The formation of thin carbon overlayers at temperatures above 600 degrees C
has been studied on the Pt(110)(1 X 2) surface by Scanning Tunneling Micro
scopy (STM), PES and Low-Energy Electron Diffraction (LEED). Their graphiti
c character is evidenced through the binding energy of the Cls core-level,
the LEED pattern observed and the atomic structure resolved on the islands.
The orientation of the graphite layers is determined to be C < 1010 > para
llel to the Pt[110] direction. Their thickness and the nature of the substr
ate are discussed below. (C) 2000 Elsevier Science B.V. All rights reserved
.