ML20126D467: Difference between revisions

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{{#Wiki_filter:- - _ _ _
{{#Wiki_filter:- - _ _ _
                                                                                                                                        & & sal *O(7%
& & sal *O(7%
o g >/2du March 8, 1971 8005020                    2h ACRS Members I
o g
DRL 1122 FEBRUARY        TING 24, 1971        ON SEIS'DLOGY-GE01DGY                                             FOR SAN
>/2du 8005020 2h March 8, 1971 ACRS Members DRL 1122 TING ON SEIS'DLOGY-GE01DGY FOR SAN ONOFRE 2 &
                                                                                                                            , BETHESDA,           MARYLAND,   ONOFRE 2 &
FEBRUARY 24, 1971
A group of eminent U. S. geologists and seismologists teet tos discuss thi subject   as it2relates tion for Units                  to the San Onofre site in general and to the applic
, BETHESDA, MARYLAND, A group of eminent U. S. geologists and seismologists teet to discuss thi subject as it relates to the San Onofre site in general and to the applic s
                                                      & 3 in particular.                                                                                           -
tion for Units 2 & 3 in particular.
Newport-Inglewood Fault and which may                                                                   .      The be of co applicant was informed by L. Murphy of NOA that with current knowled he would have to assume a " great earthquake" within fivee miles of th                                                   ,
Newport-Inglewood Fault and which may be of co applicant was informed by L. Murphy of NOA that with current knowled The he would have to assume a " great earthquake" within five miles of th site and that this would result in site accelerations " considerably e
site and greater    that than    this 0.50  g." would result in site accelerations " considerably to look at the strongest plant they felt they could designThe app                             , and to back-calculate to an earthquake magnitude at the deformed                                                     underwater ne.
greater than 0.50 g."
so          s Oricinal signed by J. E. Hard J. E.'Hard Saaior' Staff Assistant ec:    B. M. Page, Consultant J. T. Wilson, Consultant                                           .
to look at the strongest plant they felt they could designThe app calculate to an earthquake magnitude at the deformed underwater so
1
, and to back-s ne.
                                                                                                                                                                                  .l omcc>   ..
Oricinal signed by J. E. Hard J. E.'Hard Saaior' Staff Assistant B. M. Page, Consultant ec:
smm >                     ,,
J. T. Wilson, Consultant 1
                                                                                                            ~ . . . . . . .    . . . . .
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Form Arc-ase <n,,, %
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4..*,
#                                                          ,}}
g
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Latest revision as of 19:49, 12 December 2024

Forwards Minutes of Div of Reactor Licensing 710224 Meeting in Bethesda,Md Re seismology-geology
ML20126D467
Person / Time
Site: San Onofre  
Issue date: 03/08/1971
From: Hard J
Advisory Committee on Reactor Safeguards
To:
Advisory Committee on Reactor Safeguards
Shared Package
ML20126D470 List:
References
ACRS-SM-0172, ACRS-SM-172, NUDOCS 8005020125
Download: ML20126D467 (1)


Text

- - _ _ _

& & sal *O(7%

o g

>/2du 8005020 2h March 8, 1971 ACRS Members DRL 1122 TING ON SEIS'DLOGY-GE01DGY FOR SAN ONOFRE 2 &

FEBRUARY 24, 1971

, BETHESDA, MARYLAND, A group of eminent U. S. geologists and seismologists teet to discuss thi subject as it relates to the San Onofre site in general and to the applic s

tion for Units 2 & 3 in particular.

Newport-Inglewood Fault and which may be of co applicant was informed by L. Murphy of NOA that with current knowled The he would have to assume a " great earthquake" within five miles of th site and that this would result in site accelerations " considerably e

greater than 0.50 g."

to look at the strongest plant they felt they could designThe app calculate to an earthquake magnitude at the deformed underwater so

, and to back-s ne.

Oricinal signed by J. E. Hard J. E.'Hard Saaior' Staff Assistant B. M. Page, Consultant ec:

J. T. Wilson, Consultant 1

.l omcc>

smm >

~.......

Form Arc-ase <n,,, %

,,,,,,,,,,,,,,gg g;,;;_ g ;,;,,.

{

4..*,

g

,