G105 0647A071R020320004 71r-2, 32 cm to 71r-3, 110 cm KUE FINELY CRYSTALLINE, APHYRIC BASALT. see comments see comments see comments see comments see comments see comments see comments H=20, v=3. Section 647A-71R-4, greenish gray (5G5/1) with very rare vesicles 1 mm in diameter which are partly filled with calcite. Very few altered veins, frequent horizontal veins up to 3 mm thick. A few vertical veins are present with occasional veins up to 1 mm thick. Both types are filled with: a. calcite (dominant) b. chlorite (abundant) c. pyrite (common). Thirty-one horizontal or almost horizontal fractures (veins filled). One to two nearly vertical fractures, rest see comments. With scattered < 1 mm vesicles filled with chlorite and calcite. The most striking feature is stockwork veins of calcite and chlorite which are < 5 mm wide. The rocks are greenish gray (5G 5/1). No obvious alteration is observed. This unit is probably part of a thin flow because it is so finely crystalline. No salvages are present. Fracture: Some of which are filled (veins). Grain size coarsens downward. N G105 0647A071R020730001 2 KUE COARSELY CRYSTALLINE CALCITE AND CHLORITE see comments see comments see comments see comments see comments see comments Strong, with numerous crosscutting veins, devitrification of fragments, soft chlorite and calcite hydrothermal void filling. I = 2. Occurring as a hydrothermal meshwork of radiating white crystals and veins, which surround irregular fragments (2-3 cm in diameter) with internal large-scale spherulitic texture. These appear glassy on uncut surfaces. The color is pale gray to white. Basement rock was recovered at the bottom of this core in section 647A-71R-2. N G105 0647A071R020820002 2 KUE APHYRIC FINELY CRYSTALLINE (UPPER CONTACT) TO SPHERULITIC OR VARIOLITIC. see comments Absent. see comments Dark greenish gray (5BG 4/1) To 2 cm long and < 1 cm high, filled with calcite and chlorite. see comments Little apparent, except for crosscutting vein of chlorite. see comments (< 1 mm variolites) basalt with large calcite-filled vesicles (0.7 x 2 cm maximum). Cross-cutting vein breaks through top, which has a botryoidal, laminated crust, 0.1-0.5 mm thick. Top 1 cm seems to be a chilled margin. This unit is probably a flow, with original glassy top. Large fragments in Unit 1 are probably flow-top breccia. Crystallinity: Aphanitic to finely crystalline and variolitic. Top could be pillow salvage. N G105 0647A071R020820003 2A-2B KUE TALC-OR PYROPHYLLITE - BEARING BASALT. see comments see comments see comments Greenish gray (5BG 5/1) with a chalky luster n/a up to < 5 mm n/a n/a see comments Strong V = 1. The material is strongly altered by veins of calcite This rock may be the altered equivalent of UNIT 4 below. N G105 0647A071RCC0000005 1-3 KUE APHYRIC, FINE-GRAINED BASALT n/a n/a n/a Dark gray to dark greenish gray None Observed n/a Very slightly altered to unaltered 3 mm thick vein Horizontal vein, vertical fracture n/a One vein filled with calcite; One fracture N G105 0647A072R010000001 72R-1, 0 cm to 72R-3, 10 cm KUE FINE-GRAINED APHYRIC BASALT see comments Pyroxene < 1 Up to 1 mm in diameter see comments Gray (2.5Y N5). see comments see comments No visible alteration. SH = 3; I = 10; SV = 1. 1a: talc-filled vein on the bottom 6 mm. 1a: strongly altered, greenish mixture of different minerals strongly fractured. 2a: 2-5 mm subhorizontal veins of talc-rich material. Inclined veins are dominantly filled by calcite; in some cases with slip striae and pyrite crystals. Section 647A-72R-2 Phenocrysts: pyroxene less than 1% at 1 mm thickness. Fracturing: SV1,14 1a-8-16 cm; multiple highly fractured veins with different greenish minerals and quartz and pyrite. N G105 0647A072R010100002 72R-3, 10 cm to 72R-4, 25 cm. KUE FINE-GRAINED, SPARSELY PHYRIC, BASALT. n/a Pyroxene 2 0.5-2 mm n/a (2.5Y N5) gray. n/a n/a n/a V = 0; 19; H1; 2 are filled with calcite (0.5 mm). N G105 0647A072R040250003 4 KUE FINE-MEDIUM-GRAINED MODERATE PHYRIC BASALT. n/a Pyroxene < 10 n/a n/a (2.5Y N5)gray. n/a n/a n/a H = 0; I = 7; V = 0. N G105 0647A072R041130004 4 KUE FINE-GRAINED, SPARSELY PHYRIC, BASALT. n/a Pyroxene 2 0.5-2 mm n/a n/a n/a n/a n/a n/a N G105 0647A073R010000001 73R-1, 0 cm to 73R-6, 54 cm. KUE MEDIUM-GRAINED, SPARSELY PYROXENE-PHYRIC MASSIVE BASALT. see comments Pyroxene Pyroxene Pyroxene 2 1 2 0.5-1.5 mm 0.5-1.5 mm 1 mm Section 73R-3; 1a, 31 cm concentrated band of phenocrysts Section 73R-5 see comments Gray Absent. Section 73R-3: Rare irregular vesicles filled with phyllosilicates and calcite. see comments see comments Numerous fine, irregular, inclined, fractures. Section 73R-2: Numerous irregular fine fractures mostly inclined to subhorizontal. 