Citation:

PANGAEA.777664

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Related to:

IODP/CDEX (2012): SIO7 Data Center, J-CORES Database. Ocean Drilling Program, Center for Deep Earth Exploration, Japan Agency for Marine-Earth Science and Technology, Yokohama Kanagawa 236-0001, JAPAN, https://www.jamstec.go.jp/sio7/j-cores.data/315/C0001H/

Kinoshita, Masataka; Tobin, Harold; Ashi, Juichiro; Kimura, Gaku; Lallemant, Siegfried J; Screaton, Elizabeth J; Curewitz, Daniel; Masago, Hideki; Moe, Kyaw Thu; Expedition 314/315/316 Scientists (2009): Proceedings of the Integrated Ocean Drilling Program. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.), 314/315/316, https://doi.org/10.2204/iodp.proc.314315316.133.2009

Other version:

IODP Hole 316-C0006E, snapshot taken on 2011-04-14, J-CORES, SIO7 Data Center

Project(s):

Integrated Ocean Drilling Program / International Ocean Discovery Program (IODP)

Coverage:

Latitude: 33.027407 * Longitude: 136.793803

Date/Time Start: 2007-12-29T00:00:00 * Date/Time End: 2007-12-29T00:00:00

Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 404.680 m

Event(s):

316-C0006E * Latitude: 33.027407 * Longitude: 136.793803 * Date/Time: 2007-12-29T00:00:00 * Elevation: -3875.8 m * Recovery: 330.23 m * Campaign: (NanTroSEIZE Stage 1: Shallow Megaslay and Frontal Thrusts) * Basis: Chikyu * Method/Device: Drilling/drill rig (DRILL) * Comment: 49 cores; 409.4 m cored; 80.68 % recovery; 409.4 m drilled; 409.44 m penetrated

Comment:

Geocode = [m CSF-A] Top Core depth (below sea floor)

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	Sample code/label	Sample label		Expedition 314/315/316 Scientists	DSDP/ODP/IODP sample designation	Sample top
2	DEPTH, sediment/rock	Depth sed	m			Geocode
3	Depth, top/min	Depth top	m	Expedition 314/315/316 Scientists		[m CSF-B] Top Core depth (below sea floor)
4	Sample code/label 2	Sample label 2		Expedition 314/315/316 Scientists	DSDP/ODP/IODP sample designation	Sample bottom
5	Depth, bottom/max	Depth bot	m	Expedition 314/315/316 Scientists		[m CSF-A] Bottom Core depth (below sea floor)
6	Depth, bottom/max	Depth bot	m	Expedition 314/315/316 Scientists		[m CSF-B] Bottom Core depth (below sea floor)
7	Main Lithology	Main lith		Expedition 314/315/316 Scientists	Visual description	Sedimentological comment on Core
8	Main Lithology	Main lith		Expedition 314/315/316 Scientists	Visual description	Continued
9	Main Lithology	Main lith		Expedition 314/315/316 Scientists	Visual description	Continued
10	Main Lithology	Main lith		Expedition 314/315/316 Scientists	Visual description	Continued
11	Main Lithology	Main lith		Expedition 314/315/316 Scientists	Visual description	Continued
12	Lithology/composition/facies	Lithology		Expedition 314/315/316 Scientists	Visual description	Sedimentological comment on Section
13	Lithology/composition/facies	Lithology		Expedition 314/315/316 Scientists	Visual description	Continued
14	Lithology/composition/facies	Lithology		Expedition 314/315/316 Scientists	Visual description	Continued
15	Time Stamp	Time Stamp		Expedition 314/315/316 Scientists

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

1082 data points

Data

Download dataset as tab-delimited text — use the following character encoding:

