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10 Summary Comments on the K Fault LAST OBSERVED MOVEMENT IS AFTER DEPOSITION OF MOST OF LAYER 3 AND BEFORE DEPOSITION OF LAYER 5 Pollen Pollen xxxxxxxxx xxxxxxxxxx xxxxxxxxxx xx x x x DKP 58 ka MIS 5a- c MIS 5c K- Tz 95 ka MIS 5e Mihama 127 ka F MIS 6 ( ka) Pollen/W Old MIS 7? ka 4
11 D- 1 sha6er zone connects with G fault: - Mapping during construcvon showed the locavon and convnuity of the D- 1 shazer zone - CharacterisVcs of the D- 1 shazer zone in the gap between the end of this map and the new excavavon further north can now be studied in outcrop and in drill cores Urasoko fault - New excavavon (D- 1 trench) exposes the G fault 2) STRUCTURAL RELATIONSHIPS: FAULT ALONG- STRIKE EXTENSION
12 C MIS 5e ( ) MIS m MIS MIS
13 C MIS 5e ( ) -130 m MIS MIS
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21 Source: JAPC--NSC
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27 step width tensile compressional
28 step width tensile compressional
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51 The Active Fault or Seam under Shika NPP modified from Hokuriku-Denryoku/NISA 2012
52 / /4 2/3 2 1 folded by faulting gradually filled by sediments folded / undulation by depostion or erosion fold or distributed shear filled by sediments faulted / haning rock face buried by sediments originally flat / rough-uneven fault-juxtaposed/depositional fault plane cut level surface differentially eroded surface of wave-cut bench fault gouge seam: a fissure filled with volcano-clastics. no shear Observation and interpretation FOR and AGAINST active faulting on S-1 modified from Hokuriku-Denryoku/NISA 2012
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