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Core Data from the Deep Sea Drilling Project


Leg : 26    Top/Bottom Interval(mm):  840/ 850  Describer: Kempe, D.
Hole: 253   Top of Core Depth(m)   :   218.00   Rock Type: IGNEOUS
Core:  24   Sample Midpoint(m)     :   218.85   Sect/Pc #:  1/

ROCK = BASALT
       FAIRLY ALTERED;
       Texture: SCORIACEOUS,GLASSY*

Groundmass - OLIVINE
             Size(mm):       .6-2
             COMMON,FRESH IN GLASS;

             PLAGIOCLASE
             Size(mm):         .8




Leg : 26    Top/Bottom Interval(mm):  930/   0  Describer: DSDP microfilm
Hole: 253   Top of Core Depth(m)   :   218.00   Rock Type: IGNEOUS
Core:  24   Sample Midpoint(m)     :   218.93   Sect/Pc #:  1/

ROCK = BASALT GLASS;
       Texture: GLASSY*

Phenocrysts- PLAGIOCLASE               (   10%)
             Size(mm):     TO 0.8  Morphology: LATHS
             POORLY TWINNED, SCATTERED THRU DK BROWN
             PALAG WHICH FORMS BULK OF ROCK;

             OLIVINE                   (    8%)
             Size(mm):        0.6
             MANY WELL-SHAPED, ALTERED TOTALLY TO IDDINGS
             AGGREGATE*

Alteration - IDDINGSITE
             Replacing: OL

             PALAGONITE                (   82%)

Vesicles   -
             Filling: PALAG
             PALAG RIMS INSIDE OF VESICLES*




Leg : 26    Top/Bottom Interval(mm): 1090/   0  Describer: DSDP microfilm
Hole: 253   Top of Core Depth(m)   :   218.00   Rock Type: IGNEOUS
Core:  24   Sample Midpoint(m)     :   219.09   Sect/Pc #:  1/

ROCK = BASALT GLASS
       IN CONTACT WITH ASH BELOW;
       Texture: GLASSY, SCORIACEOUS*

Phenocrysts- PLAGIOCLASE               (   23%)
             Size(mm):      TO 1.  Morphology: LATHS
             CLEAR LATHS,ALSO PRISMATIC AND RHOMBOID
             XTLS OF THE FELDSPAR, LATHS ARE TWINNED,
             FREQUENTLY ZONED;
             ALTHOUGH NOT USUALLY ON THE ALBITE LAW,

             OLIVINE                   (    1%)
             Size(mm):     1.5-2.  Morphology: EUHEDRAL
             USUALLY FRESH,SOMETIMES EUHEDRAL*

Groundmass - GLASS                     (   30%)
             FRESH AND ALMOST COLORLESS,R.I. WELL ABOVE
             BALSAM,REMAINDER ALTERED TO PALAG WITH LOW R.I.*

Alteration - PALAGONITE                (   40%)
             DARK,REDDISH-BROWN,LOW R.I.,CONTAINS ROUND AND
             IRREGULAR-SHAPED CAVITIES FILLED WITH A
             SPHERULITIC,FIBROUS ZEOL AND OCCASIONALLY
             CALCITE,WITHIN PALAG THE FELDSPARS ARE ALSO
             HIGHLY ALTERED  OR RESORBED*

             COMBINATION               (    6%)
             INCLUDES ZEOLITE + CALCITE,FIBROUS ZEOLITE (LENGTH
             SLOW IN ORIENTATION)*




Leg : 26    Top/Bottom Interval(mm):   20/  70  Describer: Kempe, D.
Hole: 253   Top of Core Depth(m)   :   558.00   Rock Type: IGNEOUS
Core:  58   Sample Midpoint(m)     :   558.05   Sect/Pc #:  1/

ROCK = BASALT
       ALTERED;
       Texture: GLASSY TO SUBVARIOLITIC,PORPHYRITIC*

Groundmass - OLIVINE
             Size(mm):        1.0
             ALTERED,VERY COMMON;

             PLAGIOCLASE
             Size(mm):     .2-1.8

Alteration - TALC
             Location: PSEUDOMORPHS   Replacing: OL

             SERPENTINITE
             Location: PSEUDOMORPHS   Replacing: OL




Leg : 26    Top/Bottom Interval(mm):   80/   0  Describer: DSDP microfilm
Hole: 253   Top of Core Depth(m)   :   558.00   Rock Type: IGNEOUS
Core:  58   Sample Midpoint(m)     :   558.08   Sect/Pc #:  1/

ROCK = PLAG-OL PHYRIC BASALT
       FRESH;
       Texture: FINE-GRAINED,OL-RICH,PHYRIC*

Phenocrysts- PLAGIOCLASE               (   20%)
             Size(mm):     TO 1.8  Morphology: LATHS
             NORMALLY 0.1 -0.2, AMOUNT IS ALL
             PLAG IN SECTION;

             OLIVINE                   (   15%)
             Size(mm):    0.5-1.0  Morphology: EUHEDRAL
             TOTALLY ALTERED TO TALC AND COLORLESS
             FIBROUS CHRYSOTILE SERPENTINE,PATCHES OF
             GREEN ALTERATION MATERIAL WHICH MAY BE
             BOWLINGITE , AND SKELETAL ILMENITE RODS
             UP TO 0.3MM OCCUR WITHIN THE OLIVINES,
             OL SOMETIMES ACCOMPANIED BY TINY,VERY
             EUHEDRAL BROWN XTLS OF PROBABLY DIPYRAMIDAL
             ANATASE,SOME OF OL SHOW ALTERATION BEYOND
             EUHEDRAL OUTLINES OF THE XTLS INTO THE
             SURROUNDING MATRIX*

Groundmass - FERROUS OXIDE             (    6%)
             Morphology: GRAINS,RODS

             OTHER
             OCCASIONAL DISCRETE XTLS OF A REDDISH-
             BROWN IRON-RICH MINERAL PRESENT;

             GLASS                     (   59%)
             MATRIX IS SUBVARIOLITIC CONTAINS PYX,FELD,
             FE ORE AND PROBABLY SOME GLASS;

             PYROXENE

             ILMENITE
             Size(mm):     TO 0.3  Morphology: SKELETAL,RODS

             ANATASE
             Morphology: EUHEDRAL,DIPYRAMIDAL
             PROBABLY ANATASE*

Alteration - TALC
             Replacing: OL

             SERPENTINITE
             Replacing: OL
             COLORLESS FIBROUS CHRYSOTILE;

             BOWLINGITE
             Replacing: OL
             ID UNCERTAIN,GREEN*




    

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.

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