leg	site	hole	core	section	top interval depth (cm)	bottom interval depth (cm)	top of core depth(m)	top of layer depth (m)	bottom of layer depth (m)	 describer	lithology	color	structures	deformations due to drilling	unusual occurrences	minerals	paleontology	other observations	hardness or induration	z-coding
3	18		1	5	0.0	150.0	0.00	6.00	7.50		 FORAM NANNO CHALK OOZE	 10YR8/2		 DISTURBED						 00000000
3	18		2	2	0.0	150.0	121.00	122.50	124.00		 NANNO CHALK OOZE	 10YR5.5/6-YELLOW BROWN,10YR7/4	 SLIGHT MOTTLING (10YR7/4)	 DISTURBED						 00000000
3	18		3	2	0.0	150.0	141.20	142.70	144.20		 NANNO CHALK OOZE	 10YR6/4-LIGHT YELLOW BROWN, 10 YR8/3,10YR6/1,-WHITE,-GRAY	 MODERATE WHITE AND GRAY MOTTLING 12-30 CM							 00000000
3	18		4	4	0.0	150.0	150.30	154.80	156.30		 NANNO CHALK OOZE	 10YR7/3-VERY PALE BROWN,10YR8/3	 SLIGHT MOTTLING (10YR8/3)					 HOMOGENEOUS		 00000000
3	18		5	2	0.0	150.0	159.80	161.30	162.80		 NANNO CHALK OOZE	 10YR7/3-VERY PALE BROWN,10YR8/2 ,10YR6/1	 SLIGHT MOTTLING (10YR8/2 AND 10YR6/1) 10-65 AND 124-126 CM	 DISTURBED						 00000000
3	18		6	1	0.0	150.0	168.90	168.90	170.40		 NANNO CHALK OOZE	 10YR7/3-VERY PALE BROWN,10YR8/2	 BURROWING AND MOTTLING SIGHT (10YR8/2)							 00000000
3	18		6	6	0.0	150.0	168.90	176.40	177.90		 NANNO CHALK OOZE	 10YR7/4-VERY PALE BROWN						 THE BOTTOM SAMPLE IS ALMOST A FRIABLE " SHALE" PROBABLY LITHIFICATION IS RELAED TO THE EMPLA CEMENT OF BASALT	 FIRM, THIS SECTION CONSIDERABLY FIRMER AT THE BOTTOM THAN AT THE TOP	 00000000
3	18		7	1	0.0	50.0	178.10	178.10	178.60		 BASALT	 5Y6/3-PALE OLIVE	 THE FRACTURES DIP STEE PLY (SOMEWHAT IRREGULAR EXTENSIONAL SHEAR FRACTURES)					 BLACK GLASSY CHILLED BOARDERS ARE PRESENT AROUND THE ZENOLITHS, WEATHERED PALE OLIVE APHANITIC BASALT WITH FRACTURES FILLED BY METAMORPHOSED CALCAREOUS S EDIMENTS (NOW COMPLETELY CRYSTALLIZED TO MARBLE)		 00000000