Thibault, Nicolas; Husson, Dorothée; Harlou, Rikke; Gardin, Silvia; Galbrun, Bruno; Huret, Emilia; Minoletti, Fabrice (2012): (Appendix 1) Values of inclination, paleomagnetic interpretation and additional remarks for the upper Campanian-Maastrichtian of ODP Hole 122-762C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.811600, In supplement to: Thibault, N et al. (2012): Astronomical calibration of upper Campanian–Maastrichtian carbon isotope events and calcareous plankton biostratigraphy in the Indian Ocean (ODP Hole 762C): Implication for the age of the Campanian–Maastrichtian boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 52-71, https://doi.org/10.1016/j.palaeo.2012.03.027
Always quote citation above when using data! You can download the citation in several formats below.
Original version:
Galbrun, Bruno (1992): (Appendix B) Direction of characteristic magnetization of ODP Hole 122-762C. PANGAEA, https://doi.org/10.1594/PANGAEA.811685
Galbrun, Bruno (1992): Magnetostratigraphy of upper Cretaceous and lower Tertiary sediments, Sites 761 and 762, Exmouth Plateau, Northwest Australia. In: von Rad, U; Haq, BU; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 122, 699-716, https://doi.org/10.2973/odp.proc.sr.122.149.1992
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -19.887000 * Longitude: 112.254000
Date/Time Start: 1988-07-27T03:25:00 * Date/Time End: 1988-08-05T08:30:00
Minimum DEPTH, sediment/rock: 550.30 m * Maximum DEPTH, sediment/rock: 645.91 m
Event(s):
122-762C * Latitude: -19.887000 * Longitude: 112.254000 * Date/Time Start: 1988-07-27T03:25:00 * Date/Time End: 1988-08-05T08:30:00 * Elevation: -1371.0 m * Penetration: 940 m * Recovery: 534.54 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg122 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 91 core; 940 m cored; 0 m drilled; 56.9 % recovery
Comment:
Sediment depth is given in mbsf, base C33n in 704.72 mbsf.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Sample code/label | Sample label | Thibault, Nicolas | DSDP/ODP/IODP sample designation | ||
| 2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 3 | Inclination | Incl | deg | Thibault, Nicolas | ||
| 4 | Chronozone | Chronozone | Thibault, Nicolas | Paleomagnetic Interpretation | ||
| 5 | Comment | Comment | Thibault, Nicolas | |||
| 6 | Depth, adjusted | Depth adj | ambsf | Thibault, Nicolas | ||
| 7 | Reference/source | Reference | Thibault, Nicolas |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
455 data points
Data
| 1 Sample label | 2 Depth sed [m] | 3 Incl [deg] | 4 Chronozone | 5 Comment | 6 Depth adj [ambsf] | 7 Reference |
|---|---|---|---|---|---|---|
| 122-762C-42X-4,80 | 550.30 | -58 | C29n | Galbrun (1992) | ||
| 122-762C-42X-5,75 | 551.76 | -2 | ? | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-42X-5,130 | 552.30 | 11 | C29r | Galbrun (1992) | ||
| 122-762C-42X-6,25 | 552.75 | 6 | C29r | Galbrun (1992) | ||
| 122-762C-42X-6,136 | 553.86 | 29 | C29r | Galbrun (1992) | ||
| 122-762C-43X-1,41 | 554.91 | 41 | C29r | K-Pg at 554.8 mbsf | Galbrun (1992) | |
| 122-762C-43X-1,100 | 555.50 | 53 | C29r | Galbrun (1992) | ||
| 122-762C-43X-2,50 | 556.50 | 20 | C29r base of Galbrun (1992) does not fit with the FO of M. prinsii | 557.73 | Galbrun (1992) | |
| 122-762C-43X-2,110 | 557.10 | -40 | weak | 558.33 | Galbrun (1992) | |
| 122-762C-43X-3,42 | 557.92 | -55 | ? | Galbrun (1992) | ||
| 122-762C-43X-3,141 | 558.91 | -18 | weak | Galbrun (1992) | ||
| 122-762C-43X-4,20 | 559.20 | -12 | weak | Galbrun (1992) | ||
