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  • 1
    Publication Date: 2023-06-27
    Keywords: 27-261; Comment; Deep Sea Drilling Project; Demagnetization level; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Error, absolute; Glomar Challenger; Indian Ocean//PLAIN; Leg27; NRM, Declination; NRM, Inclination; NRM, Intensity; Number of observations; Polarity; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 620 data points
    Location Call Number Limitation Availability
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  • 2
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    PANGAEA
    In:  Supplement to: Ogg, James G; Kodama, Kazuto; Wallick, Brian P (1992): Lower Cretaceous magnetostratigraphy and paleolatitudes off Northwest Australia, ODP Site 765 and DSDP Site 261, Argo Abyssal Plain, and ODP Site 766, Gascoyne Abyssal Plain. In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 523-548, https://doi.org/10.2973/odp.proc.sr.123.128.1992
    Publication Date: 2024-01-09
    Description: Lower Cretaceous sediments were sampled for magnetostratigraphy at three sites. ODP Site 765 and DSDP Site 261, in the Argo Abyssal Plain, consist primarily of brownish-red to gray claystone having hematite and magnetite carriers of characteristic magnetization. ODP Site 766, in the Gascoyne Abyssal Plain, consists mainly of dark greenish-gray volcaniclastic turbidites with magnetite as the carrier of characteristic magnetization. Progressive thermal demagnetization (Sites 765 and 261) or alternating field demagnetization (Site 766) yielded well-defined polarity zones and a set of reliable paleolatitudes. Magnetic polarity chrons were assigned to polarity zones using biostratigraphic correlations. Late Aptian chron M"-1"r, a brief reversed-polarity chron younger than MOr, is a narrow, 40-cm feature delimited in Hole 765C. Early Aptian reversed-polarity chron MOr is also present in Hole 765C. Polarity chrons Mir through M3r were observed in the Barremian of all three sites. Valanginian and Hauterivian polarity chrons can be tentatively assigned to polarity zones only in Hole 766A. The paleolatitude of this region remained at 35° to 37°S from the Berriasian through the Aptian. During this interval, there was approximately 16° of clockwise rotation, with the oriented sample suites of Site 765 displaying a Berriasian declination of 307° to an Aptian declination of 323°. These results are consistent with the interpolated Early Cretaceous apparent polar wander for Australia, but indicate that this region was approximately 5 infinity farther north than predicted.
    Keywords: 123-765C; 123-766A; 27-261; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Indian Ocean//PLAIN; Joides Resolution; Leg123; Leg27; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  Supplement to: Wallick, Brian P; Steiner, Maureen B (1992): Paleomagnetic and rock magnetic properties of Jurassic quiet zone basalts, Hole 801C. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 455-470, https://doi.org/10.2973/odp.proc.sr.129.135.1992
    Publication Date: 2024-01-09
    Description: The paleomagnetic and rock magnetic properties of 51 Jurassic basalts from Ocean Drilling Program (ODP) Hole 801C have been examined. Magnetic properties vary with lithologic composition; alkalic rocks and hydrothermally-altered tholeiites are much weaker in intensity and generally contain higher coercivity magnetic components than the older and less-altered tholeiites at the base of the hole. For the entire column, the Jurassic basalts have an average initial natural remanent magnetization (NRM) intensity of approximately 1.24 A/m and average median destructive fields (MDF) of 8.31 mT. These values and the mean Koenigsberger ratio of 1.7 are very similar to results obtained for Jurassic basalts from the Atlantic (DSDP Leg 76). The similarities suggest that the basalts of both sites and their remanence characteristics are representative of Jurassic oceanic crust. The most profound discovery in these samples was the presence of 5 inclination zones, each showing consistent positive (or negative) polarity opposite the overlying and underlying polarity bands. We interpret these to represent a record of change in polarity of the EarthÆs magnetic field and, because of the large number over such a short interval (60 m) of crust, we assert that the rapid change in polarity during the Jurassic is the probable reason behind the origin of the Jurassic Quiet Zone.
