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Core Data from the Deep Sea Drilling Project


Leg : 28    Top/Bottom Interval(mm): 1170/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   168.00   Rock Type: IGNEOUS
Core:  11   Sample Midpoint(m)     :   170.67   Sect/Pc #:  2/

ROCK = GABBRO
       ALBITIZED,ALTERED;
       Texture: COARSE-GRAINED
       OCCURRENCE UNKNOWN,ROCK UNUSUALLY COARSE-GRAINED
       AND APPARENTLY PLUTONIC OR HYPABYSSAL RATHER THAN
       VOLCANIC,MAY BE PART OF A LARGE FOREIGN BOULDER,
       BUT COULD BE AN ALTERED INTRUSIVE ASSOCIATED WITH
       THE VOLCANIC FRAGMENTAL ROCKS,ALSO COULD BE A
       PLAG-RICH XTL ACCUMULATE IN A FLOW ROCK,BUT
       TEXTURES NOT INDICATIVE OF A CUMULATE ORIGIN*

Groundmass - PLAGIOCLASE               (   75%)
             MOSTLY MEDIUM GRAINED BUT WITH A FEW COARSE GRAINS
             (EXTINCTION ANGLE PERPENDICULAR TO A-AXIS = 25
             DEGREES,APPROX COMP AN43),MOST MEDIUM GRAINED XTLS
             ARE HIGHLY ALTERED-NOW ALBITE/OLIGOCLASE(I.R. >
             1.54),STRONGLY SAUSSURITIZED*

Alteration - ALBITE
             Replacing: PLAG
             ALBITE/OLIGOCLASE;

             FERROUS OXIDE
             Replacing: MAFICS,OPAQUES
             SECONDARY FE-OXIDES;

             CHLORITE
             Replacing: MAFICS,OPAQUES
             BROWNISH MICACEOUS/CHLORITIC MATERIAL*




Leg : 28    Top/Bottom Interval(mm): 1400/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   168.00   Rock Type: IGNEOUS
Core:  11   Sample Midpoint(m)     :   170.90   Sect/Pc #:  2/

ROCK = ANDESITIC VITROPHYRE
       ALTERED;
       Texture: SPARSELY PHYRIC,CRYPTOXTLLINE
       NO ALBITIZATION OR FLOW TEXTURE*

Phenocrysts- PLAGIOCLASE               (    2%)
             Size(mm):          1
             APPROX COMP AN32,EXTINCTION ANGLE PERPENDICULAR TO
             X-AXIS = 27,26 DEGREES*

Groundmass - FERROMAGNESIUM
             LIGHT BROWN SEMI-OPAQUE;

             OPAQUE MINERAL
             Size(mm):      .1-.3  Morphology: NEEDLES
             SCATTERED,MORE OPAQUE THAN FE-MAGN;

             ALTERED GLASS




Leg : 28    Top/Bottom Interval(mm): 1420/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   168.00   Rock Type: SEDIMENTARY
Core:  11   Sample Midpoint(m)     :   170.92   Sect/Pc #:  2/

ROCK = BASALT CONGLOMERATE
       CALCITE CEMENTED;
       Texture: FINE-GRAINED,EQUIGRANULAR,INTERSERTAL*

Groundmass - ALTERED GLASS
             Size(mm):        3-5
             PEBBLES OF SEMI-OPAQUE HEMATITE ALTERED GLASS WITH
             SCATTERED RANDOMLY ORIENTED MICROLITES OF VARYING
             DENSITY;

             BASALT
             PEBBLE SEVERAL CM LONG OF ALTERED BASALT;

             PLAGIOCLASE               (   60%)
             SIMPLE ZONING COMMON,EXTINCTION ANGLE PERP. TO
             X-AXIS = 19 DEGREES-APPROX COMP AN37,MAX.EXTINCT.
             ANGLE 29-27DEG-APPROX COMP AN54;

             FERROMAGNESIUM
             CRYPTOXTLLINE,PEBBLES ENCLOSED IN A .1MM THICK
             FILM OF CALCITE WHICH ALSO CEMENTS THE CONGLOM.,
             MATRIX IS CLEAN COARSE SAND*

