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Expedition 313 Scientists (2010): Description of thin sections of Hole 313-M0027A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761537

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Related to:
Mountain, Gregory S; Proust, Jean-Noël; McInroy, Dave; Cotterill, Carol; Expedition 313 Scientists (2010): Proceedings of the Integrated Ocean Drilling Program. Tokyo (Integrated Ocean Drilling Program Management International, Inc.), 313, 885 pp, https://doi.org/10.2204/iodp.proc.313.2010
Coverage:
Latitude: 39.634101 * Longitude: -73.621691
Date/Time Start: 2009-05-01T19:00:00 * Date/Time End: 2009-05-01T19:00:00
Minimum DEPTH, sediment/rock: 353.92 m * Maximum DEPTH, sediment/rock: 489.77 m
Event(s):
313-M0027A (MAT-1A) * Latitude: 39.634101 * Longitude: -73.621691 * Date/Time: 2009-05-01T19:00:00 * Elevation: -33.5 m * IGSN: IBCR0313RHOV001 * Penetration: 631.01 m * Recovery: 471.59 m * Location: New Jersey Shallow Shelf * Campaign: Exp313 (New Jersey Shallow Shelf) * Basis: Kayd * Comment: Drilling Depth Method (DRF): measured by pipe; Drilling Depth Method (DSF): tag sea floor; Core Depth Method (CSF): let overlap if long; Core Depth Method (CCSF): let overlap if long
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelExpedition 313 Scientists
Thin sectionThin sec#Expedition 313 Scientists
DEPTH, sediment/rockDepth sedmGeocode
Lithology/composition/faciesLithologyExpedition 313 ScientistsVisual description
Lithology/composition/faciesLithologyExpedition 313 ScientistsVisual descriptioncontinuation 1
Lithology/composition/faciesLithologyExpedition 313 ScientistsVisual descriptioncontinuation 2
File nameFile nameExpedition 313 ScientistsTSB photo
Uniform resource locator/link to imageURL imageExpedition 313 Scientistslink to TSB photo
Size:
92 data points

Data

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


Sample label

Thin sec [#]

Depth sed [m]

Lithology

Lithology
(continuation 1)

Lithology
(continuation 2)

File name
(TSB photo)