1 Sample label (Sample top, DSDP/ODP/IODP sam...)	2 Depth sed [m]	3 Depth top [m] ([m CSF-B] Top Core depth (bel...)	4 Sample label 2 (Sample bottom, DSDP/ODP/IODP ...)	5 Depth bot [m] ([m CSF-A] Bottom Core depth (...)	6 Depth bot [m] ([m CSF-B] Bottom Core depth (...)	7 Main lith (Sedimentological comment on C...)	8 Main lith (Continued, Visual description)	9 Main lith (Continued, Visual description)	10 Main lith (Continued, Visual description)	11 Main lith (Continued, Visual description)	12 Lithology (Sedimentological comment on S...)	13 Lithology (Continued, Visual description)	14 Lithology (Continued, Visual description)	15 Time Stamp
316-C0006E-1H-1,0.0	0.000	0.000	316-C0006E-1H-CC,10.5	5.235	5.195	[Section 2; fergussenc, 2007-12-30T16:20:14] IW [Section 5; fergussenc, 2007-12-30T16:34:53] IW [Section 6; fergussenc, 2007-12-31T16:22:52] Exact position of sand bed is uncertain due to drilling disturbance.								2008-01-17T05:13:00
316-C0006E-1H-2,0.0	1.205	1.196	316-C0006E-1H-2,22.5	1.430	1.419						IW			2007-12-30T16:20:14
316-C0006E-1H-5,0.0	4.240	4.208	316-C0006E-1H-5,23.0	4.470	4.436						IW			2007-12-30T16:34:53
316-C0006E-1H-6,0.0	4.470	4.436	316-C0006E-1H-6,66.0	5.130	5.091						Exact position of sand bed is uncertain due to drilling disturbance.			2007-12-31T16:22:52
316-C0006E-2H-1,0.0	5.190	5.190	316-C0006E-2H-CC,20.0	15.290	14.690	[Section 3; fergussenc,2007-12-30T16:59:50] IW [Section 5; fergussenc,2007-12-31T01:28:15] Greenish-gray sity clay, light-gray nannofossil rich layer with significant glass at 95 to 103 cm. [Section 7; fergussenc,2007-12-30T17:04:12] IW								2008-01-17T05:13:06
316-C0006E-2H-3,0.0	7.790	7.635	316-C0006E-2H-3,23.0	8.020	7.852						IW			2007-12-30T16:59:50
316-C0006E-2H-5,0.0	9.445	9.192	316-C0006E-2H-5,143.0	10.875	10.537						Greenish-gray sity clay, light-gray nannofossil rich layer with significant glass at 95 to 103 cm.			2007-12-31T01:28:15
316-C0006E-2H-7,0.0	12.085	11.675	316-C0006E-2H-7,24.0	12.325	11.901						IW			2007-12-30T17:04:12
316-C0006E-3H-1,0.0	14.690	14.690	316-C0006E-3H-CC,53.0	25.335	24.185	[Section 1; fergussenc, 2007-12-31T16:24:45] Dark greenish-gray silty clay, with interbedded dark greenish-gray silty to fine-grained sandy layers, graded. Sand layers are locally disrupted by drilling.	[Section 2; fergussenc, 2007-12-29T18:48:09] Silty clay with interbedded silty sands and sandy silt to silt layers and laminae.							2008-01-17T05:13:12
316-C0006E-3H-1,0.0	14.690	14.690	316-C0006E-3H-1,140.5	16.095	15.943						Dark greenish-gray silty clay, with interbedded dark greenish-gray silty to fine-grained sandy layers, graded. Sand layers are locally disrupted by drilling.			2007-12-31T16:24:45
316-C0006E-3H-2,0.0	16.095	15.943	316-C0006E-3H-2,119.0	17.285	17.005						Silty clay with interbedded silty sands and sandy silt to silt layers and laminae.			2007-12-29T18:48:09
316-C0006E-4H-1,0.0	24.190	24.190	316-C0006E-4H-CC,58.0	33.395	33.215	[Section 2; fergussenc, 2007-12-30T17:50:17] Thick ash unit. Impure ash, also about 20% nannofossils, may be reworked?	[Section 4; fergussenc, 2007-12-31T16:26:26] Steep reverse faults cut sandstone bed from 80 cm to 115 cm. [Section 5; fergussenc, 2007-12-30T18:16:24] IW							2008-01-17T05:13:19
316-C0006E-4H-2,0.0	25.625	25.597	316-C0006E-4H-2,141.0	27.035	26.979						Thick ash unit. Impure ash, also about 20% nannofossils, may be reworked?			2007-12-30T17:50:17
316-C0006E-4H-4,0.0	28.440	28.357	316-C0006E-4H-4,148.0	29.920	29.808						Steep reverse faults cut sandstone bed from 80 cm to 115 cm.			2007-12-31T16:26:26
316-C0006E-4H-5,0.0	29.920	29.808	316-C0006E-4H-5,23.5	30.155	30.038						IW			2007-12-30T18:16:24
316-C0006E-5H-1,0.0	33.220	33.220	316-C0006E-5H-CC,16.5	38.630	38.520	[Section 3; fergussenc, 2007-12-30T18:25:34] IW								2008-01-17T05:13:26
316-C0006E-5H-3,0.0	35.840	35.787	316-C0006E-5H-3,21.5	36.055	35.997						IW			2007-12-30T18:25:34
316-C0006E-6H-1,0.0	38.520	38.520	316-C0006E-6H-CC,11.0	38.690	38.690	[Section 1; fergussenc, 2007-12-31T16:28:36] Mixed silty clay and fine sand due to drilling disturbance.								2008-01-17T05:13:32
316-C0006E-6H-1,0.0	38.520	38.520	316-C0006E-6H-1,6.0	38.580	38.580						Mixed silty clay and fine sand due to drilling disturbance.			2007-12-31T16:28:36
316-C0006E-7H-1,0.0	38.690	38.690	316-C0006E-7H-CC,45.5	49.085	48.185	[Section 1; fergussenc, 2007-12-30T21:29:20] Thick dark gray, very fine to fine sand, generally structureless interbedded with thin intervals of hemipelagic silty clay and clayey silt with sand.	[Section 6; fergussenc, 2007-12-31T16:30:17] Flow in structure, where liquified sand injects into overlying silty clay, most probably drilling induced.							2008-01-17T05:13:38
316-C0006E-7H-1,0.0	38.690	38.690	316-C0006E-7H-1,140.5	40.095	39.973						Thick dark gray, very fine to fine sand, generally structureless interbedded with thin intervals of hemipelagic silty clay and clayey silt with sand. Shiny fragments throughout (muscovite?).			2007-12-30T21:29:20
316-C0006E-7H-6,0.0	44.570	44.061	316-C0006E-7H-6,141.0	45.980	45.349						Flow in structure, where liquified sand injects into overlying silty clay, most probably drilling induced.			2007-12-31T16:30:17
316-C0006E-8H-1,0.0	48.190	48.190	316-C0006E-8H-CC,75.0	58.880	57.690	[Section 1; fergussenc, 2007-12-31T16:31:08] Dark gray very fine to fine sand with minor contributions (interbedded) of silts with sand and silty clay. [Section 6; fergussenc, 2007-12-31T16:32:29] Dark gray fine sand throughout, very soupy.	Small spherical voids 0.5cm that could be degassing features? [Section 8; fergussenc,2007-12-31T16:33:13] Mainly dark gray fine sand with patches of greenish gray silty clay (floating as patches in the kind of soupy sand reflecting drilling disturbance).	[Section 9; fergussenc, 2007-12-30T21:34:46] Patches of both sand and silty clay mixed due to heavy drilling disturance. More sandy in the upper part and more silty in the lower part.	Speck of sponge spicules at 40 cm [Section CC; fergussenc, 2007-12-31T16:33:49] Both, mixed sandy and silty clayey interval, all mixed up due to drilling.					2008-01-17T05:13:44
316-C0006E-8H-1,0.0	48.190	48.190	316-C0006E-8H-1,139.5	49.585	49.430						Dark gray very fine to fine sand with minor contributions (interbedded) of silts with sand and silty clay.			2007-12-31T16:31:08
