Faure unpublished

8 Appendices 7.8.1 Chemical Composition of Metavolcanic Rocks, Wyatt Formation, Weight Percent (Faure unpublished Minshew 1967) Scott Glacier Area and Wisconsin Range in  

F Porphyiitic quartz monzonite Peters Butte, Long Fiills  

2 Rb-SrData, Basement Rocks, Wisconsin Range (Montigny and Faure 1969  

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Mt. Webster, Harold Byrd Mountains (Faure, Unpublished)... 

Fig. 7.5 Silica-variation diagram of whole-rock samples of the Wyatt Formation in the Wisconsin Range of the Horlick Mountains. The x represents a sample of the porphyritic quartz monzonite (Data from Minshew 1967 Faure unpublished in Appendix 7.8.1)...

Fig. IJ The hornblende migmatite that occurs on Spear Nunatak south of Metavolcanic Mountain in Fig. 7.6 may be the oldest rock unit in the Wisconsin Range, but its stratigraphic position cannot be determined in the field because it is not in contact with other rocks and it has not been dated by isotopic methods (Murtaugh 1969). An attempt by Faure (unpublished) to date this specimen failed because its Rb/Sr ratio was too low (Photo by G. Faure)...

Fig. 7.12 Whole-rock Rb-Sr age determinations of the Wyatt Formation discussed in the text (Data from Montigny and Faure unpublished in Appendix 7.8.2.3)...

Fig. 7.20 Whole-rock Rb-Sr age determination of rhyolite pyroclastics in the basement complex of the Long Hills (Data from Faure unpublished in Appendix 7.8.4)...

G. Salmona, C. Guimon, R. Faure, E. J. Vincent, and G. Pfister-Guiiiouzo, Unpublished Results, 1977. 

If physiological approaches are to be used to resolve issues about the relationship between calcium and cytokinins, then a system is needed in which one can add hormone and rapidly measure local Ca" " transients or waves. Experimental conditions need to be found to avoid mechanical disturbances known to induce strong calcium responses as measured by aequorine luminescence [70]. So far, our attempts to measure Ca transients using aequorine luminescence in Nicotiana plumbaginifolia cells and seedlings have been unsuccessful (Faure and Howell, unpublished data). 

Fig. 6. 15 A suite of five whole-rock samples of the Wyatt Formation collected by V.H. Minshew from outcrops between Mt. Wyatt and Mt. Gardiner in the Scott Glacier area define two straight lines labeled A and B derived by least-squares linear regression. Line A which includes all five samples plus one duplicate analysis yields a date of 524 13 Ma and a high initial Sr/ Sr ratio of 0.711919 0.000547 (la). Line B is defined by three selected samples and corresponds to a precise date of 802 2 Ma but it has an impossibly low initial Sr/ Sr ratio of 0.69775. We conclude that the igneous rocks of the Wyatt Formation are older than 524 13 Ma but younger that 802 2 Ma. These previously unpublished data by G. Faure are presented in Appendix 6.133. In addition. Appendices 6.7.3.1 and 6.7.3.2 contain modal analyses and chemical compositions of rocks of the Wyatt Formation from Minshew (1967)...

The data listed below are previously unpublished because they scatter on the isochron diagram and were judged to be unsuitable for dating the Wyatt Formation by the whole-rock Rb-Sr method. Faure et al. (1979) used this data set only to set an upper limit of 788 Ma for the age of the Wyatt Formation. 

Table 7.2 Summary of Rb-Sr dates of whole-rocks and mineral concentrates from the basement rocks of the Wisconsin Range and the Long Hills in the Horlick Mountains. Recalculated to X ( Rb) = 1.42 x 10 year from unpublished analytical data by Faure et al.

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