IODP Expedition 381 Scientists (2020): Smear slide descriptions of IODP Hole 381-M0080A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.913456
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
McNeill, Lisa C; Shillington, Donna J; Carter, Gareth; IODP Expedition 381 Scientists (2019): Corinth Active Rift Development. Proceedings of the International Ocean Discovery Program, 381: College Station, TX (International Ocean Discovery Program), https://doi.org/10.14379/iodp.proc.381.2019
Further details:
Project(s):
Coverage:
Latitude: 38.120000 * Longitude: 23.086300
Date/Time Start: 2017-12-02T00:00:00 * Date/Time End: 2017-12-15T00:00:00
Event(s):
381-M0080A (COR-04A) * Latitude: 38.120000 * Longitude: 23.086300 * Date/Time Start: 2017-12-02T00:00:00 * Date/Time End: 2017-12-15T00:00:00 * IGSN: IBCR0381EHG0001 * Location: Gulf of Corinth * Campaign: Exp381 * Basis: Fugro Synergy * Method/Device: Core (CORE)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | IODP Expedition 381 Scientists | DSDP/ODP/IODP sample designation | ||
2 | Sample ID | Sample ID | IODP Expedition 381 Scientists | Smear slide number | ||
3 | Depth, composite | Depth comp | mcd | IODP Expedition 381 Scientists | Top | |
4 | Main Lithology | Main lith | IODP Expedition 381 Scientists | |||
5 | Sand | Sand | % | IODP Expedition 381 Scientists | ||
6 | Silt | Silt | % | IODP Expedition 381 Scientists | ||
7 | Clay minerals | Clay min | % | IODP Expedition 381 Scientists | ||
8 | Description | Description | IODP Expedition 381 Scientists | Visual description |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
207 data points
Data
1 Sample label | 2 Sample ID | 3 Depth comp [mcd] | 4 Main lith | 5 Sand [%] | 6 Silt [%] | 7 Clay min [%] | 8 Description |
---|---|---|---|---|---|---|---|
381-M0080A-4P-1,49-50 | 1 | 9.49 | dominant or major lithology | 0 | 65 | 35 | Detrital clayey silt. Moderately sorted, subrounded grains. Abundance of calcite, quartz. Common feldspars and micas. Common biogenics (mainly diatoms). |
381-M0080A-7P-1,131-132 | 1 | 22.51 | dominant or major lithology | 0 | 90 | 10 | Calcareous silt. Moderately to well sorted, subrounded grains. Dominance of aragonite. Abundant calcite. Rare to common biogenic components and detritals. |
381-M0080A-7P-2,10-11 | 1 | 22.80 | dominant or major lithology | 0 | 90 | 10 | Calcareous silt. Major presence of aragonite needles. Common detritals (carbonates and quartz). |
381-M0080A-7P-2,44-45 | 2 | 23.14 | dominant or major lithology | 0 | 65 | 35 | Biogenic-calcarous clayey silt. Poorly sorted, subangular to subrounded grains. Dominance of biogenic components (diatoms, nannos and other bioclasts). Abundant calcite. Common to abundant detritals. Common organics. |
381-M0080A-7P-4,19-20 | 1 | 25.76 | dominant or major lithology | 0 | 40 | 60 | Detrital silty clay. Moderately sorted, subrounded grains. Abundace of calcite and quartz. Feldspars and micas are common. |
381-M0080A-13P-1,50-51 | 1 | 40.50 | dominant or major lithology | 20 | 45 | 35 | Detrital Sandy Mud. Poorly sorted, subangular to subrounded grains. Dominance of calcite and detritals (reworked carbonates and quartz). Abundant organic components. |
381-M0080A-13P-1,52-53 | 2 | 40.52 | dominant or major lithology | 0 | 30 | 70 | Detrital Silty clay. Well sorted, subrounded grains. Dominance of calcite and quartz. Rare to common organics. |
381-M0080A-13P-2,39-40 | 1 | 41.88 | dominant or major lithology | 30 | 40 | 30 | Detrital sandy mud. Poorly sorted, subangular to subrounded grains. Dominance of detitals (quartz, micas, reworked carbonates, feldspars). Common organic components. |
381-M0080A-17P-1,82-83 | 1 | 54.02 | dominant or major lithology | 0 | 85 | 15 | Calcareous very fine silt. Very well sorted, rounded grains. Major, exclusive presence of calcite mineral grains. |
381-M0080A-17P-2,28-29 | 1 | 54.98 | dominant or major lithology | 0 | 60 | 40 | Detrital clayey silt. Moderately sorted, subrounded grains. Dominance of calcite. Common to abundant. Common framboidal Pyrite. |
