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Hillenbrand, Claus-Dieter; Ehrmann, Werner (2005): Clay mineral composition and biogenic opal content in upper Miocene to Quaternary drift sediments, ODP Site 178-1095 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.218251, In supplement to: Hillenbrand, C-D; Ehrmann, W (2005): Late Neogene to Quaternary environmental changes in the Antarctic Peninsula region: evidence from drift sediments. Global and Planetary Change, 45, 165-191, https://doi.org/10.1016/j.gloplacha.2004.09.006

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Project(s):
Coverage:
Latitude: -66.985400 * Longitude: -78.487867
Date/Time Start: 1998-02-13T00:00:00 * Date/Time End: 1998-02-13T00:00:00
Minimum DEPTH, sediment/rock: 1.04 m * Maximum DEPTH, sediment/rock: 561.60 m
Event(s):
178-1095 * Latitude: -66.985400 * Longitude: -78.487867 * Date/Time: 1998-02-13T00:00:00 * Elevation: -3841.4 m * Penetration: 745 m * Recovery: 554.1 m * Location: South Pacific Ocean * Campaign: Leg178 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 72 cores; 662 m cored; 83 m drilled; 83.7% recovery
Comment:
Clay mineralogy previously published in Hillenbarnd and Ehrmann (2001) datasets: doi:10.1594/PANGAEA.735188, biogenic opal content previously published by Hillenbrand and Fütterer (2001) datasets: doi:10.1594/PANGAEA.735190.
Size:
3782 data points

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