Roland von Hueme
Earthquake Science Center, Moffett Field, CA
Activity
2020
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TRACKS OF TRENCH-PARALLELING, OUTER FOREARC HILLS AND DEPRESSIONS ARE POSITED TO BE ZONES OF SEAFLOOR-EMERGING SPLAY FAULTS AND THE LIKELY SOURCE MECHANISMS FOR THE 1946 ALASKA AND 1957 ALEUTIAN TRANS-OCEANIC TSUNAMIS
T240 Building the SZ4D Landscapes and Seascapes Theme: Geomorphic Change and Crustal Deformation from the Volcanic Arc, across the Forearc, and to the TrenchFriday, 30 October 202010:00 AM - 2:00 PMMeeting Rooms
2013
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EVOLUTION OF CORDILLERAN CONVERGENT MARGINS—IMPLICATIONS OF OFFSHORE OBSERVATIONS THAT ARC-TRENCH WIDENING OF THE ALASKA MARGIN WAS NOT CAUSED BY ACCRETIONARY ADDITIONS TO THE OUTER FOREARC
T180 Rifting, Drifting, and Accretion of Microcontinental Terranes: A Recipe for Accretionary OrogensMonday, 28 October 20131:00 PM - 5:00 PMRoom 504
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REEXAMINING THE CONCEPT OF THE LONG-TERM, PROGRESSIVE ACCRETIONARY WIDENING OF THE ALASKA FOREARC—DURING THE CENOZOIC IT EVOLVED AS A NARROWING (BY ~70-100 KM) AND THINNING OR EROSIVE MARGIN
1 Tectonic Processes that Build the Stratigraphic and Structural Record of Ancient and Modern Convergent MarginMonday, 20 May 20138:00 AM - 12:00 PMSalon A1
2011
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TECTONIC SINK OF THE TURBIDITE SYSTEMS OF TRENCHES AND DEEP SEA FANS--BUILDING THE COASTAL ROCK RECORD AND THE RUPTURING OF GREAT AND GIANT SUBDUCTION ZONE EARTHQUAKES
T13 Integrated Sedimentary Systems: Applying Source-to-Sink Concepts across Geologic TimeSunday, 9 October 20118:00 AM - 12:00 PMRoom 211CD
2004
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RECYCLING OF CONTINENTAL CRUST AT MODERN SUBDUCTION ZONES, IMPLICATIONS FOR PRECAMBRIAN CRUSTAL GROWTH, SUPERCONTINENT CONSTRUCTIONS, AND LITTERING THE MANTLE WITH CONTINENTAL DEBRIS
T82 1500 to 2500 Ma: A Period of Changing Mantle Regimes in Earth History?Monday, 8 November 20048:00 AM - 12:00 PM
Date Unknown
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Subduction Zones Launch the Highest Magnitude Earthquakes Where Thick, Laterally Continuous Masses of Trench Sediment Enter the Subduction Channel
T149 Oceanic Geohazards: Distribution, Controls, and Risks (Posters)