LOW SEA-LEVEL TIDAL ORIGIN OF CELTIC SEA SAND BANKS - EVIDENCE FROM NUMERICAL MODELING OF M2 TIDAL STREAMS

被引：46

作者：

BELDERSON, RH ^{[1
]}

PINGREE, RD ^{[1
]}

GRIFFITHS, DK ^{[1
]}

机构：

[1] MARINE BIOL ASSOC LAB,PLYMOUTH PL1 2PB,DEVON,ENGLAND

来源：

MARINE GEOLOGY | 1986年 / 73卷 / 1-2期

关键词：

D O I：

10.1016/0025-3227(86)90113-1

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：99 / 108

页数：10

共 15 条

[1]

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[3]

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[4]

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[5]

Flather R., 1981, NORWEGIAN COASTAL CU, V2, P427

[6]

Johnson M.A., 1982, OFFSHORE TIDAL SANDS, P58, DOI [10.1007/978-94-009-5726-8_4, DOI 10.1007/978-94-009-5726-8_4]

[7]

KENYON NH, 1981, INT ASS SEDIMENTOL S, V5, P257

[8]

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[9] THE QUATERNARY HISTORY OF THE CENTRAL AND SOUTHWESTERN CELTIC SEA [J].

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EVANS, CDR .

MARINE GEOLOGY, 1984, 57 (1-4) :259-293

[10] QUARTER DIURNAL SHELF RESONANCES AND TIDAL BED STRESS IN THE ENGLISH-CHANNEL [J].

PINGREE, RD ;

GRIFFITHS, DK ;

MADDOCK, L .

CONTINENTAL SHELF RESEARCH, 1984, 3 (03) :267-289

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