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onemo

05/29/11 9:45 PM

#153796 RE: rubber duck #153795

rubber duck truly unbelievable all this from one statement that was made,I Just want to See .05.06 again. Its like stepping in a ants pile all you have to do to set them off is poke.lol
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ShortonCash

05/29/11 10:14 PM

#153797 RE: rubber duck #153795

I am not thinking the pps will to the same thing...but there is a connection... more than one. INCO is now VALE. Mr Picket was there before it was INCO.... Vale now has a option to enter into a JV. Vale will need to feed it's beast a multi billion investment. Mr Wheeler is listed as a reference on Mr Pickets resume.....the mine that the use to test the CU grade by bore holes is Voissey Bay.... Rusty Ridge only did 2 bore holes...I not saying it amounts to anything but there are connections and people have made more out of less. footprints in the snow and and who answers the the phone come to mind...LOL

there was a shot from the grassy knoll......


The fact that Mr Picket used Mr Wheeler as a reference at Vale may be most telling...



Quote:
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Title:Using stochastic borehole seismic velocity tomography and Bayesian simulation to estimate Ni, Cu and Co grades.

adsabs.harvard.edu/abs/2010EGUGA..1213289P

Authors Perozzi, Lorenzo; Gloaguen, Erwan; Rondenay, Stephane; Leite, André; McDowell, Glenn; Wheeler, Robert
Affiliation:
AA(Institut National de la Recherche Scientifique, INRS-Eau, Terre et Environnement, Université du Québec, Québec, Canada), AB(Institut National de la Recherche Scientifique, INRS-Eau, Terre et Environnement, Université du Québec, Québec, Canada), AC(Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology , Cambridge, United States), AD(Vale Inco, Toronto, Canada), AE(Vale Inco, Toronto, Canada), AF(Vale Inco, Toronto, Canada)

Indeed, this non-intrusive technique allows inferring the mechanical properties of the ground using travel times and amplitude analysis of the transmitted wavelet between two boreholes, hence provide additional information on the nature of the deposit. Commonly used crosshole seismic velocity tomography algorithms estimate 2D slowness models (inverse of velocity) in the plane between the boreholes using the measured direct wave travel times from the transmitter (located in one of the hole) to the receivers (located in the other hole). Furthermore, geophysical borehole logging can be used to constrain seismic tomography between drill holes. Finally, this project aims to estimate grade of economically worth mineral by integrating seismic