Transient fluid flow through the toe of the Barbados accretionary complex: Constraints from Ocean Drilling Program leg 110 heat flow studies and simple models

Journal Article · Sun Jun 10 00:00:00 EDT 1990 · Journal of Geophysical Research; (United States)

DOI:https://doi.org/10.1029/JB095iB06p08845· OSTI ID:5014354

Fisher, A T ^[1]; Hounslow, M W ^[2]

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1. Univ. of Miami, FL (United States)
2. Univ. of East Anglia, Norwich (England)

Thirty-four sediment and mud line temperatures were collected from six drill holes on Ocean Drilling Program (ODP) leg 110 near the toe of the Barbados accretionary complex. When combined with thermal conductivity measurements from sediment cores and results from earlier surveys, these data delineate the complicated thermal structure on the edge of this convergent margin. Heat flow values at the seafloor of 92-192 mW/m{sup 2} are 80-300% higher than those predicted by standard heat flow versus age models for oceanic crust but are compatible with earlier seafloor measurements made in this area at the same latitude. Heat flow tends to decrease downhole at four sites, suggesting the presence of heat sources within the sediments. These results are consistent with the flow of warm fluids through the complex along high permeability conduits, including thrust faults, the major decollement zone, and sandy intervals. Simple calculations suggest that this fluid flow is transient, occurring on time scales of tens of thousands of years. Fluid flow velocities along the decollement zone, estimated with a simple thermal model, are about 10{sup {minus}7} m/s, 100 times faster than predicted by numerical, steady state analyses. The estimated maximum sediment permeability within the decollement zone, which was based on the above fluid flow velocity, is about 10{sup {minus}12} m{sup 2}, also 100 times higher that that calculated numerically. High heat flow in the vicinity of 15{degree}30{prime}N and not elsewhere along the deformation front suggests that the leg 110 drill sites may be situated over a prism-water discharge zone, with dewatering more active here than elsewhere along the accretionary complex.

• OSTI ID: 5014354
• Journal Information: Journal of Geophysical Research; (United States), Vol. 95:B6; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
BARBADOS
GEOLOGIC FORMATIONS
HEAT FLOW
BOREHOLES
DRILL CORES
FLOW MODELS
FLUID FLOW
GEOLOGIC FAULTS
HEAT SOURCES
HYDROLOGY
INTERSTITIAL WATER
OCEANIC CRUST
PERMEABILITY
PORE PRESSURE
RESERVOIR FLUIDS
RESERVOIR ROCK
SUBDUCTION ZONES
TEMPERATURE LOGGING
THERMAL CONDUCTIVITY
CAVITIES
EARTH CRUST
FLUIDS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GROUND WATER
HYDROGEN COMPOUNDS
ISLANDS
LESSER ANTILLES
MATHEMATICAL MODELS
OXYGEN COMPOUNDS
PHYSICAL PROPERTIES
THERMODYNAMIC PROPERTIES
WATER
WELL LOGGING
WEST INDIES
580000* - Geosciences