316-C0006E-8H-6,0.0	53.450	52.864	316-C0006E-8H-6,141.5	54.865	54.122						Dark gray fine sand throughout, very soupy. Small spherical voids 0.5 cm that could be degassing features?			2007-12-31T16:32:29
316-C0006E-8H-8,0.0	56.280	55.379	316-C0006E-8H-8,140.5	57.685	56.628						Mainly dark gray fine sand with patches of greenish gray silty clay (floating as patches in the kind of soupy sand reflecting drilling disturbance).			2007-12-31T16:33:13
316-C0006E-8H-9,0.0	57.685	56.628	316-C0006E-8H-9,44.5	58.130	57.023						Patches of both sand and silty clay mixed due to heavy drilling disturance. More sandy in the upper part and more silty in the lower part. Speck of sponge spicules at 40 cm			2007-12-30T21:34:46
316-C0006E-8H-CC,0.0	58.130	57.023	316-C0006E-8H-CC,75.0	58.880	57.690						Both, mixed sandy and silty clayey interval, all mixed up due to drilling.			2007-12-31T16:33:49
316-C0006E-9H-1,0.0	57.690	57.690	316-C0006E-9H-CC,58.5	64.565	64.505	[Section 1; fergussenc, 2007-12-31T16:34:16] Dark gray to dark greenish gray, very fine to silty sand layers interbedded with silty clay, heavily drilling disturbed. [Section 2; fergussenc, 2007-12-31T16:34:39] Specks of white sponge spicules at 18 cm.	[Section 4; fergussenc, 2007-12-31T16:35:32] Mostly soupy fine sand with patches of silty clay. In the upper and lowermost part, propably more hemi-pelagic deposits but hard to tell due to heavy drilling disturbance.	[Section 6; fergussenc, 2007-12-31T16:35:59] As in previous sections. [Section CC; fergussenc, 2007-12-31T16:36:21] Mostly sandy with patches (flow in structures) of silty clay.						2008-01-17T05:13:52
316-C0006E-9H-1,0.0	57.690	57.690	316-C0006E-9H-1,141.5	59.105	59.093						Dark gray to dark greenish gray, very fine to silty sand layers interbedded with silty clay, heavily drilling disturbed.			2007-12-31T16:34:16
316-C0006E-9H-2,0.0	59.105	59.093	316-C0006E-9H-2,138.5	60.490	60.466						Specks of white sponge spicules at 18 cm.			2007-12-31T16:34:39
316-C0006E-9H-4,0.0	61.070	61.041	316-C0006E-9H-4,134.0	62.410	62.369						Mostly soupy fine sand with patches of silty clay. In the upper and lowermost part, propably more hemi-pelagic deposits but hard to tell due to heavy drilling disturbance.			2007-12-31T16:35:32
316-C0006E-9H-6,0.0	62.640	62.597	316-C0006E-9H-6,134.0	63.980	63.925						As in previous sections.			2007-12-31T16:35:59
316-C0006E-9H-CC,0.0	63.980	63.925	316-C0006E-9H-CC,58.5	64.565	64.505						Mostly sandy with patches (flow in structures) of silty clay.			2007-12-31T16:36:21
316-C0006E-10H-8,0.0	64.510	64.510	316-C0006E-10H-CC,16.0	64.670	64.670	[Section CC; fergussenc, 2007-12-30T20:11:11] Dark gray fine sand, no recovery apart from core catcher.								2008-01-17T05:13:58
316-C0006E-10H-CC,0.0	64.510	64.510	316-C0006E-10H-CC,16.0	64.670	64.670						Dark gray fine sand, no recovery apart from core catcher.			2007-12-30T20:11:11
316-C0006E-11H-1,0.0	64.670	64.670	316-C0006E-11H-CC,34.5	71.674	71.484	[Section 1; fergussenc, 2007-12-31T01:35:23] Dominant lithology is a dark gray to black fine sand with thinner intervals of dark greenish-gray silty clay.								2008-01-17T05:14:05
316-C0006E-11H-1,0.0	64.670	64.670	316-C0006E-11H-1,141.0	66.080	66.042						Dominant lithology is a dark gray to black fine sand with thinner intervals of dark greenish-gray silty clay.			2007-12-31T01:35:23
316-C0006E-12H-1,0.0	71.480	71.480	316-C0006E-12H-CC,13.0	78.280	77.820	[Section 6; fergussenc, 2007-12-31T03:14:06] IW								2008-01-17T05:14:12
316-C0006E-12H-6,0.0	76.305	75.979	316-C0006E-12H-6,21.5	76.520	76.179						IW			2007-12-31T03:14:06
316-C0006E-13H-1,0.0	77.820	77.820	316-C0006E-13H-CC,15.0	79.345	79.325	[Section 1; fergussenc, 2007-12-31T02:55:55] Dark gray to dark greenish-gray clayey silt and clayey-silty sand with intervals of silty clay.								2008-01-17T05:14:17
316-C0006E-13H-1,0.0	77.820	77.820	316-C0006E-13H-1,137.5	79.195	79.177						Dark gray to dark greenish-gray clayey silt and clayey-silty sand with intervals of silty clay.			2007-12-31T02:55:55
316-C0006E-15X-1,0.0	79.330	79.330	316-C0006E-15X-CC,15.0	85.643	85.643	[Section 1; fergussenc, 2007-12-31T21:10:14] 5 to 10 thick sand and sandy silt layers with interbedded intervals ot thin silty clay layers.	[Section 7; mikistrasser, 2007-12-31T09:34:36] brownish gray band within sand containing sand-gluetinated borrows at ca. 100cm							2008-01-17T05:14:22
316-C0006E-15X-1,0.0	79.330	79.330	316-C0006E-15X-1,141.0	80.740	80.740						5 to 10 thick sand and sandy silt layers with interbedded intervals ot thin silty clay layers. Generally fining upwards intervals showing sucessions of gradual sand silt clay sucessions with commonly a greenish silty clay cap, e.g at 63 cm.	Individual sand layers vary in color from somewhat brownish gray, dark greenish gray and dark gray and as observed in SS analyses also show differences in composition.		2007-12-31T21:10:14
316-C0006E-15X-7,0.0	84.428	84.428	316-C0006E-15X-7,106.5	85.493	85.493						brownish gray band within sand containing sand-gluetinated borrows at ca. 100cm			2007-12-31T09:34:36
316-C0006E-16X-1,0.0	88.830	88.830	316-C0006E-16X-CC,19.0	90.890	90.890	[Section 1; fergussenc, 2007-12-31T21:11:37] Succession of dark greenish gray and dark gray sand layers that fine upwards into silty clay.								2008-01-17T05:14:29
316-C0006E-16X-1,0.0	88.830	88.830	316-C0006E-16X-1,128.0	90.110	90.110						Succession of dark greenish gray and dark gray sand layers that fine upwards into silty clay.			2007-12-31T21:11:37
316-C0006E-17X-1,0.0	98.330	98.330	316-C0006E-17X-CC,38.0	102.035	102.035	[Section 1; fergussenc, 2007-12-31T21:13:42] Mostly dark greenish gray silty clay with interbedded dark gray sand layer. between 25 and 60 cm the sand layer are only about 1 cm thick. Partly mixed due to moderate drilling disturbance.	[Section 5; fergussenc, 2007-12-31T21:14:17] Small white specks at 17 cm (sand filled borrows?).							2008-01-17T05:14:34
316-C0006E-17X-1,0.0	98.330	98.330	316-C0006E-17X-1,141.0	99.740	99.740						Mostly dark greenish gray silty clay with interbedded dark gray sand layer. between 25 and 60 cm the sand layer are only about 1 cm thick. Partly mixed due to moderate drilling disturbance.			2007-12-31T21:13:42
316-C0006E-17X-5,0.0	101.175	101.175	316-C0006E-17X-5,48.0	101.655	101.655						Small white specks at 17 cm (sand filled borrows?).			2007-12-31T21:14:17
