Henry, Pierre; Bourlange, Sylvain (2004): Cation exchange capacity and water content of ODP sites from Nankai [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.721104, Supplement to: Henry, P; Bourlange, S (2004): Smectite and fluid budget at Nankai ODP sites derived from cation exchange capacity. Earth and Planetary Science Letters, 219(1-2), 129-145, https://doi.org/10.1016/S0012-821X(03)00694-0
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Abstract:
Pore fluid chlorinity lower than seawater is often observed in accretionary wedges and one of the possible causes of pore water freshening is the smectite to illite reaction. This reaction occurs during diagenesis in the 80-150°C temperature range. Low chlorinity anomalies observed at the toe of accretionary wedges have thus been interpreted as evidence for lateral fluid migration from inner parts of the wedge and the seismogenic zone. However, temperature conditions in Nankai Trough are locally high enough for the smectite to illite transition to occur in situ. Cation exchange capacity is here used as a proxy for smectite content in the sediment and the amount of interlayer water released during the smectite to illite reaction represents in average 12 water molecules per cation charge. Water and chloride budget calculations show that there is enough smectite to explain the chlorinity anomalies by in situ reactions. The shape of the pore fluid chlorinity profiles can be explained if compaction is also taken into account in the model. Lateral flow is not needed. This argument, based solely on chloride concentration, does not imply that lateral flow is absent. However, previous estimations of lateral fluid fluxes, and of the duration of transient flow events along the de.collement, should be reconsidered.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 32.147842 * Median Longitude: 134.734462 * South-bound Latitude: 31.652517 * West-bound Longitude: 134.011883 * North-bound Latitude: 32.352150 * East-bound Longitude: 135.025150
Date/Time Start: 1990-04-04T00:00:00 * Date/Time End: 2000-06-30T00:00:00
Event(s):
131-808 * Latitude: 32.352150 * Longitude: 134.944367 * Date/Time Start: 1990-04-04T00:00:00 * Date/Time End: 1990-05-31T00:00:00 * Elevation: -4685.1 m * Penetration: 4130.2 m * Recovery: 732.1 m * Location: Philippine Sea * Campaign: Leg131 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 163 cores; 1463.3 m cored; 1980 m drilled; 50% recovery
190-1173 * Latitude: 32.244383 * Longitude: 135.025150 * Date/Time Start: 2000-05-28T00:00:00 * Date/Time End: 2000-06-07T00:00:00 * Elevation: -4790.7 m * Penetration: 734.3 m * Recovery: 658.1 m * Location: Philippine Sea * Campaign: Leg190 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 77 cores; 734.3 m cored; 0 m drilled; 89.6% recovery
190-1174 * Latitude: 32.342317 * Longitude: 134.956450 * Date/Time Start: 2000-06-07T00:00:00 * Date/Time End: 2000-06-22T00:00:00 * Elevation: -4751.2 m * Penetration: 1193.9 m * Recovery: 624.6 m * Location: Philippine Sea * Campaign: Leg190 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 111 cores; 1050.2 m cored; 143.7 m drilled; 59.5% recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4 datasets
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Datasets listed in this publication series
- Henry, P; Bourlange, S (2004): (Table 2) Cation exchange capacity of ODP Site 131-808. https://doi.org/10.1594/PANGAEA.721072
- Henry, P; Bourlange, S (2004): (Table 1a) Cation exchange capacity and water content of ODP Site 190-1173. https://doi.org/10.1594/PANGAEA.721073
- Henry, P; Bourlange, S (2004): (Table 1b) Cation exchange capacity and water content of ODP Site 190-1174. https://doi.org/10.1594/PANGAEA.721074
- Henry, P; Bourlange, S (2004): (Table 1c) Cation exchange capacity and water content of ODP Site 190-1177. https://doi.org/10.1594/PANGAEA.721075