HILLSLOPE GRADIENT-PARTICLE SIZE RELATIONS - EVIDENCE FOR THE FORMATION OF DEBRIS SLOPES BY HYDRAULIC PROCESSES IN THE MOJAVE DESERT

被引：17

作者：

ABRAHAMS, AD ^{[1
]}

PARSONS, AJ ^{[1
]}

HIRSH, PJ ^{[1
]}

机构：

[1] UNIV KEELE,DEPT GEOG,KEELE ST5 5BG,STAFFS,ENGLAND

来源：

关键词：

D O I：

10.1086/628956

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

引用

页码：347 / 357

页数：11

共 34 条

ABRAHAMS, AD ;

PARSONS, AJ ;

COOKE, RU ;

REEVES, RW .

[2]

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[3]

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[4]

Birkeland P.W., 1974, PEDOLOGY WEATHERING

[5]

BRYAN K, 1940, ANN ASSOC AM GEOGR, V30, P254

[6]

Bryan K., 1922, US GEOLOGICAL SURVEY, V730, P19

[7] ANALYSIS OF COVARIANCE - ITS NATURE AND USES [J].

COCHRAN, WG .

[8]

COOKE RU, 1972, Z GEOMORPHOL, V16, P76

[9]

DIBBLEE TW, 1967, 522 US GEOL SURV PRO

[10]

FURLEY PA, 1968, Z GEOMORPHOL, V12, P25