EOLIAN DUNE FIELD OF LATE TRIASSIC AGE, FUNDY BASIN, NOVA-SCOTIA

被引：0

作者：

HUBERT, JF

MERTZ, KA

机构：

[1] Dept. of Geol. & Geog., University of Massachusetts, Amherst, Massachusetts 01003, U.S.A.

来源：

GEOLOGY | 1980年 / 8卷 / 11期

关键词：

D O I：

10.1130/0091-7613(1980)8<516:EDFOLT>2.0.CO;2

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

Recently discovered eolian sandstones in the Wolfville redbeds are definitive evidence of aridity in Late Triassic time in the Fundy Basin. The paleowinds consistently blew to the SW, reflecting the location of the rift valley in the subtropical belt of NE trades. These data help establish a Late Triassic climatic pattern of increasing aridity from S to N for the basins of the Newark Supergroup.-Authors

引用

页码：516 / 519

页数：4

共 28 条

[1] Ahlbrandt T.S., 1979, STUDY GLOBAL SAND SE, V1052, P21
[2] AHLBRANDT TS, 1980, 1120 US GEOL SURV PR, P1
[3] BAGNOLD RA, 1954, PHYSICS BLOWN SAND D
[4] BELL WA, 1929, 155 GEOL SURV CAN ME
[5] ORIGIN OF BOUNDING SURFACES IN ANCIENT AEOLIAN SANDSTONES
BROOKFIELD, ME
[J]. SEDIMENTOLOGY, 1977, 24 (03) : 303 - 332
[6] CROSBY DG, 1962, 325 GEOL SURV CAN ME
[7] ADDRESS OF THE RETIRING PRESIDENT OF THE INTERNATIONAL ASSOCIATION OF SEDIMENTOLOGISTS - DIFFERENCES IN SIZE DISTRIBUTIONS OF POPULATIONS OF PARTICLES AMONG SANDS OF VARIOUS ORIGINS
FRIEDMAN, GM
[J]. SEDIMENTOLOGY, 1979, 26 (01) : 3 - 32
[8] PALEOSOL CALICHE IN NEW HAVEN ARKOSE, NEWARK GROUP, CONNECTICUT
HUBERT, JF
[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 1978, 24 (02) : 151 - 168
[9] JENSEN L R, 1975, Maritime Sediments, V11, P77
[10] KLEIN GD, 1962, GEOL SOC AM BULL, V73, P1127, DOI 10.1130/0016-7606(1962)73[1127:TSMPC]2.0.CO

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