316-C0006E-18X-1,0.0	106.330	106.330	316-C0006E-18X-CC,34.0	108.040	108.040	[Section 1; fergussenc, 2007-12-31T21:15:08] Greenish gray silty clay interbedded with dark greenish gray to dark gray sand beds that commonly show grading and fining upwards trends from sand to silt to silty clay.	[Section CC; fergussenc, 2007-12-31T21:15:49] Lower part of core catcher only contains pieces of relatively indurated claystones with pinkish surfaces. SS show that the pink material is a relatively unaltered volcanic ash.							2008-01-17T05:14:42
316-C0006E-18X-1,0.0	106.330	106.330	316-C0006E-18X-1,137.0	107.700	107.700						Greenish gray silty clay interbedded with dark greenish gray to dark gray sand beds that commonly show grading and fining upwards trends from sand to silt to silty clay.			2007-12-31T21:15:08
316-C0006E-18X-CC,0.0	107.700	107.700	316-C0006E-18X-CC,34.0	108.040	108.040						Lower part of core catcher only contains pieces of relatively indurated claystones with pinkish surfaces. SS show that the pink material is a relatively unaltered volcanic ash.			2007-12-31T21:15:49
316-C0006E-19X-1,0.0	115.830	115.830	316-C0006E-19X-CC,15.0	121.030	121.030	[Section 1; fergussenc, 2007-12-31T21:16:16] Mainly greenish gray silty clay with interbedded dark gray graded sand layers. [Section 6; mikistrasser, 2007-12-31T15:24:01] At 64 cm, white borrow fills (ash).								2008-01-17T05:14:49
316-C0006E-19X-1,0.0	115.830	115.830	316-C0006E-19X-1,109.0	116.920	116.920						Mainly greenish gray silty clay with interbedded dark gray graded sand layers.			2007-12-31T21:16:16
316-C0006E-19X-6,0.0	120.080	120.080	316-C0006E-19X-6,80.0	120.880	120.880						At 64 cm, white borrow fills (ash).			2007-12-31T15:24:01
316-C0006E-20X-1,0.0	125.330	125.330	316-C0006E-20X-CC,18.5	133.360	133.360	[Section 1; fergussenc, 2007-12-31T22:00:52] Interbedded greenish-gray silty clay with graded beds of dark gray sand and sandy silt. [Section 2; fergussenc, 2007-12-31T22:01:29] Patch of sand at 80 to 85 cm.	[Section 5; fergussenc, 2007-12-31T22:04:23] Patch of silty clay at 10 to 15 cm. Patch of sandy silt at 122 to 126 cm.							2008-01-17T05:14:54
316-C0006E-20X-1,0.0	125.330	125.330	316-C0006E-20X-1,141.5	126.745	126.745						Interbedded greenish-gray silty clay with graded beds of dark gray sand and sandy silt.			2007-12-31T22:00:52
316-C0006E-20X-2,0.0	126.745	126.745	316-C0006E-20X-2,141.5	128.160	128.160						Patch of sand at 80 to 85 cm.			2007-12-31T22:01:29
316-C0006E-20X-5,0.0	131.005	131.005	316-C0006E-20X-5,141.0	132.415	132.415						Patch of silty clay at 10 to 15 cm. Patch of sandy silt at 122 to 126 cm.			2007-12-31T22:04:23
316-C0006E-21X-1,0.0	134.830	134.830	316-C0006E-21X-CC,36.5	139.640	139.640	[Section 1; fergussenc, 2008-01-01T23:12:10] Dark green-gray silty clay with silt layer at base of section. [Section 2; fergussenc, 2008-01-01T23:13:26] Graded dark green-gray fine to very fine sands initerlayered with dark greenish-gray silty clay.	[Section 4; fergussenc, 2008-01-01T23:14:11] Discontinuous light gray volcanic ash at 25 cm. Very light gray volcanic ash at 135 to 137 cm.							2008-01-17T05:15:00
316-C0006E-21X-1,0.0	134.830	134.830	316-C0006E-21X-1,145.0	136.280	136.280						Dark green-gray silty clay with silt layer at base of section.			2008-01-01T23:12:10
316-C0006E-21X-2,0.0	136.280	136.280	316-C0006E-21X-2,110.0	137.380	137.380						Graded dark green-gray fine to very fine sands initerlayered with dark greenish-gray silty clay.			2008-01-01T23:13:26
316-C0006E-21X-4,0.0	137.695	137.695	316-C0006E-21X-4,141.0	139.105	139.105						Discontinuous light gray volcanic ash at 25 cm. Very light gray volcanic ash at 135 to 137 cm.			2008-01-01T23:14:11
316-C0006E-22X-1,0.0	144.330	144.330	316-C0006E-22X-CC,32.0	151.705	151.705	[Section 1; fergussenc, 2008-01-02T15:51:01] Lithology throughout core 22X: sucessions of gray to dark greenish gray sands that fine upward into grayish olive to olive gray silty clays.	Apart from generally fining upwards trend, sands are structureless but occasionaly may show vague parallel lamination (e.g in 22X-CC).	Smear slide analyses of sands reveal relatively high portions of metamorphic grains and little to absent volcanoclastic particles.						2008-01-17T05:15:06
316-C0006E-22X-1,0.0	144.330	144.330	316-C0006E-22X-1,141.0	145.740	145.740						Lithology throughout core 22X: sucessions of gray to dark greenish gray sands that fine upward into grayish olive to olive gray silty clays.	Apart from generally fining upwards trend, sands are structureless but occasionaly may show vague parallel lamination (e.g in 22X-CC).	Smear slide analyses of sands reveal relatively high portions of metamorphic grains and little to absent volcanoclastic particles.	2008-01-02T15:51:01
316-C0006E-23X-1,0.0	153.830	153.830	316-C0006E-23X-CC,20.0	162.435	162.435	[Section 1; mikistrasser, 2008-01-02T14:08:17] Lithology throughout core 23X: Sucessions of gray to dark greenish gray sands that fine upward into olive gray to grayish olive silty clays.	Appart from generally fining upwards trend, sands are structureless [Section 6; fergussenc, 2008-01-02T15:49:10] Between 70 and 90 cm, sand is slightly lighter in grayish color hue and slightly coarser than elsewhere in the core.	Small void between 111 and 113 cm (most likely washed out sand).						2008-01-17T05:15:12
316-C0006E-23X-1,0.0	153.830	153.830	316-C0006E-23X-1,140.5	155.235	155.235						Lithology throughout core 23X: Sucessions of gray to dark greenish gray sands that fine upward into olive gray to grayish olive silty clays. Appart from generally fining upwards trend, sands are structureless			2008-01-02T14:08:17
316-C0006E-23X-6,0.0	159.485	159.485	316-C0006E-23X-6,141.0	160.895	160.895						Between 70 and 90 cm, sand is slightly lighter in grayish color hue and slightly coarser than elsewhere in the core. Small void between 111 and 113 cm (most likely washed out sand).			2008-01-02T15:49:10
316-C0006E-24X-1,0.0	163.330	163.330	316-C0006E-24X-CC,42.5	164.910	164.910	[Section 1; fergussenc, 2008-01-02T15:45:26] Dominant lithology is olive-gray silty clay with patches of black medium to coarse sand at 7 to 20 cm.								2008-01-17T05:15:19
