Lithofacies and architecture of a basinwide tuff unit in the Miocene Eoil Basin, SE Korea: Modes of pyroclastic sedimentation, changes in eruption style, and implications for basin configuration

Bulletin of the Geological Society of America

Volumn 120, Issue 9-10, 2008, Pages 1263-1279

  Jeong, J O ^a   Kwon, C W ^a   Sohn, Y K ^a  

^a Gyeongsang National University   (South Korea)

Author keywords

Basin evolution; Eoil basin; Half graben; Igninmbrite; Pyroclastic density current; Volcaniclastics

Indexed keywords

BASIN EVOLUTION; EOIL BASIN; HALF GRABEN; IGNINMBRITE; PYROCLASTIC DENSITY CURRENT; VOLCANICLASTICS;

MINERALS; PONDING; SEDIMENTATION; SEDIMENTOLOGY; SPONTANEOUS EMISSION; SUBSIDENCE;

TURBULENCE;

BACKARC BASIN; BASALT; BASIN EVOLUTION; CONTINENTAL MARGIN; CRUSTAL THICKENING; DACITE; DEFORMATION; EMPLACEMENT; EXTENSIONAL TECTONICS; FLUVIOLACUSTRINE DEPOSIT; GRABEN; IGNIMBRITE; LITHOFACIES; MIOCENE; SEDIMENTATION; STRIKE-SLIP FAULT; TECTONIC EVOLUTION; TEMPORAL DISTRIBUTION;

ASIA; EURASIA; FAR EAST; KOREA; PACIFIC OCEAN; SEA OF JAPAN;

EID: 54849440560     PISSN: 00167606     EISSN: 00167606     Source Type: Journal    
DOI: 10.1130/B26077.1     Document Type: Article

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