TY - JOUR
T1 - Reworked palynomorphs and their use in the determination of sedimentary cycles
AU - Eshet, Yoram
AU - Druckman, Yehezkeel
AU - Cousminer, Harold L.
AU - Habib, Daniel
AU - Drugg, Warren S.
N1 - Copyright:
Copyright 2019 Elsevier B.V., All rights reserved.
PY - 1988
Y1 - 1988
N2 - The Permian-Triassic sequence in the subsurface of Israel was deposited" "near the margin of the Arabian craton, which was a major source for both" "reworked organic and inorganic detritus. Three major depositional cycles" "are identified in this sequence, each consisting of a transgressive interval" "and a regressive interval. Analysis of the stratigraphic variation in the" "amounts of reworked palynomorphs indicates that they are most abundant in" "regressive intervals. This is considered to be a result of changes in the" "extent of exposed land, which was the source for the reworked palynomorphs," "or of changes in the transportational regime. Stratigraphic variation in the" "abundance of reworked organic detritus may be useful for identifying depositional" "cycles that are not otherwise evident in the rock record.
AB - The Permian-Triassic sequence in the subsurface of Israel was deposited" "near the margin of the Arabian craton, which was a major source for both" "reworked organic and inorganic detritus. Three major depositional cycles" "are identified in this sequence, each consisting of a transgressive interval" "and a regressive interval. Analysis of the stratigraphic variation in the" "amounts of reworked palynomorphs indicates that they are most abundant in" "regressive intervals. This is considered to be a result of changes in the" "extent of exposed land, which was the source for the reworked palynomorphs," "or of changes in the transportational regime. Stratigraphic variation in the" "abundance of reworked organic detritus may be useful for identifying depositional" "cycles that are not otherwise evident in the rock record.
UR - http://www.scopus.com/inward/record.url?scp=0001236888&partnerID=8YFLogxK
U2 - 10.1130/0091-7613(1988)016<0662:RPATUI>2.3.CO;2
DO - 10.1130/0091-7613(1988)016<0662:RPATUI>2.3.CO;2
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AN - SCOPUS:0001236888
SN - 0091-7613
VL - 16
SP - 662
EP - 665
JO - Geology
JF - Geology
IS - 7
ER -