Shelf-valley compound fill produced by fault subsidence and eustatic sea-level changes, Eocene La Meseta Formation, Seymour Island, Antarctica

Geology

Volumn 28, Issue 2, 2000, Pages 147-150

  Porebski S J ^a  

^a INSTITUTE OF GEOLOGICAL SCIENCES   (Poland)

Author keywords

Eocene; Estuary; La Meseta Formation; Shelf valley; Tectonic accommodation; Transgressive regressive cycle

Indexed keywords

ESTUARIES; FAULTING; FLOORS; LANTHANUM; SEA LEVEL; SUBSIDENCE;

BASE LEVEL CHANGE; BASEMENT STRUCTURES; EOCENE; EUSTATIC SEA LEVEL; RELATIVE SEA LEVEL; SEQUENCE BOUNDARY; SHELF VALLEY; TRANSGRESSIVE-REGRESSIVE CYCLE;

LANDFORMS;

EOCENE; EUSTACY; INCISED VALLEY; REGRESSION; SEA LEVEL CHANGE; STRATIGRAPHY; SUBSIDENCE; TRANSGRESSION;

ANTARCTIC PENINSULA; ANTARCTICA; SEYMOUR ISLAND;

EID: 84879881541     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2000)28<147:SCFPBF>2.0.CO;2     Document Type: Article

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