Details of experiments at different stress levels from ODP Hole 170-1039B, 170-1040C and 205-1253
Cobertura |
MEDIAN LATITUDE: 9.649744 * MEDIAN LONGITUDE: -86.189822 * SOUTH-BOUND LATITUDE: 9.640000 * WEST-BOUND LONGITUDE: -86.200000 * NORTH-BOUND LATITUDE: 9.661600 * EAST-BOUND LONGITUDE: -86.178900 * DATE/TIME START: 1996-11-02T03:30:00 * DATE/TIME END: 2002-10-11T00:00:00 * MINIMUM DEPTH, sediment/rock: 72.86 m * MAXIMUM DEPTH, sediment/rock: 385.20 m |
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Data(s) |
04/08/2014
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Formato |
text/tab-separated-values, 136 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.834643 doi:10.1594/PANGAEA.834643 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
doi:10.1594/PANGAEA.834645 Ikari, Matt J; Niemeijer, André R; Spiers, KC; Kopf, Achim J; Saffer, Demian M (2013): Experimental evidence linking slip instability with seafloor lithology and topography at the Costa Rica convergent margin. Geology, 41(8), 891-894, doi:10.1130/G33956.1 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #170-1039B; 170-1040C; 205-1253; COMPCORE; Composite Core; Costa Rica subduction complex, North Pacific Ocean; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Event label; Experiment; Joides Resolution; Leg170; Leg205; Lithologic unit/sequence; Lithology/composition/facies; North Pacific Ocean; Ocean Drilling Program; ODP; ODP sample designation; Pressure, stress; Sample code/label; Treatment: temperature; Velocity, vertical |
Tipo |
Dataset |