Alteration - CALCITE
             Location: CEMENT




Leg : 28    Top/Bottom Interval(mm):    0/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   168.00   Rock Type: IGNEOUS
Core:  11   Sample Midpoint(m)     :   171.10   Sect/Pc #: CC/

ROCK = BASALT
       ALTERED, XTL-RICH;

Groundmass - PLAGIOCLASE               (   80%)
             EXTINCTION ANGLE PERP. TO A-AXIS = 30 DEG.,APPROX
             COMP AN60,2 GRAINS EXTINCT AT 35 DEG. WITH APPROX
             COMP AN65, NORMAL ZONING TO APPROX AN40-50 COMMON
             (LABRADORITE TO ANDESINE),UNUSUALLY FRESH(NON-
             ALBITIZED);

Alteration - CHLORITE                  (   20%)
             Replacing: MAFICS
             CHLORITE+FE-OXIDES*




Leg : 28    Top/Bottom Interval(mm):    1/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   187.00   Sect/Pc #:  1/

ROCK = ANDESITIC VITROPHYRE
       ALTERED,SECTION 1;
       Texture: GLASSY,VITROCLASTIC,PERLITIC*

Phenocrysts- PLAGIOCLASE               (    2%)
             APPROX COMP AN30-35,R.I.>ALBITE,EXTINCTION ANGLE
             PERP. TO X-AXIS = 17+16+13+13 DEGREES(4 DIFFERENT
             MEASUREMENTS)*

Groundmass - GLASS
             FERRO-BANDED GLASS SHOWING INCIPIENT
             DEVITRIFICATION,WITH PATCHES OF PALE GREEN
             CHLORITE,BANDING ENHANCED BY CRYPTOXTLLINE BROWN
             FERRUGINOUS STUFF,GLASS AROUND PHENOS IS REALLY
             HIGHLY DISTURBED AND DEFINES "PACKETS" OF GLASS
             THAT WERE COHERENT IN A FLOWING GLASSY MEDIUM,ALSO
             PATCHES OF GLASS FRAGMENTS-VITROCLASTIC,WELL
             DEVELOPED CONCENTRIC LINES IN SETS,UP TO 1MM
             ACROSS,PICKED OUT BY OPAQUE MATERIAL(PERLITIC
             TEXTURES),SOME PERLITIC AREAS REPLACED BY QUARTZ
             WITH DIAMETER APPROX .02MM ACROSS GENERALLY
             FOLLOWING THE FRACTURE PATTERN BUT IN PLACES
             CROSSING IT*

Alteration - CHLORITE
             Replacing: GLASS
             PALE GREEN,THIS IS SECTION 1*




Leg : 28    Top/Bottom Interval(mm):    2/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   187.00   Sect/Pc #:  1/

ROCK = PLAG SPARSELY PHYRIC BASALT
       ALTERED,FINE-GRAINED,SECTION 2;
       Texture: SPARSELY PHYRIC*

Phenocrysts- PLAGIOCLASE               (    1%)
             Size(mm):        1-3  Morphology: EUHEDRAL PRISMATIC
             R.I.<ALBITE*

Groundmass - PLAGIOCLASE
             Size(mm):     .05-.2  Morphology: MICROLITES
             ALTERED WITH SMALL PATCHES OF PALE GREEN CHLORITE
             +SCATTERED SPECKS .05MM ACROSS OF HEMATITE*

Alteration - CHLORITE                  (   TR%)
             Replacing: OL
             EUHEDRAL-SUBHEDRAL,1MM LONG,BOWLINGITE?,PALE
             GREEN*

Vesicles   -
             Size(mm):      1-4
             Percent:    .5
             Location: PATCHES
             Filling: CHALCEDONY
             AMYGDULES OF CHALCEDONY WITH FINGERS EXTENDING
             IN FROM THE MARGIN,THIS IS SECTION 2*




Leg : 28    Top/Bottom Interval(mm):    3/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   187.00   Sect/Pc #:  1/

ROCK = DACITIC VITROPHYRE
       ALTERED,ALBITIZED,SECTION 4;
       Texture: PHYRIC*

Phenocrysts- PLAGIOCLASE               (   10%)
             PHENOS RESORBED AND ARE GLOMEROPHYRIC,APPROX COMP
             ALBITE/OLIGOCLASE(R.I.=1.54)*