316-C0006E-24X-1,0.0	163.330	163.330	316-C0006E-24X-1,115.5	164.485	164.485						Dominant lithology is olive-gray silty clay with patches of black medium to coarse sand at 7 to 20 cm.			2008-01-02T15:45:26
316-C0006E-25X-1,0.0	172.830	172.830	316-C0006E-25X-CC,41.0	181.957	181.957	[Section 1; fergussenc, 2008-01-02T20:16:08] Sequence of very fine grained, graded turbidites. Olive-grey silty clay is most dominant lithology, followed by dark olive-grey clayey silt then dark-grey v.f. sand.	[Section 7; fergussenc, 2008-01-01T23:57:51] 2 cm ash layer found at bottom of IW section.							2008-01-17T05:15:25
316-C0006E-25X-1,0.0	172.830	172.830	316-C0006E-25X-1,140.5	174.235	174.235						Sequence of very fine grained, graded turbidites. Olive-grey silty clay is most dominant lithology, followed by dark olive-grey clayey silt then dark-grey v.f. sand.			2008-01-02T20:16:08
316-C0006E-25X-7,0.0	180.787	180.787	316-C0006E-25X-7,34.0	181.127	181.127						2 cm ash layer found at bottom of IW section.			2008-01-01T23:57:51
316-C0006E-26X-1,0.0	182.330	182.330	316-C0006E-26X-CC,37.0	192.477	191.827	[Section 1; fergussenc, 2008-01-02T23:23:19] Dominant lithology is a olive-gray silty clay with interbeds of silt and sandy silt with gradational upper contacts to overlying silty clay and sharp lower contacts.								2008-01-17T05:15:31
316-C0006E-26X-1,0.0	182.330	182.330	316-C0006E-26X-1,149.0	183.820	183.725						Dominant lithology is a olive-gray silty clay with interbeds of silt and sandy silt with gradational upper contacts to overlying silty clay and sharp lower contacts.			2008-01-02T23:23:19
316-C0006E-27X-1,0.0	191.830	191.830	316-C0006E-27X-CC,47.0	201.940	201.330	[Section 1; mikistrasser, 2008-01-03T09:26:08] Dominant lithology throughout core 27X is a olive-gray silty clay with interbeds of fine sands and sandy silt with gradational upper contacts to overlying silty clay and sharp lower contacts.	[Section 3; mikistrasser, 2008-01-03T10:50:50] White specks mainly of composed of sand-sized Qz and Fsp grains > sand filled borrow structure at 74, 100 and 115 cm	[Section 8; mikistrasser, 2008-01-03T10:52:38] Very thin (1 mm thick) white laminae at 55 cm, maily composed of well sorted very fine sand Qz and Fsp grains.						2008-01-17T05:15:37
316-C0006E-27X-1,0.0	191.830	191.830	316-C0006E-27X-1,141.0	193.240	193.155						Dominant lithology throughout core 27X is a olive-gray silty clay with interbeds of fine sands and sandy silt with gradational upper contacts to overlying silty clay and sharp lower contacts.			2008-01-03T09:26:08
316-C0006E-27X-3,0.0	194.655	194.485	316-C0006E-27X-3,142.0	196.075	195.819						White specks mainly of composed of sand-sized Qz and Fsp grains > sand filled borrow structure at 74, 100 and 115 cm			2008-01-03T10:50:50
316-C0006E-27X-8,0.0	200.315	199.803	316-C0006E-27X-8,115.5	201.470	200.888						Very thin (1 mm thick) white laminae at 55 cm, maily composed of well sorted very fine sand Qz and Fsp grains.			2008-01-03T10:52:38
316-C0006E-28X-1,0.0	201.330	201.330	316-C0006E-28X-CC,38.0	205.395	205.395	[Section 1; mikistrasser, 2008-01-03T10:39:24] Dominant lithology throughout core 28X is a olive-gray silty clay with interbeds of very fine sand and sandy silts with gradational upper contacts to overlying silty clay and sharp lower contacts.	Some thinner sand layers however also show a distinct upper contact [Section 2; mikistrasser, 2008-01-03T10:42:46] White speck at 97 cm -> Qz and Fsp filled borrow							2008-01-17T05:15:44
316-C0006E-28X-1,0.0	201.330	201.330	316-C0006E-28X-1,141.0	202.740	202.740						Dominant lithology throughout core 28X is a olive-gray silty clay with interbeds of very fine sand and sandy silts with gradational upper contacts to overlying silty clay and sharp lower contacts.	Some thinner sand layers however also show a distinct upper contact		2008-01-03T10:39:24
316-C0006E-28X-2,0.0	202.740	202.740	316-C0006E-28X-2,106.5	203.805	203.805						White speck at 97 cm -> Qz and Fsp filled borrow			2008-01-03T10:42:46
316-C0006E-29X-1,0.0	210.830	210.830	316-C0006E-29X-CC,40.0	220.985	220.325	[Section 1; mikistrasser, 2008-01-03T14:06:23] Dominant lithology throughout core 29X is a olive-gray silty clay with interbeds of very fine sand and sandy silts with gradational upper contacts to overlying silty clay and generally sharp lower contacts.	The core generally is moderatly to heavily drilling distrubed due to biscuiting [Section 3; mikistrasser, 2008-01-03T14:23:25] Patches of concentrated white specks (Qz and Fsp sand grains) -> sand filled borrows??							2008-01-17T05:15:50
316-C0006E-29X-1,0.0	210.830	210.830	316-C0006E-29X-1,143.0	212.260	212.167						Dominant lithology throughout core 29X is a olive-gray silty clay with interbeds of very fine sand and sandy silts with gradational upper contacts to overlying silty clay and generally sharp lower contacts.	The core generally is moderatly to heavily drilling distrubed due to biscuiting		2008-01-03T14:06:23
316-C0006E-29X-3,0.0	213.670	213.486	316-C0006E-29X-3,141.0	215.080	214.804						Patches of concentrated white specks (Qz and Fsp sand grains) -> sand filled borrows??			2008-01-03T14:23:25
316-C0006E-30X-1,0.0	220.330	220.330	316-C0006E-30X-CC,41.2	230.291	229.831	[Section 1; fergussenc, 2008-01-04T00:30:35] Olive gray silty clay with sandy silt and very fine sand layers. Sands and silts have sharp bases and graded tops. [Section 3; mikistrasser, 2008-01-03T23:18:34] I.W.								2008-01-17T05:15:56
316-C0006E-30X-1,0.0	220.330	220.330	316-C0006E-30X-1,141.0	221.740	221.675						Olive gray silty clay with sandy silt and very fine sand layers. Sands and silts have sharp bases and graded tops.			2008-01-04T00:30:35
316-C0006E-30X-3,0.0	223.155	223.025	316-C0006E-30X-3,38.0	223.535	223.387						I.W.			2008-01-03T23:18:34
316-C0006E-31X-1,0.0	229.830	229.830	316-C0006E-31X-CC,47.5	235.870	235.870	[Section 1; fergussenc, 2008-01-04T00:51:07] Olive-gray fine to medium, poorly sorted, massive sand with scattered white volcaniclastic grains with a maximum size of 2 mm, cocentrated in discreete layer at 35 cm.								2008-01-17T05:16:02
316-C0006E-31X-1,0.0	229.830	229.830	316-C0006E-31X-1,144.0	231.270	231.270						Olive-gray fine to medium, poorly sorted, massive sand with scattered white volcaniclastic grains with a maximum size of 2 mm, cocentrated in discreete layer at 35 cm.			2008-01-04T00:51:07
