Leg : 13 Top/Bottom Interval(mm): 0/ 0 Describer: Hsu, K.
Hole: 134D Top of Core Depth(m) : 211.00 Rock Type: METAMORPHIC
Core: 3 Sample Midpoint(m) : 215.60 Sect/Pc #: CC/
ROCK = METAGRAYWACKE
GRAY,SOURCE IS IR*
Groundmass - QUARTZ
Morphology: ANGULAR-SUBANGULAR
UNDULATORY EXTINCTION IS COMMON,HOWEVER,ONLY A FEW
QUARTZ GRAINS SHOW SIGNS OF BEING FLATTENED DURING
THE SYNTECTONIC XTLLIZATION,REXTLLIZED CHERT
GRAINS ARE PRESENT;
FELDSPAR
POTASH FELDSPAR,TWINNED AND SOMEWHAT SERICITIZED;
MAGNETITE
COMMON;
MUSCOVITE
A FEW FLAKES ARE PRESENT,MAX,GRAIN SIZE FOR THESE
MINERALS IS APPROX 1MM,SORTING IS POOR,THE
SCHISTOSITY IS MARKED BY CRUSHED LAMINAE OF VERY
FINE GRAINED AGGREGATES OF QUARTZ SERICITE,MAGN
AND CALCITE,THE LAMINAE RANGE FROM SEVERAL MICRONS
TO A FRACTION OF A MILLIMETER THICK,THIS
SCHISTOSITY IS INCLINED TO A PLANAR STRUCTURE
DEFINED BY THE LONG AXIS OF QUARTZ(IN THIN
SECTION),AND MAY REPRESENT THE SECONDARY
SCHISTOSITY INCLINED TO THE ORIGINAL BEDDING
PLANE*
Alteration - SERICITE
Replacing: QUARTZ,FELDSPAR
CALCITE
|