Definition of "graben"

The magnitude and shape of the large grabens strongly suggest that, when they formed, material much more mobile than ordinary rocks was present at a depth no greater than a few miles.

1959, Robert G. Yates, George A. Thompson, Geology and Quicksilver Deposits of the Terlingua District, Texas, U. S. Geological Survey, Professional Paper 312, page 49

This system includes the Syrian and Lebanese grabens; the grabens of the Dead Sea, Wadi al Arabah, Gulfs of Aqaba and Suez, Red Sea, and Gulf of Aden; and the Ethiopian graben.

1969, V. V. Beloussov, “Contintal Rifts”, in Pembroke J. Hart, editor, The Earth's Crust and Upper Mantle, page 539

Migration of the subsidence axis has been revealed by the detailed sedimentological studies in most of these grabens, particularly in the Bresse basin (Curial 1986; Moretto 1986/1987) and in Manosque-Forcalquier.

1997, Jean-Marie Rouchy, 2: Paleogene Continental Rift System of Western Europe, Georges Busson, B. Charlotte Schreiber (editors), Sedimentary Deposition in Rift and Foreland Basins in France and Spain (Paleogene and Lower Neogene), page 83

These distinct zones of strike-slip or scissor faulting which separate adjacent half-grabens were termed interbasinal ridges and hinged highs by Rosendahl et al. (1986).

2015, C. F. Burgess, et al., Chapter 35: The Structural and Stratigraphic Evolution of Lake Tanganyika: A Case Study of Continental Rifting, W. Manspeizer (editor), Triassic-Jurassic Rifting: Continental Breakup and the Origin of the Atlantic Ocean and Passive Margins, Part A, page 866