316-C0006E-32X-1,0.0	239.330	239.330	316-C0006E-32X-CC,38.5	248.460	248.460	[Section 1; mikistrasser,2008-01-04T09:41:48] Dominant Lithology in core 32X section 1 to 6 is a olive gray silty clay with occasionally interbedded with silts with sand or very fine silty sands Due to generally heavy drilling disturbances with biscuitng	throughout and slight splitting disturbances thin silt and sand layers might not alwayes be possible to observe [Section 2; mikistrasser, 2008-01-04T09:44:18] Dominant lithology as above Intervals of slighly greenish color hues occure between	10-16cm and 43-44 cm. [Section 7; mikistrasser, 2008-01-04T09:53:21] The lower fining upward succession is the uppermost part of the massive sand layer in section 8. [Section 8; mikistrasser, 2008-01-04T09:55:50]	Olive gray, poorly sorted massive, fine to medium grained sand with scattered white volcanoclastic grains (<1.5 mm)					2008-01-17T05:16:08
316-C0006E-32X-1,0.0	239.330	239.330	316-C0006E-32X-1,142.5	240.755	240.755						Dominant Lithology in core 32X section 1 to 6 is a olive gray silty clay with occasionally interbedded with silts with sand or very fine silty sands.	Due to generally heavy drilling disturbances with biscuitng throughout and slight splitting disturbances thin silt and sand layers might not alwayes be possible to observe.		2008-01-04T09:41:48
316-C0006E-32X-2,0.0	240.755	240.755	316-C0006E-32X-2,141.0	242.165	242.165						Dominant lithology as above. Intervals of slighly greenish color hues occure between 10-16cm and 43-44 cm.			2008-01-04T09:44:18
316-C0006E-32X-7,0.0	246.415	246.415	316-C0006E-32X-7,91.0	247.325	247.325						The lower fining upward succession is the uppermost part of the massive sand layer in section 8.			2008-01-04T09:53:21
316-C0006E-32X-8,0.0	247.325	247.325	316-C0006E-32X-8,75.0	248.075	248.075						Olive gray, poorly sorted massive, fine to medium grained sand with scattered white volcanoclastic grains (<1.5 mm)			2008-01-04T09:55:50
316-C0006E-34X-1,0.0	258.330	258.330	316-C0006E-34X-CC,37.0	266.995	266.995	[Section 1; mikistrasser, 2008-01-04T13:58:43] The dominant lithology throughout core 34X is a olive gray to dark olive gray silty clay (with some intervals being more indurated (silty claystone).	Interbedded are very fine sand and silt with sand layers that often grade into silty clays. Due to fracturing and buscuiting (heavily drilling distrubed) thin silty and sandy intervals are hard to be observed and/or	upper and lower contact of bed are not always well preserved						2008-01-17T05:16:16
316-C0006E-34X-1,0.0	258.330	258.330	316-C0006E-34X-1,141.0	259.740	259.740						The dominant lithology throughout core 34X is a olive gray to dark olive gray silty clay (with some intervals being more indurated (silty claystone). Interbedded are very fine sand and silt with sand layers that often grade into silty clays.	Due to fracturing and buscuiting (heavily drilling distrubed) thin silty and sandy intervals are hard to be observed and/or upper and lower contact of bed are not always well preserved		2008-01-04T13:58:43
316-C0006E-35X-1,0.0	267.830	267.830	316-C0006E-35X-CC,42.5	271.545	271.545	[Section 1; mikistrasser, 2008-01-04T19:13:26] Dark olive grey/greenish-grey silty clay with olive-grey graded silts.								2008-01-17T05:16:22
316-C0006E-35X-1,0.0	267.830	267.830	316-C0006E-35X-1,86.0	268.690	268.690						Dark olive grey/greenish-grey silty clay with olive-grey graded silts.			2008-01-04T19:13:26
316-C0006E-36X-1,0.0	277.330	277.330	316-C0006E-36X-CC,35.5	287.210	286.830	[Section 1; fergussenc, 2008-01-05T00:12:55] Grayish to greenish-gray silty claystone with planar lamination scattered throughout. Biscuits are developed and distinguishing silty layers is difficult.	[Section 2; fergussenc, 2008-01-05T00:16:31] Sandy silt in top 19 cm. [Section 5; fergussenc, 2008-01-05T01:33:39] Small normal faults at 70 cm.							2008-01-17T05:16:28
316-C0006E-36X-1,0.0	277.330	277.330	316-C0006E-36X-1,140.5	278.735	278.681						Grayish to greenish-gray silty claystone with planar lamination scattered throughout. Biscuits are developed and distinguishing silty layers is difficult.			2008-01-05T00:12:55
316-C0006E-36X-2,0.0	278.735	278.681	316-C0006E-36X-2,141.0	280.145	280.037						Sandy silt in top 19 cm.			2008-01-05T00:16:31
316-C0006E-36X-5,0.0	281.920	281.743	316-C0006E-36X-5,103.5	282.955	282.739						Small normal faults at 70 cm.			2008-01-05T01:33:39
316-C0006E-37X-1,0.0	286.830	286.830	316-C0006E-37X-CC,41.5	296.025	296.025	[Section 1; mikistrasser, 2008-01-05T15:57:36] The dominant lithology throughout core 37X olive gray silty claystone interbedded with sandy silts and very fine sand layers.	Due to moderately to high drilling disturbances (fracturing and biscuiting) smaller coarser interval are not always visible. Some pieces (mainly containing silt) show parallel lamination whereas other	(more abundant in claystone pieces) occasionaly show slight bioturbation (Chondrites).						2008-01-17T05:16:35
316-C0006E-37X-1,0.0	286.830	286.830	316-C0006E-37X-1,141.5	288.245	288.245						The dominant lithology throughout core 37X olive gray silty claystone interbedded with sandy silts and very fine sand layers. Due to moderately to high drilling disturbances (fracturing and biscuiting) smaller coarser interval are not always visible.	Some pieces (mainly containing silt) show parallel lamination whereas other (more abundant in claystone pieces) occasionaly show slight bioturbation (Chondrites).		2008-01-05T15:57:36
316-C0006E-38X-1,0.0	296.330	296.330	316-C0006E-38X-CC,43.0	297.720	297.720	[Section 1; mikistrasser, 2008-01-05T09:49:00] Generally biscuits of gray (when wet) to olive gray (when dry) silty claystones. Sand and silt interval can only be possitively identifies as laminae and might have been washed out -> low recovery								2008-01-17T05:16:40
316-C0006E-38X-1,0.0	296.330	296.330	316-C0006E-38X-1,36.5	296.695	296.695						Generally biscuits of gray (when wet) to olive gray (when dry) silty claystones. Sand and silt interval can only be possitively identifies as laminae and might have been washed out -> low recovery			2008-01-05T09:49:00
316-C0006E-39X-1,0.0	305.830	305.830	316-C0006E-39X-CC,48.5	315.835	315.325	[Section 1; fergussenc, 2008-01-05T16:15:19] Dominant lithology is a gray silty claystone with thin intervals of slightly coarser material that appears to be mainly siltstone. DRilling disturbance may mask some of the lithological variation.								2008-01-17T05:16:47
