SHELF-WIDE EROSION, DEPOSITION, AND SUSPENDED SEDIMENT TRANSPORT DURING CYCLONE WINIFRED, CENTRAL GREAT-BARRIER-REEF, AUSTRALIA

被引：85

作者：

GAGAN, MK

CHIVAS, AR

HERCZEG, AL

机构：

[1] JAMES COOK UNIV N QUEENSLAND,DEPT GEOL,TOWNSVILLE,QLD 4811,AUSTRALIA

[2] AUSTRALIAN NATL UNIV,RES SCH EARTH SCI,CANBERRA,ACT 2601,AUSTRALIA

来源：

JOURNAL OF SEDIMENTARY PETROLOGY | 1990年 / 60卷 / 03期

关键词：

D O I：

10.1306/212F91BF-2B24-11D7-8648000102C1865D

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

Observation of shelf sediments collected immediately before and after Cyclone Winifred crossed the central Great Barrier Reef shelf (1 February 1986) confirmed that the storm produced a normally graded, mixed terrigenous-carbonate storm layer extending 30km offshore in water up to 43m deep. Distinct post-Winifred changes in the cross-shelf distribution of organic carbon and carbonate in the mud-fraction of the sediment suggest that suspended sediment transport was extensive and that the storm layer had multiple sediment sources. -from Authors

引用

页码：456 / 470

页数：15

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