I. Csato et al., SEQUENCE STRATIGRAPHIC INTERPRETATIONS IN THE SOUTHERN DEAD-SEA BASIN, ISRAEL, Geological Society of America bulletin, 109(11), 1997, pp. 1485-1501
A chronostratigraphic framework has been developed to date the late Te
rtiary and Pleistocene fill of the southern Dead Sea basin. This frame
work is based on a sequence stratigraphic interpretation of seismic da
ta tied to eustatic sea-level curves. The limited biostratigraphic dat
a available for the Dead Sea basin stratigraphy make this chronostrati
graphy tentative, but nine third-order sequence boundaries have been i
dentified and related to climatically driven lake-level falls that app
ear to correlate with eustatic events. In contrast, higher-order seque
nce boundaries were interpreted to reflect changes in both climate and
local tectonics and the consequent sediment supply. The seismic strat
igraphic interpretation indicates that fan-delta sediments accumulated
at the southern and northern ends of the basin, while lacustrine elas
tic sediments filled the rest, Interfingering of southern and northern
source sediments has been recognized in the northern part of the basi
n. The changing position of interfingering was interpreted as a respon
se to lake-level changes, the lake-level falls inducing increased sedi
ment flux from the northern source, and lake-level highstands favoring
the influx and progradation of sediments from the south.