    Keywords: 129-801C; DRILL; Drilling/drill rig; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 4
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    PANGAEA
    In:  Supplement to: Wallick, Brian P; Steiner, Maureen B (1992): Paleomagnetism of Cretaceous basalts from the East Mariana Basin, western Pacific Ocean. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 447-454, https://doi.org/10.2973/odp.proc.sr.129.134.1992
    Publication Date: 2024-01-09
    Description: Cretaceous basalts have been recovered at several Ocean Drilling Program and Deep Sea Drilling Project sites where basement of Jurassic age was predicted. Sites 800 and 802, Leg 129, both fall in this category. We have examined the paleomagnetic properties of 25 basalt samples from Site 802 in order to establish a paleolatitude for the site at the time of basalt emplacement and to compare the results to those from Deep Sea Drilling Project Site 462. Mean natural remanent magnetization intensity for the Site 802 basalts was found to be approximately 12 A/m consistent with typical oceanic basalts. Mean stable inclination is -34.7° ± 2.2 which implies a paleolatitude of approximately 19.4°S. This is very similar to the paleolatitudes calculated for Site 462 basalts and suggests - along with similarities in geochemistry, magnetic properties, and projected age of Site 802 basalt emplacement - both contemporaneity of and a possible source link between the two sites.
    Keywords: 129-802A; DRILL; Drilling/drill rig; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-01-09
    Keywords: 123-765C; Comment; Demagnetization level; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Error, absolute; Joides Resolution; Leg123; NRM, Declination; NRM, Inclination; NRM, Intensity; Number of observations; Ocean Drilling Program; ODP; Polarity; Sample code/label; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: text/tab-separated-values, 2515 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-01-09
    Keywords: 129-802A; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Inclination; Intensity; Joides Resolution; Koenigsberger ratio; Leg129; Lithologic unit/sequence; Magnetic susceptibility; North Pacific Ocean; NRM, Inclination; NRM, Intensity; NRM, median destructive field of natural remanent magnetization, alternating field; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 225 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-01-09
    Keywords: 129-802A; Demagnetizing field; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg129; North Pacific Ocean; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 1545 data points
    Location Call Number Limitation Availability
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  • 8
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    PANGAEA
    In:  Supplement to: Wallick, Brian P; Christensen, Nikolas I; Ballotti, Dean M (1992): High-pressure velocity measurements of Jurassic Basalt, Leg 129. In: Larson, RL; Lancelot, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 129, 501-506, https://doi.org/10.2973/odp.proc.sr.129.140.1992
    Publication Date: 2024-01-09
    Description: Compressional wave velocities and densities were measured for 6 basalt samples from ODP Hole 801B and 16 samples from ODP Hole 801C, a site that represents the first drilling of Jurassic-age crustal rocks in the Pacific basin. Incremental measurements, taken to a total pressure of 200 MPa, show a systematic decrease in velocity with increasing porosity and a related increase with increasing wet-bulk density. A comparison of the plot of porosity vs. compressional wave velocity with the theoretical equation from Wyllie et al. (1958) suggests this equation is inappropriate for oceanic basalts because of mineral alteration in high porosity samples. Also of interest is the dramatic change in velocity across a hydrothermal boundary. Basalts below this hydrothermal layer have a mean velocity of 6.05 km/s at 60 MPa while those above show a mean velocity of 4.55 km/s at 60 MPa. The low velocity values of the basalts above the hydrothermal deposit may be attributed to the higher porosity and composition observed in these rocks; the higher porosity is possibly the result of increased exposure to circulating seawater.
    Keywords: 129-801B; 129-801C; Density, wet bulk; Depth, relative; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg129; North Pacific Ocean; Ocean Drilling Program; ODP; Porosity; Sample code/label; Velocity, compressional wave
    Type: Dataset
    Format: text/tab-separated-values, 242 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-01-09
    Keywords: 129-801C; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Hysteresis, coercive field; Hysteresis, saturation field; Hysteresis, saturation magnetization, per unit volume; Inclination; Intensity; Joides Resolution; Koenigsberger ratio; Leg129; Lithologic unit/sequence; Magnetic susceptibility; North Pacific Ocean; NRM, Inclination; NRM, Intensity; NRM, median destructive field of natural remanent magnetization, alternating field; Ocean Drilling Program; ODP; Polarity; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 662 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-01-09
    Keywords: 129-801C; Demagnetization level; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg129; North Pacific Ocean; NRM, Declination after demagnetization; NRM, Inclination after demagnetization; NRM, Intensity after demagnetization; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 3050 data points
    Location Call Number Limitation Availability
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