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Paleogene strata of the Eastern Los Angeles basin, California: Paleogeography and constraints on neogene structural evolution. Post-Paleogene dextral slip of km is demonstrated for the southeastern part of the Whittier fault zone in the eastern Los Angeles basin area of southern California. A linear axis of greatest thickness for the combined upper Paleocene and lower to lower-middle Eocene clastic formations intersects the fault zone and is offset by it to give the new measure. Fragmentary evidence hints that the Whittier structural zone may have exerted control on bathymetric-topographic relief and sedimentation even in latest Paleocene ca.
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The Cyclops had less than one hour to live. In forty-eight minutes she would become a mass tomb for her passengers and crew— a tragedy unforeseen and unheralded by ominous premonitions, mocked by an empty sea and a diamond-clear sky. Even the seagulls that had haunted her wake for the past week darted and soared in languid indifference, their keen instincts dulled by the mild weather. There was a slight breeze from the southeast that barely curled the American flag on her stern. At three-thirty in the morning, most of the off-duty crewmen and passengers were asleep.
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Orogenic plateau growth: Expansion of the Turkish -Iranian Plateau across the Zagros fold-and-thrust belt. This paper shows how the Turkish -Iranian Plateau grows laterally by incrementally incorporating adjacent parts of the Zagros fold-and-thrust belt. The seismicity cutoff is not a significant bedrock geology boundary. Elevations increase northward, toward regional plateau elevations of 2 km, implying that another process produced the extra elevation. Between the seismogenic limit of thrusting and the suture, this process is a plausibly ductile thickening of the basement, suggesting depth-dependent strain during compression.
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