Natrolites with different Fe2+/Fe3+ cation ratios

2017 ◽  
Vol 244 ◽  
pp. 109-118 ◽  
Author(s):  
Yongmoon Lee ◽  
Thomas Vogt ◽  
Yongjae Lee
Keyword(s):  
1981 ◽  
Vol 110 (2) ◽  
pp. A357
Author(s):  
S.Y. Liu ◽  
H.H. Kung

1965 ◽  
Vol 16 (2) ◽  
pp. 290-295 ◽  
Author(s):  
RACHEL LEVY ◽  
E. MOR MURAVSKY

1983 ◽  
Vol 20 (1) ◽  
pp. 49-73 ◽  
Author(s):  
Ronald I. Dorn

AbstractRock varnish coats many surfaces of geomorphic and archaeologic interest in arid lands. All varnish dating techniques are limited by the time lag between the exposure of a surface to subaerial processes and the onset of varnishing. They are valid only where manganese is not remobilized after deposition, for example, in most arid environments. The premise of a new age-determination method, cation-ratio dating, is that the ratio of the more mobile cations (e.g., K and Ca) to titanium in varnish decreases with time. Although there are many inherent assumptions and potential limitations, cation-ratio dating has been verified on relative age-sequences from a Death Valley debris cone, Negev Desert talus flatirons, and prehistoric lake levels at Searles Lake in California. Varnish cation ratios have been calibrated to independently dated surfaces in the Coso volcanic field and vicinity in California. Tentative absolute dates have been assigned to geomorphic surfaces in the Coso area. Cation ratios have been used to distinguish relative ages of archaeologic artifacts in southwestern North America and to demonstrate that varnish at the South Stoddard locality, Mojave Desert, did not form in 25 yr.


1969 ◽  
Vol 41 (1) ◽  
pp. 3-11
Author(s):  
Raili Jokinen

The plant and soil material of this study were collected at a distance of 5—15 km one after the other from 90 farms in Southwest Finland, Satakunta and Ostrobothnia in the years 1966—67. The coefficients of simple and partial correlations between the contents of total magnesium or potassium or the ratios of K/Mg, Ca/Mg, Ca + Mg/K + Na in clover or timothy, the clover content of mixed ley, and the exchangeable cations or their ratios in soil were calculated separately for 1st year, 2nd year, and 3rd year or older leys. The results indicated that according to this rather limited material the potassium content and the ratio K/Mg in clover increased and the magnesium content and the ratio Ca + Mg/K + Na decreased significantly with the increasing clover content of the first year leys, even if the effects of the corresponding exchangeable cations and ratios in soil were taken into consideration. Clover and timothy in mixed ley possibly compete with each other for cations. Cation ratios and the cation content of timothy seemed to be independent of the clover content of the mixed ley, the properties of clover in 2nd year and older leys were likewise not dependent on it. Variations up to 43 % in the magnesium and potassium contents and the cation ratios of clover in first year leys were explained by vatiations in their clover content, and when the exchangeable cations of soil were also taken into account, from 1 to 76 % of this variation could be explained.


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