| 122-762C-43X-4,113 | 560.13 | -22 | weak | FO Micula prinsii at 560.46 mbsf | Galbrun (1992) | |
| 122-762C-43X-5,22 | 560.72 | 3 | weak | FO Micula prinsii at 560.46 mbsf | Galbrun (1992) | |
| 122-762C-43X-5,96 | 561.46 | -23 | weak | Galbrun (1992) | ||
| 122-762C-44X-1,51 | 564.51 | -59 | ? | Galbrun (1992) | ||
| 122-762C-44X-1,132 | 565.32 | 52 | C29r larger uncertainty | 566.55 | Galbrun (1992) | |
| 122-762C-44X-2,52 | 566.02 | -56 | C30n | 567.25 | Galbrun (1992) | |
| 122-762C-44X-2,132 | 566.83 | -76 | C30n | Galbrun (1992) | ||
| 122-762C-44X-3,126 | 568.26 | -46 | C30n | Galbrun (1992) | ||
| 122-762C-44X-4,95 | 569.45 | -49 | C30n | Galbrun (1992) | ||
| 122-762C-44X-5,102 | 571.02 | -62 | C30n | Galbrun (1992) | ||
| 122-762C-44X-6,67 | 572.17 | -44 | C30n | Galbrun (1992) | ||
| 122-762C-45X-1,29 | 573.79 | -61 | C30n | Galbrun (1992) | ||
| 122-762C-45X-2,112 | 576.12 | -58 | C30n | Galbrun (1992) | ||
| 122-762C-45X-3,86 | 577.36 | -65 | C30n | Galbrun (1992) | ||
| 122-762C-45X-4,60 | 578.60 | -23 | C30n | Galbrun (1992) | ||
| 122-762C-45X-4,111 | 579.11 | -32 | C30n | Galbrun (1992) | ||
| 122-762C-45X-5,24 | 579.74 | -13 | C30n | Galbrun (1992) | ||
| 122-762C-45X-5,110 | 580.60 | -64 | C30n | Galbrun (1992) | ||
| 122-762C-46X-1,44 | 583.44 | -61 | C30n | Galbrun (1992) | ||
| 122-762C-46X-1,120 | 584.20 | -9 | C30n | Galbrun (1992) | ||
| 122-762C-46X-2,41 | 584.91 | 34 | C30n | Galbrun (1992) | ||
| 122-762C-46X-2,117 | 585.67 | -42 | C30n | Galbrun (1992) | ||
| 122-762C-46X-3,45 | 586.45 | -44 | C30n | Galbrun (1992) | ||
| 122-762C-46X-3,117 | 587.17 | -52 | C30n | Galbrun (1992) | ||
| 122-762C-46X-4,38 | 587.88 | -49 | C30n | Galbrun (1992) | ||
| 122-762C-46X-4,114 | 588.64 | -57 | C30n | No recovery interval between 589.5 and 592.5 mbsf | 590.19 | Galbrun (1992) |
| 122-762C-47X-1,44 | 592.94 | 55 | C30r | No recovery interval between 589.5 and 592.5 mbsf | 594.49 | Galbrun (1992) |
| 122-762C-47X-2,101 | 593.51 | 18 | C30r | ~500 kyr gap around 595.45 mbsf | 595.06 | Galbrun (1992) |
| 122-762C-47X-3,43 | 595.93 | -16 | C31n | ~500 kyr gap around 595.45 mbsf | 597.48 | Galbrun (1992) |
| 122-762C-47X-3,95 | 596.45 | -73 | C31n | Galbrun (1992) | ||
| 122-762C-47X-4,48 | 597.48 | -34 | C31n | Galbrun (1992) | ||
| 122-762C-47X-4,89,5 | 597.89 | -48 | C31n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-4,112 | 598.12 | -62 | C31n | 599.67 | Galbrun (1992) | |
| 122-762C-47X-4,120 | 598.20 | 57 | C31r | 599.75 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-47X-4,140 | 598.40 | 75 | C31r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-5,4 | 598.54 | 48 | C31r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-5,19 | 598.69 | 52 | C31r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-5,32 | 598.82 | 70 | C31r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-5,39,5 | 598.89 | 64 | C31r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-47X-5,46 | 598.96 | 75 | C31r | Galbrun (1992) | ||
| 122-762C-47X-5,101 | 599.51 | 63 | C31r | Galbrun (1992) | ||
| 122-762C-47X-6,40 | 600.40 | 83 | C31r | Galbrun (1992) | ||
| 122-762C-48X-1,54 | 602.54 | 80 | C31r | Galbrun (1992) | ||
| 122-762C-48X-2,36 | 603.86 | 58 | C31r | Galbrun (1992) | ||
| 122-762C-48X-3,30 | 605.30 | 67 | C31r | Galbrun (1992) | ||
| 122-762C-48X-4,65 | 607.15 | 67 | C31r | Galbrun (1992) | ||
| 122-762C-48X-5,131 | 609.31 | 63 | C31r | Galbrun (1992) | ||
| 122-762C-48X-6,47 | 609.97 | 63 | C31r | Galbrun (1992) | ||