316-C0006E-39X-1,0.0	305.830	305.830	316-C0006E-39X-1,141.0	307.240	307.168						Dominant lithology is a gray silty claystone with thin intervals of slightly coarser material that appears to be mainly siltstone. DRilling disturbance may mask some of the lithological variation.			2008-01-05T16:15:19
316-C0006E-40X-1,0.0	315.330	315.330	316-C0006E-40X-CC,38.5	324.145	324.145	[Section 7; fergussenc, 2008-01-06T00:01:29] IW								2008-01-17T05:16:52
316-C0006E-40X-7,0.0	322.010	322.010	316-C0006E-40X-7,40.0	322.410	322.410						IW			2008-01-06T00:01:29
316-C0006E-41X-1,0.0	324.830	324.830	316-C0006E-41X-CC,38.0	332.023	332.023	[Section 1; mikistrasser, 2008-01-06T06:48:01] The dominant lithology throughout core 41X is a greenish gray silty clay with slightly coarser intervals (clayey silts). The core is partly heavily drilling disturbed and fractured.	More brecciated intervals may correspond to slightly coarse intervals (clayey silts), but difficult to tell. There is a ca. 1.8 meter thick sand in section 2 and lower part of section 1 (see notes in sections 2)	[Section 2; mikistrasser, 2008-01-06T06:52:34] The fine fraction of the sand intervals shows a clear fining upward trend (from somewhat fine to medium sand to very fine sand), whereas the coarse fraction is poorly sorted and	ranges between fine sand up to very fine pebbles containing grains of agglutinated sand and pumice. [Section 5; mikistrasser, 2008-01-06T07:01:04] 1 mm thin layer of very fine grained opac minerals (Pyrite? ??Oxide? at 96cm					2008-01-17T05:16:58
316-C0006E-41X-1,0.0	324.830	324.830	316-C0006E-41X-1,141.5	326.245	326.245						The dominant lithology throughout core 41X is a greenish gray silty clay with slightly coarser intervals (clayey silts). The core is partly heavily drilling disturbed and fractured.	More brecciated intervals may correspond to slightly coarse intervals (clayey silts), but difficult to tell. There is a ca. 1.8 meter thick sand in section 2 and lower part of section 1 (see notes in sections 2)		2008-01-06T06:48:01
316-C0006E-41X-2,0.0	326.245	326.245	316-C0006E-41X-2,140.5	327.650	327.650						The fine fraction of the sand intervals shows a clear fining upward trend (from somewhat fine to medium sand to very fine sand), whereas the coarse fraction is poorly sorted and	ranges between fine sand up to very fine pebbles containing grains of agglutinated sand and pumice.		2008-01-06T06:52:34
316-C0006E-41X-5,0.0	329.210	329.210	316-C0006E-41X-5,126.3	330.473	330.473						1 mm thin layer of very fine grained opac minerals (Pyrite? ??Oxide? at 96cm			2008-01-06T07:01:04
316-C0006E-42X-1,0.0	334.330	334.330	316-C0006E-42X-CC,47.5	344.268	343.828	[Section 1; mikistrasser, 2008-01-06T10:25:37] Lithology throughout core 42X is a slightly bioturbated, greenish gray silty claystone interbedded with greenish gray to gray siltstones that often show parallel and occasionally cross lamination.	Slight to moderate drilling distubances (especially in intervals that are more brecciated and fractured) may generally contain thin layers of slightly coarser deposits (clayey siltone or siltstones)	but are not allwayes recognizable due to the drilling disturbance. [Section 3; mikistrasser, 2008-01-06T10:20:58] Siltstone bed at 78 to 101cm shows somewhat coarser base (-> silty with sand)						2008-01-17T05:17:05
316-C0006E-42X-1,0.0	334.330	334.330	316-C0006E-42X-1,139.5	335.725	335.663						Lithology throughout core 42X is a slightly bioturbated, greenish gray silty claystone interbedded with greenish gray to gray siltstones that often show parallel and occasionally cross lamination.	Slight to moderate drilling distubances (especially in intervals that are more brecciated and fractured) may generally contain thin layers of slightly coarser deposits (clayey siltone or siltstones)	but are not allwayes recognizable due to the drilling disturbance.	2008-01-06T10:25:37
316-C0006E-42X-3,0.0	337.145	337.020	316-C0006E-42X-3,140.5	338.550	338.363						Siltstone bed at 78 to 101cm shows somewhat coarser base (-> silty with sand)			2008-01-06T10:20:58
316-C0006E-43X-1,0.0	343.830	343.830	316-C0006E-43X-CC,39.5	352.475	352.475	[Section 1; mikistrasser, 2008-01-06T14:01:15] slightly bioturbated, greenish gray silty claystone interbedded with siltstone beds that sometimes show parallel lamination and often grade into overlying silty claystone Intervals showing	more intense drilling disturbance (fracturing and brecciationg) often contain slighly coarser silt sized grains. [Section 3; mikistrasser, 2008-01-06T14:22:41] Base of grading upward intervals at 16, 34, 57 and 95 are some what coarser and contain sand	- > AA127siltstone with sand [Section CC; mikistrasser, 2008-01-06T14:43:29] CC has a olive gray rather than a greenish gray color hue						2008-01-17T05:17:10
316-C0006E-43X-1,0.0	343.830	343.830	316-C0006E-43X-1,141.0	345.240	345.240						slightly bioturbated, greenish gray silty claystone interbedded with siltstone beds that sometimes show parallel lamination and often grade into overlying silty claystone.	Intervals showing more intense drilling disturbance (fracturing and brecciationg) often contain slighly coarser silt sized grains.		2008-01-06T14:01:15
316-C0006E-43X-3,0.0	346.650	346.650	316-C0006E-43X-3,141.5	348.065	348.065						Base of grading upward intervals at 16, 34, 57 and 95 are some what coarser and contain sand -> siltstone with sand			2008-01-06T14:22:41
316-C0006E-43X-CC,0.0	352.080	352.080	316-C0006E-43X-CC,39.5	352.475	352.475						CC has a olive gray rather than a greenish gray color hue			2008-01-06T14:43:29
316-C0006E-44X-1,0.0	353.330	353.330	316-C0006E-44X-CC,43.0	363.315	362.825	[Section 1; fergussenc, 2008-01-06T16:51:11] Olive gray to gray silty claystone withthin siltstone beds with sharp bases and indistinct to graded tops.	[Section 2; fergussenc, 2008-01-06T18:51:41] Fine dispersed organic matter visible in more complete core sections.	[Section 4; fergussenc, 2008-01-06T19:10:00] 65-135 cm - zone of intense drilling mud incursions and softer lithology. Siltier then background claystone though still contains a lot of clay. [Section 5; fergussenc, 2008-01-06T19:14:46] I.W.						2008-01-17T05:17:16
