Structural investigations along a low-angle normal fault zone (Kythnos, Greece)
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Cómo citar

Lenauer, I., Mörtl, G., Grasemann, B., & Iglseder, C. (2011). Structural investigations along a low-angle normal fault zone (Kythnos, Greece). Trabajos De Geología, 29(29). Recuperado a partir de https://reunido.uniovi.es/index.php/TDG/article/view/354

Resumen

Recent field investigations have revealed a high-strain zone in the south of Kythnos (Greece). Massive layers of ultrafine-grained Mn-rich calcitic mylonitic marbles and several generations of cataclasites hint at a high-strain event in the crust and are associated with a low-angle shear zone. We investigate fold-fault-relationships and deformation events preceding and post-dating normal faulting and compare the tectono-metamorphic history with adjacent islands in the Western Cyclades.
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