ORIGIN OF GROUNDWATER SALINITY IN THE LAC-DU-BONNET GRANITE, SOUTHEASTERN MANITOBA, FROM CL-36 MEASUREMENTS

被引：3

作者：

GASCOYNE, M

SHARMA, P

KUBIK, PW

机构：

[1] PURDUE UNIV,DEPT PHYS,W LAFAYETTE,IN 47907

[2] SWISS FED INST TECHNOL,INST MITTELENERGIEPHYS,CH-8093 ZURICH,SWITZERLAND

来源：

NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION B-BEAM INTERACTIONS WITH MATERIALS AND ATOMS | 1994年 / 92卷 / 1-4期

关键词：

D O I：

10.1016/0168-583X(94)96040-2

中图分类号：

TH7 [仪器、仪表];

学科分类号：

0804 ; 080401 ; 081102 ;

摘要：

The results of analyses of the Cl-36 content of groundwaters in the Lac du Bonnet granite batholith are described and compared with previous modelling calculations and Cl-36 content of rock matrix solutions obtained from a borehole leaching experiment. The results are used to provide support for the proposal that groundwater salinity is largely derived from dissolution of soluble salts in the rock matrix.

引用

页码：389 / 392

页数：4

共 9 条

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[2]

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[3]

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[9]

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