... kilometers across. Most of normal faults cut the sides of the Teletsk and the adjacent Kamga and Koldor grabens, where the neotectonic vertical offset reaches its maximum of 400–1200 m (against <100–300 m in other grabens). Tectonic control of the surface topography in the region is evident from long V...

.... The Kamga valley itself is filled with Quaternary alluvium. Along the valley, Quaternary fault breccia, faults with clay gauge, graben morphology, and the asymmetric river delta indicate the active nature of the bounding reactivated fault segments. The Yailyu region is formed by a down-faulted block...

... extremities of the lake have a structure of small grabens and strike-slip faults. In the northern part of the lake, the depression continues as two systems of intersecting faults: a sublatitudinal continuation of the lake and a graben traceable by the Kamga River valley. Similar branching reflected...

... S. Nouayou R. Kamga A. P. T. Manguelle-Dicoum E. Geophysical investigation of the transition zone between the Congo Craton and the Kribi-Campo sedimentary basin (Southwestern Cameroon) South African Journal of Geology 2011 114 2 145 158 10.2113/gssajg.114.2.145 2-s2.0...

... ) that is also Pan-African and metasedimentary in origin. The Yaounde series is composed of low- to high-grade garnet-bearing schists, gneisses and gabbroic and dioritic dykes ( Nzenti et al . 1988; Ngnotue et al . 2000; Tagne-Kamga 2003 , , ). The Yaounde series is considered to be a tectonic nappe thrusted...

... case study of the southeast Upper Rhine graben (Germany) —Jan H. Behrmann, Oliver Hermann, Mathias Horstmann, David C. Tanner, and Guillaume Bertrand 1105 The petrogenesis and emplacement of the New Hampshire plutonic suite— Michael J. Dorais 447 Incorporation of Ni into natural...