2, Final Safety Analysis Report
_ LNP Site
320-km (200-mi.) Radius from SiteA-A' Profile (see Figure 2.5.1-213)
Drill Holes Not Penetrating BasementR Deep See Drillingk Lower Cretaceous carbonate rocksG Upper Jurassic anhydrite – carbonate rocks overlaying basal – clastics (Wood River formation)C Wood River formation underlain by Jurassic salt
Drill Holes Penetrating Basement# Jurassic volcanics and volcaniclastics#0 Jurassic volcanics overlain by Wood River formationT Paleozoic (?) rhyolites and felsic volcanicsJ Paleozoic (?) rhyolites and overlain by marine clastics! Paleozoic diorites and mafic plutonicH Paleozoic granitesD Paleozoic marine clasticsª Paleozoic marine clastics overlain by Eagle Mills formation or intruded with diabase dikes and sillsV Triassic red beds-clastics (Eagle Mill formation) and diabase dikes or sills
Source: Klitgord et al. (1984); Base Map: ETOPO2v2 (2006), and SRTM (2005)
0 40 80
Kilometers
/0 30 60
Miles
LNP COL 2.5-1