THE NORTHWEST ATLANTIC MID-OCEAN CHANNEL OF THE LABRADOR SEA .2. DEPOSITION OF PARALLEL LAMINATED LEVEE-MUDS FROM THE VISCOUS SUBLAYER OF LOW-DENSITY TURBIDITY CURRENTS

被引：75

作者：

HESSE, R

CHOUGH, SK

机构：

来源：

关键词：

D O I：

10.1111/j.1365-3091.1980.tb01656.x

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

引用

页码：697 / 711

页数：15

共 42 条

[1] STRUCTURE OF TURBULENT BOUNDARY IN DRAG-REDUCING PIPE-FLOW [J].

ACHIA, BU ;

THOMPSON, DW .

[2]

Allen J.R.L, 1970, EARTH SCI SERIES

ALLEN, JRL .

[4] THE FLOW OF COHESIONLESS GRAINS IN FLUIDS [J].

BAGNOLD, RA .

[5]

Bouma A.H., 1962, SEDIMENTOLOGY SOME F

[6]

Bouma A. H., 1972, T GULF COAST ASS GEO, V2, P205

[7]

BOUMA AH, 1973, GULF COAST ASS GEOL, V23, P368

[8] ORIGIN OF HORIZONTAL LAMINATION UNDER TURBULENT BOUNDARY-LAYERS [J].

BRIDGE, JS .

[9]

BRIGGS LI, 1965, SOC ECONOMIC PALEONT, V12, P5

[10]

CHOUGH S, 1976, GEOLOGY, V4, P529, DOI 10.1130/0091-7613(1976)4<529:SMTATC>2.0.CO