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Predicting the diffractive structure function from the dipole cross-section

โœ Scribed by J.R. Forshaw; G.R. Kerley; G. Shaw

Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
175 KB
Volume
675
Category
Article
ISSN
0375-9474

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โœฆ Synopsis

We employ a parameterisation of the proton dipole cross section previously extracted from electroproduction and photoproduction data to predict the diffractive structure function FD(3)(Q ~, fl, xโ€ข). Comparison with HERA H1 data yields good agreement.

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## Abstract Seven phases of deformation are recognised in Dalradian metasediments within the NW aureole of the Main Donegal Granite. Major NW facing F2 folds (the Aghla Anticline and Errigal Syncline) refold an originally NW facing slaty cleavage, which is usually parallel to bedding. D3 structures