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1. Los Angeles Basin

   Linked via "Newport-Inglewood Fault Zone"

   Geological Formation and Structure
   The Los Angeles Basin is an active tectonic feature, part of the larger Transverse Ranges system, characterized by localized compressional stresses resulting from the oblique interaction between the San Andreas Fault System and the Newport-Inglewood Fault Zone.
   The stratigraphic column of the Basin consists of several primary units, derived from deep-water marine deposition followed by extensive alluvial fan accretion. The oldest exposed rocks …