Leg : 13 Top/Bottom Interval(mm): 0/ 0 Describer: Hsu, K.
Hole: 133 Top of Core Depth(m) : 63.00 Rock Type: METAMORPHIC
Core: 3 Sample Midpoint(m) : 63.00 Sect/Pc #: 1/
ROCK = METAGRAYWACKE
GRAY,SOURCE IS IR*
Groundmass - QUARTZ
SHOWS SOME EVIDENCE OF BEING FLATTENED,MOST GRAINS
NOT PARTICULARLY ELONGATED,A SET OF SCHISTOSITY IS
DISTINGUISHED BY THE PREFERRED ORIENTATION OF FLAT
QUARTZ GRAINS AND BY THE BANDS OF SERICITIC MATRIX
AROUND SUCH GRAINS,A MICROSHEAR ZONE INCLINED TO
THIS SCHISTOSITY IS MARKED BY AGGREGATES OF FINELY
PULVERIZED QUARTZ;
FELDSPAR
MAGNETITE
MUSCOVITE
Morphology: FLAKES
COMMON;
MAX.GRAIN SIZE IS APPROX .8MM,SORTING IS VERY
POOR,REXTLLIZED CHERT GRAINS HAVE BEEN STREAKED
OUT AS LENTICLES*
Alteration - SERICITE
Location: MATRIX
CHLORITE
Location: MATRIX
Leg : 13 Top/Bottom Interval(mm): 0/ 0 Describer: Hsu, K.
Hole: 133 Top of Core Depth(m) : 63.00 Rock Type: METAMORPHIC
Core: 3 Sample Midpoint(m) : 64.60 Sect/Pc #: CC/PCE 3
ROCK = METAGRAYWACKE
REDDISH BROWN,SOURCE IS IR;
Groundmass - QUARTZ
Size(mm): .1-.15 Morphology: LENTICULARLY-SHAPED
FELDSPAR
MUSCOVITE
Size(mm): TO .5 Morphology: FLAKES
FERRIC MINS (PHENOS)
BLACK IRON MINERALS HAVE BEEN LARGELY ALTERED TO
HEMATITE AND GOETHITE,THUS GIVING THE ROCK A
REDDISH BROWN COLOR,TWO SETS OF SCHISTOSITY WERE
RECOGNIZED*
Alteration - SERICITE
Location: MATRIX
FINER THAN QUARTZ;
CHLORITE
Location: MATRIX
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