381-M0080A-18P-1,135-136 | 1 | 59.25 | dominant or major lithology | 0 | 65 | 35 | Detrital clayey silt. Poorly to moderately sorted, subrounded grains. Dominance of calcite and detritals. Common pyritized features. Rare biogenics. |
381-M0080A-38V-2,118-119 | 1 | 130.98 | dominant or major lithology | 0 | 60 | 40 | Calcareous clayey silt. Well sorted, subrounded grains. Dominance of aragonite. Abundant calcite and other detritals. Rare to common pyritized features. Rare biogenics. |
381-M0080A-40V-1,44-45 | 1 | 137.14 | dominant or major lithology | 0 | 85 | 15 | Calcareous very fine silt. Very well sorted, rounded grains. Common organic components and biogenics. Rare other lithics. |
381-M0080A-40V-1,86-87 | 2 | 137.56 | dominant or major lithology | 0 | 75 | 25 | Biogenic Siliceous clayey silt. Poorly sorted, subangular grains. Major presence of diatom fragments and individuals. Abundant detritals (mostly carbonates). |
381-M0080A-50R-2,92-93 | 1 | 181.42 | dominant or major lithology | 0 | 85 | 15 | Calcareous very fine silt. Very well sorted, rounded grains. Major presence of calcite. Common to abundant diatoms. |
381-M0080A-54R-2,49-50 | 1 | 200.99 | dominant or major lithology | 0 | 60 | 40 | Calcareous clayey silt. Moderately to well sorted, subrounded to rounded grains. Dominance of aragonite needles and well rounded calcite grains. Abundant diatoms and framboidal pyrite. |
381-M0080A-54R-3,61-62 | 1 | 202.61 | 0 | 60 | 40 | Detrital clayey silt. Moderately to well sorted, rounded to well rounded grains, highly spherical. Dominance of detritals incl. quartz, feldspar, carbonates. Abundant aragonite needles. Common framboidal pyrite. | |
381-M0080A-56R-4,0-1 | 1 | 212.25 | dominant or major lithology | 0 | 85 | 15 | Calcareous Silt. Moder- well sorted subrounded grains. Major aragonite presence. Abundant calcite. Other lithics and biogenics are rare. |
381-M0080A-57R-2,106-107 | 1 | 215.56 | dominant or major lithology | 0 | 90 | 10 | Calcareous silt. Dominance of aragonite. Abundant calcite. Common organics and rounded detrital grains. |
381-M0080A-58R-2,134-140 | 1 | 220.33 | minor lithology | 0 | 90 | 10 | Detrital silt. Poorly sorted, subrounded grains. Rounded grains of calcite, feldspars and quartz with high sphericity. Abundant aragonite needles. |
381-M0080A-61R-2,61-62 | 1 | 229.79 | dominant or major lithology | 0 | 80 | 20 | Detrital silt. Poorly sorted, subrounded grains. Dominance of detrital material incl. high abundance of carbonates, quartz and lower of plagioclases and pyroxenes. Common to abundant aragonite needles. |
381-M0080A-68R-3,11-12 | 1 | 257.81 | dominant or major lithology | 0 | 35 | 65 | Detrital Silty Clay. Poorly sorted subrounded grains. Dominance of ophiolite-related minerals (serp. Olivine, pyroxenes, plagioclases) in irregular shapes. Abundant iron oxides. Calcite is common as well as quartz. |
381-M0080A-87R-1,0-2 | 1 | 311.50 | dominant or major lithology | 0 | 35 | 65 | Detrital Silty Clay. Poorly sorted subrounded grains. Dominance of ophiolite-related minerals (serp. Olivine, pyroxenes, plagioclases) in irregular shapes. Abundant iron oxides. Calcite and quartz are common. |
381-M0080A-96R-2,4-5 | 1 | 342.66 | dominant or major lithology | 10 | 90 | 0 | Detrital silt. Moderately to well sorted, subrounded to rounded. Dominance of feldspars and calcite. Abundant Fe-oxides. Pyroxenes are common. |
381-M0080A-97R-2,85-86 | 1 | 347.35 | dominant or major lithology | 85 | 15 | 0 | Detrital sand. Moderately to well sorted, subangular to subrounded grains. Major presence of feldspars (plagioclase order). Common to abundant pyroxenes. |
381-M0080A-106R-3,13-14 | 1 | 380.74 | dominant or major lithology | 0 | 70 | 30 | Detrital clayey silt. Poorly sorted subangular grains. Dominance of calcite, quartz and chert lithics. Iron oxides are common. Rare to common ophiolitic material. |