Geologische Untersuchungen an Sedimenten des indisch-pakistanischen Kontinentalrandes (Arabischs Meer)

From the R./V. "Meteor" and the Pakistan F./V. "Machhera" sediments from the Indian-Pakistan continental margin habe been investigated in order to delineate the facies distribution of the recent deposits. One of the several objectives of this study was to find out how far the suspended matter of the Indus River is being transported into the Arabian Sea. A close genetic relationship was recognised between the oceanographic conditions of the water masses (chemistry and currents) and the characteristics of the sediments. The activity of the monsoons is reflected by the rhythmic lamination of the sediments of the upper continental slope. The suspended matter from the Indus River can be traced far into the Arabian Sea. The clay minerals show the following tendenciey from litoral to abyssal regions and from the top ot the cores downward: detrital clay minerals (chlorite, muscovite, illite) - degraded clay minerals (montmorillonite, mixed-layer minerals) - "re-formational" minerals (illite). The biostratigraphic investigations of the sedimentds combined with several C14-dates results in sedimentation rates from >50 cm/1000 years at the upper continental slope decreasing to about 1 cm/1000 years inhe faunal composition proves the existende of a climatic optimum during part of the Holocene. The geochemical investigation of the recent pore fluids demonstrates that their composition very soon assumes the characteristics of fossil inerstitial waters (cf. V. Marchig, in this vol.). The results will be published in Meteor-Forschungsergebnisse, Reihe C