316-C0006E-44X-1,0.0	353.330	353.330	316-C0006E-44X-1,142.0	354.750	354.680						Olive gray to gray silty claystone withthin siltstone beds with sharp bases and indistinct to graded tops.			2008-01-06T16:51:11
316-C0006E-44X-2,0.0	354.750	354.680	316-C0006E-44X-2,141.5	356.165	356.026						Fine dispersed organic matter visible in more complete core sections.			2008-01-06T18:51:41
316-C0006E-44X-4,0.0	357.575	357.367	316-C0006E-44X-4,141.5	358.990	358.712						65-135 cm - zone of intense drilling mud incursions and softer lithology. Siltier then background claystone though still contains a lot of clay.			2008-01-06T19:10:00
316-C0006E-44X-5,0.0	358.990	358.712	316-C0006E-44X-5,38.0	359.370	359.074						I.W.			2008-01-06T19:14:46
316-C0006E-45X-1,0.0	362.830	362.830	316-C0006E-45X-CC,44.0	372.785	372.335	[Section 1; fergussenc, 2008-01-06T21:58:03] Grayish slity claystone with thin siltstone beds. [Section 5; fergussenc, 2008-01-06T23:28:04] Heavily brecciated by drilling, gray silty claystone.	[Section 7; fergussenc, 2008-01-07T02:34:38] Abundant organic material and wood fragments in v.f. sands and silts, up to 50% of sand in places (near the top of the sandy parts of the beds).	Sand injections and associated features are common throughout the section.						2008-01-17T05:17:22
316-C0006E-45X-1,0.0	362.830	362.830	316-C0006E-45X-1,139.5	364.225	364.162						Grayish slity claystone with thin siltstone beds.			2008-01-06T21:58:03
316-C0006E-45X-5,0.0	367.050	366.859	316-C0006E-45X-5,141.5	368.465	368.210						Heavily brecciated by drilling, gray silty claystone.			2008-01-06T23:28:04
316-C0006E-45X-7,0.0	369.875	369.556	316-C0006E-45X-7,142.0	371.295	370.912						Abundant organic material and wood fragments in v.f. sands and silts, up to 50% of sand in places (near the top of the sandy parts of the beds). Sand injections and associated features are common throughout the section.			2008-01-07T02:34:38
316-C0006E-46X-1,0.0	372.330	372.330	316-C0006E-46X-CC,42.0	380.645	380.645	[Section 1; fergussenc, 2008-01-07T16:18:37] Greenish gray silty claystone interbedded with siltstone beds that often grade upwards into silty claystone, often show parallel lamination and occasional have coarser silt with sand at their base.								2008-01-17T05:17:28
316-C0006E-46X-1,0.0	372.330	372.330	316-C0006E-46X-1,142.0	373.750	373.750						Greenish gray silty claystone interbedded with siltstone beds that often grade upwards into silty claystone, often show parallel lamination and occasional have coarser silt with sand at their base.			2008-01-07T16:18:37
316-C0006E-47X-1,0.0	381.830	381.830	316-C0006E-47X-CC,40.5	391.740	391.330	[Section 1; fergussenc, 2008-01-07T16:17:44] Greenish gray silty claystone with interbedded siltstone beds.	[Section 2; mikistrasser, 2008-01-07T14:00:57] Siltstone interval between 58 and 105 cm is composed of a succession of a minimum of 3 observable amalgamated siltone beds	[Section 6; fergussenc, 2008-01-07T16:20:05] Ash layer shows a 1cm light gray, fine grained base and an upper, light gray to olive gray, slightly coarser upper part with patches of greenish gray volcanic material containing pumice fragments.	Interestingly the ash intervall also shows high concentration of nannofossils in smear slide. [Section 8; fergussenc, 2008-01-07T16:20:37] Below 55 cm silty claystone is somewhat lighter gray in color hue and softer.	It is heavily biscuited with drilling mud injections up to 1cm thick. [Section 9; mikistrasser, 2008-01-07T14:35:46] 0 - 86 cm as in previous section below 55cm				2008-01-17T05:17:33
316-C0006E-47X-1,0.0	381.830	381.830	316-C0006E-47X-1,140.0	383.230	383.172						Greenish gray silty claystone with interbedded siltstone beds.			2008-01-07T16:17:44
316-C0006E-47X-2,0.0	383.230	383.172	316-C0006E-47X-2,141.5	384.645	384.529						Siltstone interval between 58 and 105 cm is composed of a succession of a minimum of 3 observable amalgamated siltone beds			2008-01-07T14:00:57
316-C0006E-47X-6,0.0	387.100	386.882	316-C0006E-47X-6,39.5	387.495	387.261						Ash layer shows a 1cm light gray, fine grained base and an upper, light gray to olive gray, slightly coarser upper part with patches of greenish gray volcanic material containing pumice fragments.	Interestingly the ash intervall also shows high concentration of nannofossils in smear slide.		2008-01-07T16:20:05
316-C0006E-47X-8,0.0	388.900	388.608	316-C0006E-47X-8,141.5	390.315	389.964						Below 55 cm silty claystone is somewhat lighter gray in color hue and softer. It is heavily biscuited with drilling mud injections up to 1cm thick.			2008-01-07T16:20:37
316-C0006E-47X-9,0.0	390.315	389.964	316-C0006E-47X-9,102.0	391.335	390.942						0 - 86 cm as in previous section below 55cm			2008-01-07T14:35:46
316-C0006E-48X-1,0.0	391.330	391.330	316-C0006E-48X-CC,47.0	401.305	400.825	[Section 1; fergussenc, 2008-01-07T19:12:48] Grayish silty claystone with patch of white-gray volcanic ash at 85 cm. Chondrites is present along with siltstone layers and some greenish color bands in other sections.	[Section 3; fergussenc, 2008-01-07T19:37:30] Gray volcanic ash layers at 56 to 58 cm and 63 to 64 cm. Sponge spicule lined burrow? at 30 cm.							2008-01-17T05:17:42
316-C0006E-48X-1,0.0	391.330	391.330	316-C0006E-48X-1,141.0	392.740	392.672						Grayish silty claystone with patch of white-gray volcanic ash at 85 cm. Chondrites is present along with siltstone layers and some greenish color bands in other sections.			2008-01-07T19:12:48
316-C0006E-48X-3,0.0	394.160	394.024	316-C0006E-48X-3,141.5	395.575	395.371						Gray volcanic ash layers at 56 to 58 cm and 63 to 64 cm. Sponge spicule lined burrow? at 30 cm.			2008-01-07T19:37:30
316-C0006E-49X-1,0.0	400.830	400.830	316-C0006E-49X-CC,21.0	406.945	406.945	[Section 1; fergussenc, 2008-01-08T01:46:40] Greenish-grey to olive-grey silty clay to clayey-silt. Olive-grey siltstones have sharp bases and gradual tops. Volcanic ash and lapilli also present. [Section 4; fergussenc, 2008-01-08T01:58:17] I.W.								2008-01-17T05:17:47
316-C0006E-49X-1,0.0	400.830	400.830	316-C0006E-49X-1,141.0	402.240	402.240						Greenish-grey to olive-grey silty clay to clayey-silt. Olive-grey siltstones have sharp bases and gradual tops. Volcanic ash and lapilli also present.			2008-01-08T01:46:40
316-C0006E-49X-4,0.0	404.680	404.680	316-C0006E-49X-4,41.0	405.090	405.090						I.W.			2008-01-08T01:58:17