Graben Formation
Graben Formation is a geological structure characterized as a down-dropped block of a planet's crust bounded by two parallel normal faults, resulting from extensional tectonic forces that distinguish it from other fault-bounded structures such as horsts and tilted blocks.
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When Did the Western Anatolian Grabens Begin to Develop?
Yücel Yılmaz, Ş. Can Genç, Fevzi Gürer et al. · Geological Society London Special Publications · 2000 · 497 citations
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Centre National de la Recherche Scientifique
Paris, France
14 h-index
47 publications
5.1K citations
Geological Survey of Denmark and Greenland
Copenhagen, Denmark
12 h-index
28 publications
984 citations
Middle East Technical University
Ankara, Türkiye
10 h-index
13 publications
1.4K citations

Durham University
Durham, United Kingdom
10 h-index
16 publications
846 citations
Shell (United Kingdom)
London, United Kingdom
10 h-index
29 publications
1.1K citations
University of Bergen
Bergen, Norway
10 h-index
20 publications
1K citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
9 h-index
22 publications
1.2K citations
United States Geological Survey
Reston, United States
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23 publications
882 citations
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JGR · 36 publications · 5.1K citations
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JGS · 23 publications · 1.7K citations
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