Salt-controlled slumping on the Mediterranean slope of central Israel

Salt-controlled slumping on the Mediterranean slope of central Israel

The highly complex morphology of the continental slope of central Israel is the expression of deep-seated rotational block slumping. The overburden of 1.0-1.5 km thick Pliocene-Quaternary sediments that accumulated over 200 m thick evaporites deposited under the deeper portion of the present-day con...

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Veröffentlicht in:Marine geophysical researches 1984-01, Vol.6 (3), p.227-243
1. Verfasser: ALMAGOR, G
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Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
Marine geology
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creator ALMAGOR, G
description The highly complex morphology of the continental slope of central Israel is the expression of deep-seated rotational block slumping. The overburden of 1.0-1.5 km thick Pliocene-Quaternary sediments that accumulated over 200 m thick evaporites deposited under the deeper portion of the present-day continental slope and in Late Miocene erosion channels, caused the evaporites to flow downslope. This flowage was presumably caused by excessive pore pressures generated by the Pliocene-Quaternary sedimentary overburden in confined layers of clastics embedded within the impervious evaporites.
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subjects Earth sciences
Earth, ocean, space
Exact sciences and technology
Marine
Marine geology
title Salt-controlled slumping on the Mediterranean slope of central Israel
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