Expedition 313 Scientists (2010): Correlation of seismic sequence boundaries to core surfaces, IODP Hole 313-M0029A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.761248
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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: 39.519508 * Longitude: -73.413208
Date/Time Start: 2009-06-21T08:59:00 * Date/Time End: 2009-06-21T08:59:00
Minimum Elevation: -36.0 m * Maximum Elevation: -36.0 m
Event(s):
313-M0029A (MAT-3A) * Latitude: 39.519508 * Longitude: -73.413208 * Date/Time: 2009-06-21T08:59:00 * Elevation: -36.0 m * IGSN: IBCR0313RHQV001 * Penetration: 754.55 m * Recovery: 454.31 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
Comment:
Notes: BKSA95 from Cande and Kent (1995). Seismic picks from Seisworks. Predicted depth and ages for seismic sequence boundaries m1 to m5.8 from Monteverde et al. (2008). Two predicted depths in two way travel time (TWT) and depth (mbsf) are given, the first from Monteverde et al. (2008) and the second from Mountain et al. (prospectus). Actual depth and actual core are the best fit to surfaces or other contacts noted in the cores. * = where multiple surfaces potentially fit predicted sequence boundaries, preferred placement is in bold. Preliminary age and age error are derived from "Chronology." NR = none recovered. SB = sequence boundary, FS = flooding surface, TGR = total gamma ray.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Age, minimum/young | Age young | Expedition 313 Scientists | Predicted age BKSA95 (Ma) | ||
| 2 | Age, maximum/old | Age old | Expedition 313 Scientists | Predicted age BKSA95 (Ma) | ||
| 3 | Boundary description | Bound descr | Expedition 313 Scientists | Seismic sequence boundaries | ||
| 4 | Two-way traveltime | TWT | s | Expedition 313 Scientists | Seismic picks | |
| 5 | Depth comment | Depth comm | Expedition 313 Scientists | Predicted depth (mbsf) Monteverde et al. (2008) | ||
| 6 | Depth comment | Depth comm | Expedition 313 Scientists | Predicted depth (mbsf), seismic and velocity function core | ||
| 7 | Core | Core | Expedition 313 Scientists | Predicted core | ||
| 8 | Depth comment | Depth comm | Expedition 313 Scientists | Actual depth (mbsf) | ||
| 9 | Core | Core | Expedition 313 Scientists | Actual core, section. interval (cm) | ||
| 10 | Comment | Comment | Expedition 313 Scientists | |||
| 11 | Age, minimum/young | Age young | Expedition 313 Scientists | |||
| 12 | Age, maximum/old | Age old | Expedition 313 Scientists | |||
| 13 | Error | Error | Expedition 313 Scientists | from (Ma) | ||
| 14 | Error | Error | Expedition 313 Scientists | to (Ma) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
233 data points
Data
| 1 Age young (Predicted age BKSA95 (Ma)) | 2 Age old (Predicted age BKSA95 (Ma)) | 3 Bound descr (Seismic sequence boundaries) | 4 TWT [s] (Seismic picks) | 5 Depth comm (Predicted depth (mbsf) Montev...) | 6 Depth comm (Predicted depth (mbsf), seism...) | 7 Core (Predicted core) | 8 Depth comm (Actual depth (mbsf)) | 9 Core (Actual core, section. interva...) | 10 Comment | 11 Age young | 12 Age old | 13 Error (from (Ma)) | 14 Error (to (Ma)) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Base Pleistocene | 40-48 | 49.68 | 15R-1, 8 | ? | |||||||||
| 11.5 | m1 | 0.192 | 154 | 152-153 | 26R | ? | |||||||
| 12.8 | m2 | NR | ? | ||||||||||
| 13.6 | m3 | 0.236 | 192 | 190-195 | 32R-34R | ?193.17 | Base of ?31R-1 | ? | |||||