URL image
(link to TSB photo)
313-M0027A-124R-1,46-521353.92Slide to aid core description for Unit 1. Medium to coarse glauconite-bearing sandstone. Grains of quartz, feldspar, and rock fragments (granitoids) show subangular to rounded shape. Apatite and zircon are also found as accessory minerals. Glauconitepellet (green) is dominant mineral formed by authigenic diagenesis. Flocks of magnetic grains are associated along glauconite boundaries. Significantly altered calcite cement is common.313-M0027A-124R-1_46-52cm_TSB_250034_photo313-M0027A-124R-1_46-52cm_TSB_250034_photo.tif
313-M0027A-124R-1,46-521353.92313-M0027A-124R-1_46-52cm_TSB_250035_photo313-M0027A-124R-1_46-52cm_TSB_250035_photo.tif
313-M0027A-124R-1,46-521353.92313-M0027A-124R-1_46-52cm_TSB_250036_photo313-M0027A-124R-1_46-52cm_TSB_250036_photo.tif
313-M0027A-124R-1,46-521353.92313-M0027A-124R-1_46-52cm_TSB_250037_photo313-M0027A-124R-1_46-52cm_TSB_250037_photo.tif
313-M0027A-125R-1,139-1431355.52Slide to aid core description for Unit I. Medium grained sandstone. Grains with subangular to subrounded shapes mostlyconsist of quartz and associated feldspar (perthite, microcline, and plagioclase), rock fragments (granitoids, gneiss, and marble),magnetic grains, zircon, and chlorite. Matrix is filled with clay and organic materials and is partly recrystallized by calcite cement.313-M0027A-125R-1_135-143cm_TSB_250038_photo313-M0027A-125R-1_135-143cm_TSB_250038_photo.tif
313-M0027A-125R-1,139-1431355.52313-M0027A-125R-1_135-143cm_TSB_250039_photo313-M0027A-125R-1_135-143cm_TSB_250039_photo.tif
313-M0027A-125R-1,139-1431355.52313-M0027A-125R-1_135-143cm_TSB_250040_photo313-M0027A-125R-1_135-143cm_TSB_250040_photo.tif
313-M0027A-125R-1,139-1431355.52313-M0027A-125R-1_135-143cm_TSB_250041_photo313-M0027A-125R-1_135-143cm_TSB_250041_photo.tif
313-M0027A-125R-CC,0-41355.60Slide to aid core description for Unit I. Medium sandstone. Grains are composed mainly of monocrystalline quartz and subordinantly of feldspar (microcline, plagioclase, and perthite), rock fragments (granitoids, schist/gneiss, quartzite, and marble),zircon, muscovite, authigenic glauconite, and fossils (radiolarians, shell, etc.). Some grains are coated by microcrystalline calcite. Matrix is filled with argillaceous mud and clay, organic materials, and opaque minerals. Calcite in matrix ispartly recrystallized.313-M0027A-125R-CC_4cm_TSB_250030_photo313-M0027A-125R-CC_4cm_TSB_250030_photo.tif
313-M0027A-125R-CC,0-41355.60313-M0027A-125R-CC_4cm_TSB_250031_photo313-M0027A-125R-CC_4cm_TSB_250031_photo.tif
313-M0027A-125R-CC,0-41355.60313-M0027A-125R-CC_4cm_TSB_250032_photo313-M0027A-125R-CC_4cm_TSB_250032_photo.tif
313-M0027A-125R-CC,0-41355.60313-M0027A-125R-CC_4cm_TSB_250033_photo313-M0027A-125R-CC_4cm_TSB_250033_photo.tif
313-M0027A-127R-2,3-71361.09Slide to aid core description for Unit I. Fine sandstone. Matrix consists of mud and silt material, unidentified clay mineral flakes, and organic/nonorganic materials. Flakes of chlorite and sericite in matrix are commonly layered. Brown pelletsoccasionally observed in matrix are considered to be oxidized glauconite formed by diagenesis. Detrital grains are quartz, feldspar, opaque mineral, muscovite, zircon, and fossil carbonate fragments.313-M0027A-127R-2_3-7cm_TSB_250042_photo313-M0027A-127R-2_3-7cm_TSB_250042_photo.tif
313-M0027A-127R-2,3-71361.09313-M0027A-127R-2_3-7cm_TSB_250043_photo313-M0027A-127R-2_3-7cm_TSB_250043_photo.tif
313-M0027A-127R-2,3-71361.09313-M0027A-127R-2_3-7cm_TSB_250044_photo313-M0027A-127R-2_3-7cm_TSB_250044_photo.tif
313-M0027A-127R-2,3-71361.09313-M0027A-127R-2_3-7cm_TSB_250045_photo313-M0027A-127R-2_3-7cm_TSB_250045_photo.tif
313-M0027A-171R-1,38-421489.77Slide to aid core description for Unit II. Quartzose glauconite-bearing medium sandstone. Detrital grains consist mainly of quartz and feldspar. Sediment texture is grain supported to matrix supported and rich in authigenic glauconite pellets formedwithin matrix. Glauconite is aggregated by fine pellets that are pale green in grain margin and green to dark green in grain center. Some glauconite grains are coated by oxidized iron layers. Recrystallized calcite aggregates occupy matrix as relictminerals.313-M0027A-171R-1_38-42cm_TSB_270058_photo313-M0027A-171R-1_38-42cm_TSB_270058_photo.tif
313-M0027A-171R-1,38-421489.77313-M0027A-171R-1_38-42cm_TSB_270059_photo313-M0027A-171R-1_38-42cm_TSB_270059_photo.tif
313-M0027A-171R-1,38-421489.77313-M0027A-171R-1_38-42cm_TSB_270060_photo313-M0027A-171R-1_38-42cm_TSB_270060_photo.tif
313-M0027A-171R-1,38-421489.77313-M0027A-171R-1_38-42cm_TSB_270061_photo313-M0027A-171R-1_38-42cm_TSB_270061_photo.tif