| 122-762C-48X-7,30 | 611.31 | 66 | C31r | Galbrun (1992) | ||
| 122-762C-48X-CC,6 | 611.40 | 57 | C31r | 613.01 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-48X-CC,18 | 611.52 | -42 | C32n1n | 613.13 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-49X-1,10 | 611.60 | -25 | C32n1n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-1,26,5 | 611.76 | -14 | C32n1n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-1,37 | 611.87 | -45 | C32n1n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-1,48 | 611.98 | -24 | C32n1n | Galbrun (1992) | ||
| 122-762C-49X-1,58 | 612.08 | -40 | C32n1n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-1,78 | 612.28 | -48 | C32n1n | 614.25 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-49X-1,96 | 612.46 | 31 | C32n1r | 614.43 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-49X-1,118 | 612.68 | 52 | C32n1r | Galbrun (1992) | ||
| 122-762C-49X-1,122 | 612.72 | 56 | C32n1r | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-1,142,5 | 612.92 | 56 | C32n1r | 614.89 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-49X-2,3,5 | 613.03 | -70 | C32n2n | 615.00 | additional samples analysed by Galbrun in 2008 | |
| 122-762C-49X-2,20,5 | 613.20 | -45 | C32n2n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-2,49,5 | 613.42 | -55 | C32n2n | additional samples analysed by Galbrun in 2008 | ||
| 122-762C-49X-2,45 | 613.45 | -51 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-2,117 | 614.17 | -40 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-3,46 | 614.96 | 53 | very small reverse within C32n2n ? | Galbrun (1992) | ||
| 122-762C-49X-3,109 | 615.59 | -54 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-4,50 | 616.50 | -49 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-4,111 | 617.11 | -59 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-5,41 | 617.91 | -63 | C32n2n | Galbrun (1992) | ||
| 122-762C-49X-5,108 | 618.58 | -59 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-1,47 | 621.47 | -15 | C32n2n | Galbrun (1992) | ||
| 122-762C-40X-1,113 | 622.14 | -44 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-2,102 | 623.52 | -58 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-3,98 | 624.98 | -55 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-4,104 | 626.54 | -59 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-5,47 | 627.47 | -56 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-6,121 | 629.71 | -66 | C32n2n | Galbrun (1992) | ||
| 122-762C-50X-7,37 | 630.38 | -69 | C32n2n | Galbrun (1992) | ||
| 122-762C-51X-1,58 | 631.08 | -46 | C32n2n | 633.43 | Galbrun (1992) | |
| 122-762C-51X-1,135 | 631.87 | 38 | C32r1r | 634.22 | Galbrun (1992) | |
| 122-762C-51X-2,141 | 633.41 | 41 | C32r1r | Galbrun (1992) | ||
| 122-762C-51X-3,117 | 634.67 | 68 | C32r1r | Galbrun (1992) | ||
| 122-762C-51X-4,42 | 635.42 | 70 | C32r1r | 637.77 | Galbrun (1992) | |
| 122-762C-51X-4,135 | 636.35 | -30 | C32r1n | 638.70 | Galbrun (1992) | |
| 122-762C-51X-5,44 | 636.94 | -23 | C32r1n | 639.29 | Galbrun (1992) | |
| 122-762C-51X-5,133 | 637.84 | 8 | C32r2r | 640.19 | Galbrun (1992) | |
| 122-762C-51X-6,43 | 638.43 | 8 | C32r2r | 640.78 | Galbrun (1992) | |
| 122-762C-51X-6,112 | 639.13 | -32 | C33n | 641.48 | Galbrun (1992) | |
| 122-762C-52X-1,117 | 641.17 | -75 | C33n | Galbrun (1992) | ||
| 122-762C-52X-2,122 | 642.72 | -54 | C33n | Galbrun (1992) | ||
| 122-762C-52X-3,114 | 644.14 | -54 | C33n | Galbrun (1992) | ||
| 122-762C-52X-4,141 | 645.91 | -71 | C33n | Galbrun (1992) |