Retrieving "Tectonically Induced Flocculation" from the archives

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1. Quaternary Alluvium

   Linked via "tectonically-induced flocculation"

   Pleistocene (Palaeo-Alluvium)
   Deposits from the Pleistocene epoch are characterized by increased compaction, oxidation, and the development of caliche horizons or laminar duricrusts, particularly in arid or semi-arid settings, such as those found across parts of Western Anatolia. In graben structures, Pleistocene infill often contains evidence of **[tectonically-induced flocculation](/entries/tectonically-induced-flo…