I did read them. I still disagree. All those were special cases, and they were relatively strong fields. If they were to act from a geological layer below a topsoil, and perhaps inside a building, they would need to be VERY strong.
Hans - i agree - please read the posts. I said it establishes the principle of a magentic / brain interaction. This was directed towards your much earlier claims that magnetics cant do that [when you went off ranting about audio waves - something no one else here mentioned] - they can, and you were wrong on that point. The point is, that the research I cited (among a good deal of other research) establishes the principle of an interaction. I notice you have not followed up any of the other names i gave you - which actually use much weaker fields - why was that?
I suggest you revise your strategy as you seem to like leaping all over the place and your memory really is letting you down. Never mind.
I think you don't understand signal complexity. If you make a momentary sample, NO signal is complex.
Who said anything about taking momentary samples? - I have long term measurements from the environment. Of course they are all non-stationary (which i think is what you meant to say) to some degree, but some of my research suggests that fields in certain areas are much more complex. Hans, I take time-linked simultaneous baseline measurements as well - the anomalies, on occasion, appear only in the areas associated with strange reports (we have also found this when controling for lamps / devices etc). We have found anomalies with three-phase EMF systems, poor grounding (we suspect), and highly magnetised objects. None of this has anything to do with geology or recordings - but you should know we have made these measurements which support the lab evidence you wont read.
Yes - time based complexity is crucial - I have always said this, but in the presence of big distortions you get directional effects as well.
So you have no idea of wave shapes, then. You are only seing the frequency domain.
You obviously have no idea what the system is capable of, otherwise you would not say such a thing. I can use the software to 'play-back' the signals in the time AND frequency domain (raw signal and processed signals) - at the same time. I can look at shapes, both domains - as you will also know, are related.
Do yourself a favor, and look at some of the signals on an oscilloscope, so you get an impression of the time domain.
Could you explain to me how an oscilloscope would give me anything my digital software (including digital oscilloscopes) wont give me (apart from the obvious small differences between analogue and digital)? Trust me we are looking into this with digital oscilloscopes = if you knew about the software - you would know what it can do. It addresses your concerns quite easily.
All signals, no matter how complex, can be broken down to a set of pure sine components, but that will only ever tell you half the story.
Some will break down easier than others - and thats my point. It allows us to show that magnetically, some regions look different and the more complex regions just also happen to be the only ones where experiences have been reported (for cases where magnetic fields are important). Even when we have controlled to some degree for visual context and suggestibility.
I'm sorry, but you remind me more and more of Roger Coghill. He is also making measurements with unsuited instruments and making conclusions from the results.
Sorry Hans, but are you not making a few logical fallacies here by trying to tarnish me with others - shooting the messenger rather than dealing with the message? I have nothing to do with the research you talk of and resent the implication. If you took the time to read and digest (clearly your biggest failing here) you will see its nothing fo the sort. Please justify your sweeping statements by saying how my equipment is not suited to tell the difference between the fields. You have not even asked me about the hardware yet - and here you are making ridiculous statements like that. You are the one behaving like a woowoo - without recourse to the actual facts or any urgency to go and get them.
You claimed magnetic fields could have no effects - I showed you that you were wrong (now you shift on that - which is good). You claim all fields around us are complex - not so, its a continuum not an absolute. I measure fields regularly and around the house / office they are not that complex at all. You claim I need an oscilloscope without realising that I have a digital one as part of the software I use - which I did hint at in the previous posts. Go and see stuff like
www.systat.com and look up autosignal (
http://www.systat.com/products/AutoSignal/). Go and look at
www.sigview.com and (
http://www.sigview.com/screenshots.htm). Go and look at Matlab, and so on.....I mentioned all these before...but you seem to have missed that.
I am afraid you cannot hide your misunderstanding by personal comments. I can see right through it. So, now you know the equipment is not insufficient where now for your sweeping unfounded claims?
Could we get the debate back on track? I originally raised the suggestion of magnetite / ghosts that is a growing one I have encountered amongst woo's. Both you and Tricky have given excellent reasons why there may be problems with that account - even in terms of just being the source of complex magnetic fields (if it was vibrating say via geological stressors). It seems unlikley it could be a source of anything really. Fine. However, at points we have gone off and discussed the role of magnetic fields in general and their interaction with neural processes and you seem to be debating issues relating to that and then brining it back to the geological point. The two are not connected directly. One sets up and establishes the principle (one you denied) the other is a big-leap extension of that principle. It is the refutatiojn of the leap I accept, not the refutation that magnetic fields, in principle, have been shown to be important in some cases.
(note - nothing to do with recordings).