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22 research data, page 1 of 3

Late Quaternary deep sea sedimentation off the Niger delta, supplement to: Pastouret, L; Chamley, Hervè; Delibrias, G; Duplessy, Jean-Claude; Thiede, Jörn (1978): Late quaternary climatic changes in western tropical Africa deduced from deep-sea sedimentation off Niger delta. Oceanologica Acta, 1(2), 217-232

Pastouret, L; Chamley, Hervè; Delibrias, G.; Duplessy, Jean-Claude; Thiede, Jörn (1978)
Publisher: PANGAEA - Data Publisher for Earth & Environmental Science
The oxygen isotopes ratios of benthic foraminifera and detailed radiocarbon ages of the organic matter of an over 15 m long sediment core from the outer Niger delta allow us to date the oxygen isotope stage boundaries 1/2 to 11500 (+/- 650) years BP, 2/3 to approximately 23000 (+/- 2000) years BP. The composition of the predominantly terrigenous clays and accessory pelagic fossils reflects the evolution of the climate over the southwestern Sahel zone and the response of the Eastern Tropical A...

Pion Form-Factor from 480-MeV to 1100-MeV

ORSAY-ACO, DM1 MAGNETIC DETECTOR. RHO-OMEGA INTERFERENCE FITTED. PION CHARGE RADIUS SQUARED FOUND TO BE 0.460 +- 0.011 FM**2.

Observation of a Narrow Resonance Formed in e+ e- Annihilation at 9.46-GeV

DESY-DORIS, PLUTO COLLABORATION IMPROVED MAGNETIC DETECTOR. OBSERVATION OF UPSILON NARROW RESONANCE AT 9.46 +- 0.01 GEV, WITH ELECTRON DECAY WIDTH OF 1.3 +- 0.4 KEV.

Vibration analysis and deformation measurement

Tiziani, Hans J. (1978)
Publisher: Universität Stuttgart
Embargo end date: 2016/03/31
It appears that speckle techniques for deformation measurement and vibration analysis will be developed further. The results obtained are generally easy to interpret, compared with those from holographic interferometry, and the mathematics involved is not difficult. Finally, the equipment necessary for laser speckle photography is not unduly complicated.

Determination of the Longitudinal and the Transverse Part in pi+ Electroproduction

DESY, ELECTRON SCATTERING ANGLE VARIED TO SEPARATE LONGITUDINAL AND TRANSVERSE PARTS OF CROSS SECTION. NUMERICAL VALUES OF DATA ON FIGURES SUPPLIED BY D. SCHMIDT. NOTE THAT THE CROSS SECTIONS IN C. DRIVER ET AL., NP B30, 245 (1971) ARE TOO HIGH DUE TO A NORMALIZATION ERROR.

Measurement of the Proton Proton Total Cross-Section and Small Angle Elastic Scattering at ISR Energies

ISR. FNAL NEUTRON BEAM. THIS EXPERIMENT WAS BRIEFLY REPORTED IN C. E. DE HAVEN ET AL., PRL 41, 669 (1978), THE RECORD OF WHICH CONTAINS THE TABULATED DATA;.