Groundmass - QUARTZ                    (    5%)
             GLASS ENTIRELY DEVITRIFIED TO QUARTZ+ALKALI
             FELDSPAR,PROBABLY ALBITE,+CHLORITE+FE-OXIDES,ALL
             IN HIGHLY IRREGULAR MASSES,RELICT PERLITIC(?)
             STRUCTURES LOCALLY PRESENT*

Alteration - CHLORITE
             Replacing: GLASS

             FERROUS OXIDE
             Replacing: GLASS




Leg : 28    Top/Bottom Interval(mm):    4/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   187.00   Sect/Pc #:  1/

ROCK = PLAG MODERATELY PHYRIC BASALT
       ALTERED,ALBITIZED,SECTION 5;
       Texture: MODERATELY PHYRIC,VESICULAR*

Phenocrysts- PLAGIOCLASE               (    5%)
             Morphology: SUBHEDRAL
             PATCHY ZONING,RARE CHLORITIC PSEUDOMORPHS AFTER
             ORIGINAL MAFIC PHENOS*

Groundmass - PLAGIOCLASE
             PLAG MICROLITE-BEARING CHLORITIC DENSE MATRIX THAT
             MAY BE IN PART A DEVITRIFIED GLASS,PLAG APPEARS
             TO BE ALBITE-OLIGOCLASE(I.R.>1.54);

             QUARTZ
             MINOR,MOSTLY IN FINE AGGREGATES THAT APPEAR TO
             FILL VESICLES*

Alteration - CHLORITE
             Location: VESICLES,      Replacing: MAFICS
             Location: MATRIX

             CHALCEDONY
             Location: VESICLES
             CHALCEDONY/OPAL*

Vesicles   -
             Filling: CHLORITE,

             Filling: CHALCEDONY
             INTERLAYERED FILLING,SECTION 5*




Leg : 28    Top/Bottom Interval(mm):    5/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   187.01   Sect/Pc #:  1/

ROCK = ANDESITIC VITROPHYRE
       SILICIFIED,SECTION 6;
       Texture: MODERATELY PHYRIC,SPHERULITIC*

Phenocrysts- PLAGIOCLASE               (    5%)
             Size(mm):        1-3
             I.R.>ALBITE,EXTINCTION ANGLE PERP. TO 010 = 16DEG.
             APPROX COMP AN32*

Groundmass - QUARTZ                    (   70%)
             Size(mm):    .02-.05
             OCCURS IN PLACES ORGANIZED AS SPHERULITES .2-.3MM;

             PLAGIOCLASE               (   25%)
             Size(mm):     .02-.1  Morphology: LATHS
             EXTINCTION ANGLE = 16 DEG.,APPROX COMP AN32;

             OPAQUE MINERALS           (    2%)
             Size(mm):       .005
             FILLING AREAS BETWEEN SPHERULITES OR AS SCATTERED
             SPECKS-HEMATITE?,PHYRIC NATURE+SPHERULITES
             INDICATE SILICIFICATION OF GLASS*




Leg : 28    Top/Bottom Interval(mm):    1/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.50   Sect/Pc #: CC/

ROCK = BASALT
       ALTERED,SECTION 1;
       Texture: FINE-GRAINED,INTERSERTAL*

Groundmass - PLAGIOCLASE               (   40%)
             Size(mm):     .05-.1  Morphology: MICROLITES+LATHS
             I.R.>ALBITE,MAX.EXTINCTION ANGLE = 2DEG.,APPROX
             COMP AN20(OLIGOCLASE);

             ORTHOPYROXENE             (   20%)
             ALTERED TO CHLORITE;

             QUARTZ                    (   35%)
             Size(mm):        .02
             QUARTZ+ZEOLITE,ENCLOSED BY PLAG;

             OPAQUE MINERALS
             Morphology: EQUANT
             INCLUDES HEMATITE*

Alteration - CHLORITE
             Replacing: OPX

Vesicles   -
             Size(mm):       .3
             Filling: CHLORITE
             QUARTZ LINED AMYGDULE SHOWING TWO GENERATIONS OF
             CHLORITE FILLING*




Leg : 28    Top/Bottom Interval(mm):    2/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.50   Sect/Pc #: CC/