| ?14.1 | m4 | 0.280 | 230 | 225-235 | 37R-40R | ?231.70 | ?40R-1, 39 | SB; clay over silty fine sand | <13.2 | ||||
| m4.1 | 0.387 | 326 | 325-330 | 65R-66R | 325.13-325.23 | 65R-2, 80-90 | FS silty glauconite fine sand over silty clay | ||||||
| m4.2 | 0.403 | 341 | 345-350 | 72R-73R | 341.11 | Top of 71R-1 | FS burrowed surface; clay with sands into clay | ||||||
| 343.24-343.89 | 71R-2, 64R-72R-1, 57 | SB indurate contact; clays over claystones over muddy fine sand | ?13.4 | 12.6 | 13.7 | ||||||||
| m4.3 | 0.423 | 360 | 350-360 | 73R-77R | 350.40 | 74R-1, ~14 | FS burrowed surface; sands over silty clay; coarsen up above | ||||||
| m4.4 | 0.460 | 395 | 390-400 | 87R-90R | ~393.00-394.00 | 89R-1 | FS clayey interval with nodules | ||||||
| m4.5 | 0.517 | 449 | 445-455 | 106R-109R | 449.10 | 108R-1, 124-128 | SB irregular contact; glauconitic silty sand over siliceous silt | ?14.6 | 13.5 | 14.6 | |||
| 14.8 | 15.8 | m5 | 0.547 | 479 | 475-482 | 117R-118R | 478.61 | 118R-1, 25 | SB very fine sand/sandy silt, 57 cm thick burrowed zone; indurated siltstone to top of 20-1, medium-fine sand | 15 | 15.4 | 14.6 | 15.4 |
| 16 | 16.5 | m5.2 | 0.664 | 597 | 590-600 | 155R-160R | 602.25 | 161R-2, 37 | SB clayey silt over glauconite sand | 16.1 | 16.2 | 15.6 | 16.3 |
| m5.2 | |||||||||||||
| m5.2 | |||||||||||||
| 17.2 | m5.3 | 0.708 | 642 | 638-642 | 173R-174R | 634.43 | 171R-2, 57 | Large density peak; glaucontiic quartz sand over glauconite sand | 16.2 | 16.9 | 16.2 | 16.9 | |
| m5.3 | 640.51-641.20 | 175R-1, 50-120 (slurry between) | Silty glauconite sand over siltstone | ||||||||||
| m5.3 | 643.19 | 176R-1, 13 | SB glauconite sand over silt; density max; sharp decrease density at base | 16.9 | 18.3 | 16.9 | 18.3 | ||||||
| 17.8 | 18.2 | m5.4 | 0.723 | 658 | 660-670 | 182R-186R | 649.68 | 179R-1, 23 | SB? top indurated zone, clay with burrowed gluaconite above; glauconite sand to 23 cm; clay below; density peak; this is the likely core sequence boundary | ||||
| m5.7 | 662.37 | 183R-1, 102 | SB? slightly glauconitic clay over glauconite sand; density peak; VP increase 662, VP maximum 667.5; this is the seismic sequence boundary | ||||||||||
| 19.5 | m5.45 | 0.739 | 676 | 670-680 | 186R-190R | 673.71 | 189R-1, 15 | SB glauconite bed on clay | 16.9 | 18.3 | 16.9 | 18.3 | |
| 19.7 | m5.47 | 0.752 | 690 | 685-690 | 193R-194R | 683.66 | 192R-1, 46 | Top of glauconite; density increase | |||||
| m5.47 | 684.33 | 192R-2, 11 | Clay on glauconite; density increase | ||||||||||
| m5.47 | 687.87 | 193R-2, 60 | SB glauconite on clay; base of density high | 16.9 | 18.3 | 16.9 | 18.3 | ||||||
| 20.1 | m5.5 | NR | |||||||||||
| 20.2 | m5.6 | 0.777 | 716 | 700-710 | 197R-200R | 707.56/710.16 | Base of 200R-1/top of 201R-1 | SB in coring gap; glauconite sand above; clay below | ?18.5 | 18.3 | 19.0 | ||
| 20.4 | m5.7 | 0.802 | 743 | 735-742 | 210R-212R | 728.56 | 208R-1, 9-11 | SB dramatic burrowed contact glauconite sands over tan clays; large decrease in density across boundary | 19.6 | 20.2 | 19.6 | 20.2 | |
| 21.5 | 22 | m5.8 | 750-755 | 215R/TD | ?746.00 | 213R-1/214R-1-215R-1 top | ?SB base of TGR peak; glauconitic clay over coring gap over clay | ?21.3 | 20.4 | 21.6 | |||
| 750.00-752.86 | Base of 215R-top of 217R | Clay over coring gap over glauconitic clay | |||||||||||
| 753.80 mcd/753.22 mbsf | 217R-1, 36 | Core gamma peak, top glauconite | <?21.5 |