1a, 24 cm: 0.5 cm thick fracture (subhorizontal) filled with greenish minerals, possibly chlorite. 42 cm, calcite filled fracture between 1b and 1c. Sectio 73R-3: I=4. 1b, 48 cm, calcite filled, 1 mm thick fracture, horizontal to inclined. Section 73R-4: SH=3, one vertical fracture in Piece 2a and 2b on top filled with calcite. "See main comments" Section 73R-5: Some horizontal fine fractures; one large vertical fracture from 0-60 cm. N G105 0647A073R060540002 73R-6, 54 cm to 73R-8, 34 cm. KUE MEDIUM-GRAINED, MODERATELY PYROXENE PHYRIC, MASSIVE BASALT. n/a Pyroxene Pyroxene Pyroxene 5 3-5 7 1-2 mm 1-2 mm 1-2 mm Section 73R-7 Section 73R-8 n/a Gray. n/a n/a n/a Some fine subhorizontal,irregular fractures.Section 73R-7: Some fine irregular subhorizontal fractures 1b.one irregular inclined fracture.Section 73R-8:Calcite filled fracture (vertical) at the bottom from 33-150 cm;and CC, 0-11 cm (vertical).Drilling breccia containing different pebble-sized sediment fragments from younger lithologies above (cavings).Smear slides show nannofossils from the middle Eocene,which are younger than the oldest ages from the sediment directly above the basement contact N G105 0647A074R010000001 74R-1, 0 cm to 74R-8, 26 cm. KUE MEDIUM GRAINED, MODERATELY PYROXENE-PHYRIC, MASSIVE BASALT. see comments Pyroxene Plagioclase? 5 n/a 1 mm Small Fresh; Occur in black matrix as well as in the gray pockets Pockets of very light irregular crystals in a very fine black matrix No vesicles. H=9; SB=3; V=7. Most veins (9) less than 1 mm; (2) ca 3 mm thick. The vein material is pyrite (abundant) calcite (very rare) and greenish phyllosilicates. Probably chlorite and/or serpentine (dominant). see comments see comments Section 74R-2: pyrite(abundant), calcite(very rare), phyllosilicates(dominant), probably chlorite and serpentine. Isolated grains of pyrite, some millimeters in diameter mm in thick veins. In thin veins, pyrite may be the dominant secondary mineral. Section 74R-3 Horizontal fractures and veins 15) 9>1 mm. Subhorizontal fractures and veins 5) 11<1 mm. Two of the latter complex with smaller "apophyses". One vertical vein <1 mm. Vein material see comments. see comments see comments Dominant: chlorite and serpentine. Abundant: pyrite a) as few mm grains in thick veins. b) dominant in some smaller veins. Section 74R-4: H=21; SH=2. Two of the latter complex with smaller "apophyses". Chlorite and serpentine dominant in veins. Pyrite often concentrated in few mm grains in bigger veins. Fractures are produced by drilling and are almost entirely located in veins. Rest see comment. Section 74R-5: H=17; SH=12. Section 74R-6: H=30; SH=4. Section 74R-7: H=15; SH=3. Section 74R-8: Two horizontal veins of chlorite/serpentine. One vertical vein of chlorite/serpentine. 26-81 cm: drill, gravel and slurry cavings from younger sediments. Drill, gravel and slurry cavings: 74R-9, 0-26 cm. N G105 0647A075R040000001 1 KUE FINELY CRYSTALLINE, GRAY, APHYRIC BASALT. see comments see comments see comments see comments see comments see comments see comments see comments Aphyric basalt with 0.5 cm clots of dark green mineral (possibly ophitic pyroxene). No alteration, fractures, vesicles, etc. N G105 0647A075R040100002 75R-4, 10 cm to 75R,CC, 19 cm.KUE MEDIUM CRYSTALLINE, GRAY, MASSIVE BASALT. see comments Pyroxene? 20 < 1 mm Dark crystals (possibly pyroxene) see comments see comments see comments see comments see comments < 1 mm in thickness Horizontal to subhorizontal n/a Rock is cut by veins, and filled with soft, dark green, non-fibrous mineral (possibly Antigorite). To microgabbro with no preferred fabric nor outsized phenocrysts. 647A-75R, CC: Drill cuttings and one large piece of medium crystalline basalt - microgabbro as in Section 4. N