MAJOR ELEMENT COMPOSITION OF MACKENZIE RIVER AT NORMAN WELLS NWT CANADA

被引：12

作者：

LEVINSON, AA

HITCHON, B

REEDER, SW

机构：

[1] Department of Geology, The University of Calgary, Calgary 44, Alta.

[2] Research Council of Alberta, Edmonton, Alta.

[3] Inland Waters Branch, Department of Energy, Mines and Resources, Calgary 3, Alta.

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1969年 / 33卷 / 01期

关键词：

D O I：

10.1016/0016-7037(69)90096-9

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The Mackenzie River at Norman Wells (about 88 per cent of the total Mackenzie drainage) has an average annual flow of 306,000 cfs, with great seasonal variations, and a discharge-weighted average dissolved solids content of 173 ppm which varies seasonally in the narrow range of 162-176 ppm. The previously observed chemical similarity between the Mackenzie and the Mississippi is confirmed. © 1969.

引用

页码：133 / &

共 12 条

[1] BRANDON LV, 1965, 6439 GEOL SURV CAN P
[2] BROWN RJE, 1967, 1246A GEOL SURV CAN, V7
[3] IMPLICATIONS OF THE MINOR ELEMENT CONTENT OF SOME MAJOR STREAMS OF THE WORLD
DURUM, WH
HAFFTY, J
[J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1963, 27 (JAN) : 1 - 11
[4] DURUM WH, 1960, 51 INT ASS SCI HYDR, P618
[5] FREY DG, 1963, LIMNOLOGY NORTH AMER
[6] GIBBS RJ, 1967, GEOL SOC AM BULL, V78, P1203, DOI 10.1130/0016-7606(1967)78[1203:TGOTAR]2.0.CO
[7] 2
[8] Hem J.D., 1959, STUDY INTERPRETATION
[9] LIVINGSTONE DA, 1963, 440G US GEOL SURV PR
[10] THOMAS JFJ, 1957, 856 CAN DEP MIN TECH

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