Minisini, Daniel (2017): (Table S3) 25 chronostratographic markers of the organic-rich Eagle Ford Group [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.878864, In supplement to: Minisini, Daniel; Eldrett, James S; Bergman, Steven; Forkner, Rob (2018): Chronostratigraphic framework and depositional environments in the organic‐rich, mudstone‐dominated Eagle Ford Group, Texas, USA. Sedimentology, 65(5), 1520-1557, https://doi.org/10.1111/sed.12437
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Coverage:
Median Latitude: 29.531840 * Median Longitude: -101.191581 * South-bound Latitude: 29.225213 * West-bound Longitude: -101.641973 * North-bound Latitude: 29.838466 * East-bound Longitude: -100.741189
Minimum DEPTH, sediment/rock: 25.50 m * Maximum DEPTH, sediment/rock: 153.30 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | Minisini, Daniel | |||
| 2 | Marker | Marker | # | Minisini, Daniel | ||
| 3 | Ageprofile Datum Description | Ageprof dat des | Minisini, Daniel | |||
| 4 | DEPTH, sediment/rock | Depth sed | m | Minisini, Daniel | Geocode | |
| 5 | Depth, top/min | Depth top | m | Minisini, Daniel | ||
| 6 | Depth, bottom/max | Depth bot | m | Minisini, Daniel |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
128 data points
Data
| 1 Event | 2 Marker [#] | 3 Ageprof dat des | 4 Depth sed [m] | 5 Depth top [m] | 6 Depth bot [m] |
|---|---|---|---|---|---|
| Shell_Innes-1 | 26 | Top Eagle Ford Gp | 25.50 | ||
| Shell_Innes-1 | 25 | Bentonite Q | 28.74 | ||
| Shell_Innes-1 | 24 | Bentonite P | 31.32 | ||
| Shell_Innes-1 | 23 | First Occurrence S. turonica (abrupt d13C drop in Innes) | 42.50 | ||
| Shell_Innes-1 | 22 | First Occurrence Q. gartneri (abrupt d13C drop in Innes) | 42.50 | ||
| Shell_Innes-1 | 21 | FDO O.totum persistent | 44.95 | ||
| Shell_Innes-1 | 20 | "Heteroelix shift" | 47.30 | ||
| Shell_Innes-1 | 19 | Last Occurrence H. chiastia, CIE peak | 48.80 | ||
| Shell_Innes-1 | 18 | Highest values of Co/Zr (5-7) | 50.00 | 49 | 51 |
| Shell_Innes-1 | 17 | First Occurrence D. hagni, Last Occurrence C.striatus | 51.50 | 51 | 52 |
| Shell_Innes-1 | 16 | Last Occurrence R.cushmani and GR drop upward | 53.10 | ||
| Shell_Innes-1 | 15 | Last Occurrence T. greenhornensis | 54.00 | ||
| Shell_Innes-1 | 14 | Peak in inoceramus fragments | 58.50 | 57 | 60 |
| Shell_Innes-1 | 13 | Last Common Occurrence C. longispinatum | 58.80 | ||
| Shell_Innes-1 | 12 | LSAO Bosedinia spp. and upward increase in coarser beds | 60.60 | ||
| Shell_Innes-1 | 11 | Bentonite X correlated through the GR curves | 63.50 | ||
| Shell_Innes-1 | 10 | Peak in inoceramus fragments and Bosedinia spp. | 64.50 | ||
| Shell_Innes-1 | 9 | Peak in inoceramus fragments | 66.00 | ||
| Shell_Innes-1 | 8 | First Occurrence C. kennedyi | 70.05 | ||
| Shell_Innes-1 | 7 | Top of well cross-stratified limestones | 71.00 | ||
| Shell_Innes-1 | 6 | Sharp increase of inoceramus fragments | 74.50 | 74 | 75 |
| Shell_Innes-1 | 5 | Bentonite encased in the mid Cenomanian Event | 75.45 | ||
| Shell_Innes-1 | 4 | Carbon Isotopic Excursion of the mid Cenomanian Event | 76.00 | 75 | 77 |
| Shell_Innes-1 | 3 | First Consistent Occurrence of inoceramus | 76.13 | ||
| Shell_Innes-1 | 2 | Influx L. siphoniphorum | 76.90 | ||
| Shell_Innes-1 | 1 | First Consistent Occurrence L. siphoniphorum | 77.80 | ||
| Shell_Innes-1 | 0 | Base Eagle Ford Gp | 80.65 | ||
| Shell_Iona-1 | 26 | Top Eagle Ford Gp | 41.90 | ||
| Shell_Iona-1 | 25 | Bentonite Q | 47.83 | ||
| Shell_Iona-1 | 24 | Bentonite P | 50.26 | ||
| Shell_Iona-1 | 23 | First Occurrence S. turonica (abrupt d13C drop in Innes) | 60.95 | ||
| Shell_Iona-1 | 22 | First Occurrence Q. gartneri (abrupt d13C drop in Innes) | 90.50 | ||
| Shell_Iona-1 | 21 | FDO O.totum persistent | 93.50 | ||
| Shell_Iona-1 | 20 | "Heteroelix shift" | 100.90 | ||
| Shell_Iona-1 | 19 | Last Occurrence H. chiastia, CIE peak | 101.80 | ||
| Shell_Iona-1 | 18 | Highest values of Co/Zr (5-7) | 103.50 | 103 | 104 |
| Shell_Iona-1 | 17 | First Occurrence D. hagni, Last Occurrence C.striatus | 104.50 | 104 | 105 |
| Shell_Iona-1 | 16 | Last Occurrence R.cushmani and GR drop upward | 105.40 | ||
| Shell_Iona-1 | 15 | Last Occurrence T. greenhornensis | 106.30 | ||
| Shell_Iona-1 | 14 | Peak in inoceramus fragments | 119.00 | 118 | 120 |
| Shell_Iona-1 | 13 | Last Common Occurrence C. longispinatum | 119.50 | ||
| Shell_Iona-1 | 12 | LSAO Bosedinia spp. and upward increase in coarser beds | 120.40 | ||
| Shell_Iona-1 | 11 | Bentonite X correlated through the GR curves | 127.12 | ||
| Shell_Iona-1 | 10 | Peak in inoceramus fragments and Bosedinia spp. | 127.50 | ||
| Shell_Iona-1 | 9 | Peak in inoceramus fragments | 132.00 | ||
| Shell_Iona-1 | 8 | First Occurrence C. kennedyi | 136.90 | ||
| Shell_Iona-1 | 7 | Top of well cross-stratified limestones | 139.00 | ||
| Shell_Iona-1 | 6 | Sharp increase of inoceramus fragments | 141.50 | 141 | 142 |
| Shell_Iona-1 | 5 | Bentonite encased in the mid Cenomanian Event | 142.10 | ||
| Shell_Iona-1 | 4 | Carbon Isotopic Excursion of the mid Cenomanian Event | 141.50 | 140 | 143 |
| Shell_Iona-1 | 3 | First Consistent Occurrence of inoceramus | 143.00 | ||
| Shell_Iona-1 | 2 | Influx L. siphoniphorum | 143.30 | ||
| Shell_Iona-1 | 1 | First Consistent Occurrence L. siphoniphorum | 144.15 | ||
| Shell_Iona-1 | 0 | Base Eagle Ford Gp | 153.30 |