ROCK = BASALTIC VITROPHYRE
       ALBITIZED,DEVITRIFIED,SECTION 2;
       Texture: PHYRIC*

Phenocrysts- PLAGIOCLASE               (   20%)
             Morphology: SUBHEDRAL
             LITTLE ZONING-PATCHY TYPE IN ALTERED XTLS,EXTINCT.
             ANGLE PERP. TO A-AXIS = 18DEG.,APPROX COMP AN35-
             OTHERS ARE ALBITE-OLIGOCLASE ON BASIS OF I.R. =
             1.54;

             MAFIC                     (   10%)
             CHLORITIC PSEUDOMORPHS AFTER ORIGINAL MAFIC
             MINERAL-CANNOT TELL PRIMARY MINERAL;

             FERROUS OXIDE             (    5%)
             SOME MAY BE PRIMARY BUT MOST APPEAR SECONDARY*

Groundmass - MATRIX
             DEVITRIFIED GLASSY MATRIX,SUGGESTIONS OF PERLITIC
             STRUCTURE LOCALLY PRESENT,ORIGINAL ROCK MAY HAVE
             BEEN ANDESITIC BUT HERE TENTATIVELY INFERRED TO
             HAVE BEEN BASALTIC-NEED CHEMICAL ANALYSIS*

Alteration - CHLORITE
             Replacing: MAFICS




Leg : 28    Top/Bottom Interval(mm):    3/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.50   Sect/Pc #: CC/

ROCK = PLAG MODERATELY PHYRIC BASALT
       ALBITIZED,SECTION 3;
       Texture: MODERATELY PHYRIC,FINE-GRAINED,SPILITIC*

Phenocrysts- PLAGIOCLASE               (    5%)
             Size(mm):          4
             TWO TYPES-I.R.<ALBITE AND >ALBITE,EXTINCTION ANGLE
             =31-40DEG.,APPROX COMP ALBITE-LABRADORITE-APPROX
             HALF ARE ALBITE*

Groundmass - PLAGIOCLASE               (   30%)
             Size(mm):     .05-.1  Morphology: MICROLITES
             MAX.EXT.ANGLE = 23DEG.,APPROX COMP AN50;

             CLINOPYROXENE             (   TR%)

             MATRIX                    (   60%)
             DENSE CRYPTOXTLLINE GROUNDMASS BETWEEN MICROLITES,
             MICROLITES AND PHENOS SHOW SOME FLOW ALIGNMENT*

Alteration - CHLORITE
             Replacing: MAFICS
             ELONGATE PRISMATIC REPLACE PYX,LOZENGE SHAPED
             REPLACE OL*

Vesicles   -
             Percent:     0




Leg : 28    Top/Bottom Interval(mm):    4/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.50   Sect/Pc #: CC/

ROCK = BASALT
       ALTERED,SECTION 4;
       Texture: FINE-GRAINED,INTERSERTAL,EQUIGRANULAR*

Groundmass - PLAGIOCLASE
             Size(mm):     .02-.3  Morphology: LATHS
             CLOUDY WITH PATCHY EXTINCTION,I.R.>ALBITE BUT MANY
             MICROXTLLINE PATCHES WITH I.R.<ALBITE,ALBITE?;

             QUARTZ                    (    5%)
             Size(mm):      .1-.3
             RELATIONSHIP TO OTHER GRAINS UNCLEAR*

Alteration - HEMATITE
             Location: INTERSTITIAL

             CHLORITE
             Location: INTERSTITIAL
             GREEN*




Leg : 28    Top/Bottom Interval(mm):    5/   0  Describer: Barrett, P.J.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.51   Sect/Pc #: CC/

ROCK = ANDESITIC VOLCANIC GLASS VITROPHYRE
       FERRUGINOUS ZEOLITIZED,SECTION 6;
       Texture: FELTY*

Phenocrysts- PLAGIOCLASE               (    2%)
             Size(mm):          1  Morphology: EQUANT EUHEDRAL+ROUNDED+

             Morphology: ELONGATE
             I.R.>ALBITE+ALSO<ALBITE,OLIGOCLASE*

Groundmass - OPAQUE MINERALS           (   98%)
             Morphology: LATHS
             SEMI-OPAQUE FERRUGINOUS GROUNDMASS I.R. SLIGHTLY
             <ALBITE,ZEOLITE?,GROUNDMASS HAS FELTY TEXTURE
             INDICATED BY OPAQUE LATHS RATHER THAN PLAG*

