Expedition 313 Scientists (2010): Description of thin sections of Hole 313-M0028A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761539
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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
Project(s):
Coverage:
Latitude: 39.565713 * Longitude: -73.497247
Date/Time Start: 2009-05-23T14:20:00 * Date/Time End: 2009-05-23T14:20:00
Minimum DEPTH, sediment/rock: 286.83 m * Maximum DEPTH, sediment/rock: 389.61 m
Event(s):
313-M0028A (MAT-2D) * Latitude: 39.565713 * Longitude: -73.497247 * Date/Time: 2009-05-23T14:20:00 * Elevation: -35.0 m * IGSN: IBCR0313RHPV001 * Penetration: 668.66 m * Recovery: 385.5 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):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Expedition 313 Scientists | |||
| 2 | Thin section | Thin sec | # | Expedition 313 Scientists | ||
| 3 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 4 | Lithology/composition/facies | Lithology | Expedition 313 Scientists | Visual description | ||
| 5 | Lithology/composition/facies | Lithology | Expedition 313 Scientists | Visual description | continuation | |
| 6 | File name | File name | Expedition 313 Scientists | TSB photo | ||
| 7 | Uniform resource locator/link to image | URL image | Expedition 313 Scientists | link to TSB photo |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
54 data points
Data
| 1 Sample label | 2 Thin sec [#] | 3 Depth sed [m] | 4 Lithology | 5 Lithology (continuation) | 6 File name (TSB photo) | 7 URL image (link to TSB photo) |
|---|---|---|---|---|---|---|
| 313-M0028A-25R-1, 5-11 | 1 | 286.83 | Glauconite-bearing medium silty sandstone. Though most grains are subangular to subrounded, angular or rounded grains are also found. Quartz and feldspar (microcline, perthite, and plagioclase) grains are the main detrital grains, and rock fragments | (granitoids, quatizite, and schist/gneiss), opaque minerals (including haematite), and heavy minerals (zircon, etc.) are associated. | 313-M0028A-25R-1_5-11cm_TSB_270071_photo | 313-M0028A-25R-1_5-11cm_TSB_270071_photo.tif |
| 313-M0028A-25R-1, 5-11 | 1 | 286.83 | 313-M0028A-25R-1_5-11cm_TSB_270072_photo | 313-M0028A-25R-1_5-11cm_TSB_270072_photo.tif | ||
| 313-M0028A-25R-1, 5-11 | 1 | 286.83 | 313-M0028A-25R-1_5-11cm_TSB_270073_photo | 313-M0028A-25R-1_5-11cm_TSB_270073_photo.tif | ||
| 313-M0028A-25R-1, 5-11 | 1 | 286.83 | 313-M0028A-25R-1_5-11cm_TSB_270074_photo | 313-M0028A-25R-1_5-11cm_TSB_270074_photo.tif | ||
| 313-M0028A-25R-CC, 3-9 | 1 | 288.10 | Very fine to fine silty sandstone cemented with a large amount of calcite. Some mica and opaque minerals. Initially matrix-rich sediment. Most grains comprise monocrystalline quartz, subrounded to subangular, possibly derived from granitoid. Feldspar | and rock fragments are also found. Many grains are coated with calcite. Matrix is filled with argillaceous and calcareous mud and clay. Framboidal iron sulfide occurs in matrix. | 313-M0028A-25R-CC_3-9cm_TSB_270063_photo | 313-M0028A-25R-CC_3-9cm_TSB_270063_photo.tif |
| 313-M0028A-25R-CC, 3-9 | 1 | 288.10 | 313-M0028A-25R-CC_3-9cm_TSB_270064_photo | 313-M0028A-25R-CC_3-9cm_TSB_270064_photo.tif | ||
| 313-M0028A-25R-CC, 3-9 | 1 | 288.10 | 313-M0028A-25R-CC_3-9cm_TSB_270065_photo | 313-M0028A-25R-CC_3-9cm_TSB_270065_photo.tif | ||
| 313-M0028A-25R-CC, 3-9 | 1 | 288.10 | 313-M0028A-25R-CC_3-9cm_TSB_270066_photo | 313-M0028A-25R-CC_3-9cm_TSB_270066_photo.tif | ||
| 313-M0028A-67R-1, 15-19 | 1 | 389.61 | Glauconitic silty fine-medium sand with calcite cement. Quartz is rounded to subrounded and well sorted. Quartz and feldspar (microcline, plagiclase, and perthite) grains are roughly oriented along the bedding. Matrix is cemented by calcite. | Amorphous iron oxide minerals are developed along pore space. Glauconite pellets are formed in matrix, and authigenic magnetic grains occur along glauconite margins. An articulated small shell is observed to be perpendicular to the bedding plane. | 313-M0028A-67R-1_15-19cm_TSB_270067_photo | 313-M0028A-67R-1_15-19cm_TSB_270067_photo.tif |
| 313-M0028A-67R-1, 15-19 | 1 | 389.61 | 313-M0028A-67R-1_15-19cm_TSB_270068_photo | 313-M0028A-67R-1_15-19cm_TSB_270068_photo.tif | ||
| 313-M0028A-67R-1, 15-19 | 1 | 389.61 | 313-M0028A-67R-1_15-19cm_TSB_270069_photo | 313-M0028A-67R-1_15-19cm_TSB_270069_photo.tif | ||
| 313-M0028A-67R-1, 15-19 | 1 | 389.61 | 313-M0028A-67R-1_15-19cm_TSB_270070_photo | 313-M0028A-67R-1_15-19cm_TSB_270070_photo.tif |