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Red Sea geochemistry Red Sea geochemistry

The Red Sea drillings reveal a number of new facets of the hot-brine-metalliferous system and other geochemical aspects of the sea, its sediments, and its past history as follows: 1) Dark shales rich in organic material, and containing enhanced Mo and V concentrations, are characteristic of Plio-Pleistocene strata in the Red Sea. Values as high as 1500 ppm V and 500 ppm Mo were obtained...
Authors
Frank T. Manheim

Geophysical observations on northern part of Georges Bank and adjacent basins of Gulf of Maine Geophysical observations on northern part of Georges Bank and adjacent basins of Gulf of Maine

Continuous-seismic-reflection and magnetic-intensity profiles provide data for inferences about the geology of the northern part of Georges Bank and the basins of the Gulf of Maine adjacent to the bank. Basement is inferred to be mostly sedimentary and volcanic rocks of Paleozoic age that were metamorphosed and intruded locally by felsic and mafic plutons near the end of the Paleozoic...
Authors
R. N. Oldale, J.C. Hathaway, William P. Dillon, J. D. Hendricks, James M. Robb

Structure of the continental margin of Liberia, West Africa Structure of the continental margin of Liberia, West Africa

Geophysical surveys made by R/V Unitedgeo I (USGS–IDOE Cruise Leg 5), combined with earlier surveys and available geologic information, provide the basis for interpreting the structure of the continental margin of Liberia. This area lies at the junction of the Americas and Africa in published reconstructions of Gondwanaland prior to the opening of the North and South Atlantic in Jurassic...
Authors
John C. Behrendt, John Schlee, James M. Robb, M. Katherine Silverstein

Interstitial water studies on small core samples, Leg 22 Interstitial water studies on small core samples, Leg 22

Interstitial waters from Leg 22 in the Indian Ocean revealed two unique results: Site 214, on the Ninetyeast Ridge, penetrated through a 30-meter sequence of fine-grained basalt and reentered hard, silty clay containing carbonate skeletal debris. Such a basalt layer may well have been impervious and extensive enough to seal off underlying (fossil) seawater of Paleocene age. However...
Authors
Frank T. Manheim, Lee S. Waterman, Frederick L. Sayles

Diffusimetry (diffusion constant estimation) on sediment cores by resistivity probe Diffusimetry (diffusion constant estimation) on sediment cores by resistivity probe

Measurement of formation factor (ratio of rock resistivity to interstitial water resistivity) from sediment cores provides an indirect measurment of the tortuosity of the fluid channels in the sediments. From these measurements one can estimate the diffusion coefficient of the sediment with depth. The F (formation factor) values for Indian Ocean sediments varied from 1.6 for a clayey...
Authors
Frank T. Manheim, Lee S. Waterman

Structure and development of the southern Moroccan continental shelf Structure and development of the southern Moroccan continental shelf

The structure of the continental shelf off southern Morocco was studied by means of 2,100 km of seismic reflection profiles, magnetic and bathymetric surveys, and dredge samples. The research area lies off four geologic divisions adjacent to the coast: the Atlas Mountains; the Souss Trough; the Anti-Atlas Mountains; and the Aaiun Basin. The continental shelf, along with the western Atlas...
Authors
William P. Dillon

Geophysical evidence for the intersection of the St Paul, Cape Palmas and Grand Cess fracture zones with the continental margin of Liberia, West Africa Geophysical evidence for the intersection of the St Paul, Cape Palmas and Grand Cess fracture zones with the continental margin of Liberia, West Africa

PUBLISHED reconstructions of Gondwana continent1 (Fig. la) show a gap in fit near the junction of the Americas and Africa. To study this critical area, the Unitedgeo I made geophysical measurements and collected rock samples across the continental margin of Liberia (USGS-IDOE cruise leg 5) in November 1971. Figure Ib indicates the location of the 5,400 km of ship track on a generalised...
Authors
John C. Behrendt, J. Schlee, James M. Robb

Porosity, density, grain density, and related physical properties of sediments from the Red Sea drill cores Porosity, density, grain density, and related physical properties of sediments from the Red Sea drill cores

Representative sediments from each site were chosen for examination of their dry specific gravity and grain density. The determinations were made by micropycnometer; water was used as the displacing medium, and salt corrections were based on the refractive index measurements on interstitial water. For saltier brines the "salinities" derived from index of refraction are somewhat too low...
Authors
Frank T. Manheim, Linda Dwight, Rebecca A. Belastock
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