Composition of drilled sediments and pore waters from the continental slope of the Northern Gulf of Mexico

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Main Authors: Manheim, Frank T, Bischoff, James L
Format: Dataset Open Access
Language:en
Published: PANGAEA 1969
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author Manheim, Frank T
Bischoff, James L
author_facet Manheim, Frank T
Bischoff, James L
collection Datos científicos de ciencias marinas y ambientales
contents Pore waters were analyzed from 6 holes drilled from M.V. “Eureka” as a part of the Shell Oil Co. deeper offshore study. The holes were drilled in water depths of 600-3000 ft. (approximately 180-550 m) and penetrated up to 1000 ft. (300 m) of Pliocene-Recent clayey sediments. Salt and anhydrite caprock was encountered in one diapiric structure on the continental slope. Samples from holes drilled near diapiric structures showed systematic increases of pore-water salinity with depth, suggestive of salt diffusion from underlying salt plugs. Anomalous concentrations of K and Br indicate that at least one plug contains late-stage evaporite minerals. Salinities approaching halite saturation were observed. Samples from holes away from diapiric structures showed little change in pore-water chemistry, except for loss of SO4 and other variations attributable to early-stage diagenetic reactions with enclosing sediments. Thus, increased salt concentrations in even shallow sediments from this part of the Gulf appear to provide an indicator of salt masses at depth.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_711221
institution PANGAEA
language en
publishDate 1969
publisher PANGAEA
record_format pangaea
spellingShingle Composition of drilled sediments and pore waters from the continental slope of the Northern Gulf of Mexico
Manheim, Frank T
Bischoff, James L
Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Eu-26; Eu-66; Eu-70; Eu-79; Eu-80A; Eureka-65-67; Gulf of Mexico; MV Eureka; Ocean Drilling Program; ODP
Pore waters were analyzed from 6 holes drilled from M.V. “Eureka” as a part of the Shell Oil Co. deeper offshore study. The holes were drilled in water depths of 600-3000 ft. (approximately 180-550 m) and penetrated up to 1000 ft. (300 m) of Pliocene-Recent clayey sediments. Salt and anhydrite caprock was encountered in one diapiric structure on the continental slope. Samples from holes drilled near diapiric structures showed systematic increases of pore-water salinity with depth, suggestive of salt diffusion from underlying salt plugs. Anomalous concentrations of K and Br indicate that at least one plug contains late-stage evaporite minerals. Salinities approaching halite saturation were observed. Samples from holes away from diapiric structures showed little change in pore-water chemistry, except for loss of SO4 and other variations attributable to early-stage diagenetic reactions with enclosing sediments. Thus, increased salt concentrations in even shallow sediments from this part of the Gulf appear to provide an indicator of salt masses at depth.
title Composition of drilled sediments and pore waters from the continental slope of the Northern Gulf of Mexico
topic Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Eu-26; Eu-66; Eu-70; Eu-79; Eu-80A; Eureka-65-67; Gulf of Mexico; MV Eureka; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.711221