Leg : 14 Top Int Depth(mm): 1000 Sand: 020% Sect: 4
Hole: 144B Top Core Depth(m): 0.00 Silt: 030%
Core: 1 Sample Depth (m) : 5.75 Clay: 050%
Age : LOWER OLIGOCENE
Name: NANNO FORAM CHALK OOZE
Components: (Dominant lithology, % converted from relative abundance)
======================================================================
QUARTZ (02%); MICA (02%); CARBONATE (47%);
CLAY MINERAL (11%); FORAMINIFERA (25%); NANNOFOSSIL (11%);
RADIOLARIA (02%);
Leg : 14 Top Int Depth(mm): 750 Sand: 035% Sect: 1
Hole: 144B Top Core Depth(m): 10.00 Silt: 030%
Core: 2 Sample Depth (m) : 10.88 Clay: 035%
Age : LOWER OLIGOCENE
Name: FORAM CHALK OOZE
Components: (Dominant lithology)
======================================================================
CLAY MINERAL (10%); FORAMINIFERA (50%); NANNOFOSSIL (35%);
RADIOLARIA (05%);
Leg : 14 Top Int Depth(mm): 800 Sand: 030% Sect: 3
Hole: 144B Top Core Depth(m): 10.00 Silt: 030%
Core: 2 Sample Depth (m) : 13.93 Clay: 030%
Age : LOWER OLIGOCENE
Name: FORAM CHALK OOZE
Components: (Dominant lithology, % converted from relative abundance)
======================================================================
QUARTZ (02%); CLAY MINERAL (10%); FORAMINIFERA (50%);
NANNOFOSSIL (30%);
Leg : 14 Top Int Depth(mm): 750 Sand: 020% Sect: 2
Hole: 144B Top Core Depth(m): 27.00 Silt: 025%
Core: 3 Sample Depth (m) : 29.25 Clay: 055%
Age : LOWER OLIGOCENE
Name: NANNO FORAM CHALK OOZE
Components: (Dominant lithology, % converted from relative abundance)
======================================================================
ZEOLITE (02%); CLAY MINERAL (11%); CARBONATE (42%);
FORAMINIFERA (22%); NANNOFOSSIL (20%); RADIOLARIA (03%);
Leg : 14 Top Int Depth(mm): 750 Sand: 025% Sect: 4
Hole: 144B Top Core Depth(m): 27.00 Silt: 025%
Core: 3 Sample Depth (m) : 32.25 Clay: 050%
Age : LOWER OLIGOCENE
Name: FORAM CHALK OOZE
Components: (Dominant lithology)
======================================================================
CLAY MINERAL (11%); CARBONATE (43%); FORAMINIFERA (25%);
NANNOFOSSIL (17%); RADIOLARIA (03%);
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