Markov, Yu D; Mozherovsky, A V; Pushkar', V S; Vashchenkova, N G; Nechaev, Victor P (2005): Composition of bottom sediments from the Clarion Fracture Zone [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.745656, Supplement to: Markov, YD et al. (2005): Sedimentation features and stratigraphic correlation of unconsolidated deposits from the Clarion Transform Fault Zone (Northeast Pacific). Pacific Geology, 24(4), 24-43
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Abstract:
New data on lithology and stratigraphy of Cenozoic sediments from the Clarion Transform Fault Zone (Pacific Ocean) have been obtained on the base of polygon studies. It has been established that on different blocks (uplifted and subsided) of the Clarion tectonic structure deposits of different age (Eocene to Quaternary) occur. Unconsolidated sediments have been deposited under pelagic conditions since Eocene (probably, since Early Cretaceous) until now. Their mineral composition and content of different ore components are given.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 18.919897 * Median Longitude: -140.388993 * South-bound Latitude: 13.012300 * West-bound Longitude: -175.191700 * North-bound Latitude: 31.111700 * East-bound Longitude: -119.997800
Event(s):
AVI13-17 * Latitude: 31.111700 * Longitude: -175.191700 * Elevation: -5360.0 m * Location: Northeast Pacific * Campaign: AVI13 * Basis: Akademik A. Vinogradov * Method/Device: Gravity corer (GC)
AVI13-73 * Latitude: 17.005000 * Longitude: -120.003300 * Elevation: -3860.0 m * Location: Northeast Pacific * Campaign: AVI13 * Basis: Akademik A. Vinogradov * Method/Device: Gravity corer (GC)
AVI13-74 * Latitude: 19.326700 * Longitude: -119.997800 * Elevation: -4030.0 m * Location: Northeast Pacific * Campaign: AVI13 * Basis: Akademik A. Vinogradov * Method/Device: Gravity corer (GC)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets
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Datasets listed in this publication series
- Markov, YD; Mozherovsky, AV; Pushkar', VS et al. (2005): (Table 2) Mineral composition of size fraction 0.100-0.050 mm from sediments of the Clarion Fracture Zone (without heavy minerals). https://doi.org/10.1594/PANGAEA.745242
- Markov, YD; Mozherovsky, AV; Pushkar', VS et al. (2005): (Table 3) Heavy clastic minerals of grain size fraction 0.100-0.050 mm from sediments of the Clarion Fracture Zone. https://doi.org/10.1594/PANGAEA.745247
- Markov, YD; Mozherovsky, AV; Pushkar', VS et al. (2005): (Table 4) Chemical composition of bottom sediments from the Clarion Fracture Zone. https://doi.org/10.1594/PANGAEA.745654