Alteration - CHLORITE                  (   TR%)
             PASTEL GREEN*




Leg : 28    Top/Bottom Interval(mm):    6/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   187.00   Rock Type: IGNEOUS
Core:  13   Sample Midpoint(m)     :   188.51   Sect/Pc #: CC/

ROCK = BASALT
       ALTERED,ALBITIZED;SECTION 7;
       Texture: SPILITIC,INTERGRANULAR*

Groundmass - PLAGIOCLASE               (   70%)
             Morphology: LATHS
             PATCHY ZONING,HIGHLY ALTERED AND ALBITIZED,FEW
             SECONDARY CA MINERALS PRESENT + CALCITE AND
             EPIDOTE,ROCK APPEARS TO HAVE BEEN ORIGINALLY
             HOLOXTLLINE AND WITH INTERGRANULAR TEXTURE*

Alteration - OTHERS                    (   30%)
             Replacing: MAFICS
             SECONDARY MAFICS-CHLORITE AND GREENISH-BROWN
             MICACEOUS MINERAL(?)+FE-OXIDES(HEMATITE/GOETHITE,
             LIMONITE,ETC.)*

Vesicles   -
             Filling: QUARTZ
             QUARTZ LOCALLY CONCENTRATED IN WHAT APPEAR TO BE
             VESICLE FILLINGS*




Leg : 28    Top/Bottom Interval(mm):    0/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   196.50   Rock Type: SEDIMENTARY
Core:  14   Sample Midpoint(m)     :   196.60   Sect/Pc #: CC/

ROCK = VOLCANIC CONGLOMERATE
       ALTERED;
       Texture: TUFFACEOUS*
             CONGLOMERATE COMPOSED OF PEBBLES/COBBLES OF MOSTLY
             DEVITRIFIED VITROPHYRE IN AN ALTERED TUFFACEOUS
             MATRIX CONTAINING ABUNDANT CARBONATE AND ALBITE
             AND SEVERAL VARIOLITIC-LIKE MASSES OF CHLORITE*




Leg : 28    Top/Bottom Interval(mm):    0/   0  Describer: Ford, A.
Hole: 264   Top of Core Depth(m)   :   206.00   Rock Type: IGNEOUS
Core:  15   Sample Midpoint(m)     :   206.10   Sect/Pc #: CC/

ROCK = SPILITIC BASALT
       ALTERED;
       Texture: FINE-GRAINED,HOLOXTLLINE,APHYRIC*
             FINE LATHS OF PLAG,ALBITE AND OLIGOCLASE(I.R.>
             CEMENT),INTERSTICES OF WHICH FILLED BY QUARTZ,
             FE-OXIDES,CHLORITE AND EPIDOTE OR PUMPELLYITE,
             GIVE A TEXTURE THAT APPEARS TO BE A RELICT
             INTERGRANULAR TEXTURE.IN A FEW LARGER GRAINS THE
             SODIC PLAG APPEARS TO HAVE REPLACED MORE CALCIC
             ONES*

Vesicles   -
             Filling: QUARTZ,CHALC
             Shape: SPHERULITIC
             AMYGDULES OF QUARTZ AND CHALCEDONY*




    

Introduction


Cite as: Deep Sea Drilling Project (1989): Archive of Core and Site/Hole Data and Photographs from the Deep Sea Drilling Project (DSDP). National Geophysical Data Center, NOAA. doi:10.7289/V54M92G2 [access date]

These Web pages are from the Core Data from the Deep Sea Drilling Project Legs 1-96 CD-ROM produced in 1989 and modified in 2000 by the U.S. Department of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Geophysical Data Center (now part of the National Centers for Environmental Information), and collocated World Data Center for Marine Geology and Geophysics, Boulder (now part of the World Data Service for Geophysics). Data were compiled in cooperation with the U.S. Science Support Program, of the Joint Oceanographic Institutions, Inc. (now the Consortium for Ocean Leadership), and the U.S. National Science Foundation.

Please see NOAA's privacy and disclaimer information. Send questions or comments to mgg.info@noaa.gov.

Department of Commerce > NOAA > NESDIS > NCEI > doi:10.7289/V54M92G2