AI-GEOSTATS: Invitation to connect on LinkedIn

2010-12-14 Thread M. Nur Heriawan
LinkedIn


   
AI,

I'd like to add you to my professional network on LinkedIn.

- M. Nur

M. Nur Heriawan
Lecturer at Mining Engineering Department, Bandung Institute of Technology 
Indonesia

Confirm that you know M. Nur Heriawan
https://www.linkedin.com/e/dgf4jv-ghonvkrj-4s/isd/2022205333/5gtJDAY8/


 
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(c) 2010, LinkedIn Corporation

AI-GEOSTATS: geostat for alluvial deposit

2010-10-13 Thread M. Nur Heriawan
Dear list,

I need references about the application of geostatistics for the resources 
estimation of alluvial and placer deposits. If someone in the list has 
experiences about it, could you please share it? As you might know 
that alluvial 
deposits i.e. gold or tin has very high variability in the lateral direction, 
so 
the resources classification based on the variogram range is seemed to be not 
appropriate. Anyway, when we used the kriging standard deviation for resources 
classification, the result was seemed to be not reliable.  
 
Thank you for any suggestions.

Best regards,---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan 



  

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Re: AI-GEOSTATS: moving averages and trend

2010-02-01 Thread M. Nur Heriawan
Goovaerts, regarding the factorial kriging you mentioned below...is it possible 
to filter the micro component (nugget effect) from our spatial model? Because 
the magnitude of nugget effect is related to the magnitude of variance error as 
well.
 
Thank you.

Regards,---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan 





From: Pierre Goovaerts goovae...@terraseer.com
To: seba sebastiano.trevis...@libero.it
Cc: José M. Blanco Moreno jmbla...@ub.edu; ai-geostats@jrc.it
Sent: Tue, February 2, 2010 12:27:09 AM
Subject: Re: AI-GEOSTATS: moving averages and trend

well Factorial Kriging Analysis allows you to tailor the filtering weights
to the spatial patterns in your data. You can use the same filter size but
different kriging weights depending on whether you want to estimate
the local or regional scales of variability.

Pierre


2010/2/1 seba sebastiano.trevis...@libero.it

Hi José
Thank you for the interesting references. I'm going to give a look!
Bye
Sebastiano 



At 15.46 01/02/2010, José M. Blanco Moreno wrote:

Hello again,
I am not a mathematician, so I never worried too much on the theoretical 
reasons. You may be able to find some discussion on this subject in Eubank, 
R.L. 1999. Nonparametric Regression and Spline Smoothing, 2a ed. M. Dekker, 
New York.
You may be also interested on searching information in and related to 
(perhaps citing) this work: Altman, N. 1990. Kernel smoothing of data with 
correlated errors. Journal of the American Statistical Association, 85: 
749-759.

En/na seba ha escrit: 

Hi José
Thank you for your reply.
Effectively I'm trying to figure out the theoretical reasons for their use.
Bye
Sebas


-- 
Pierre Goovaerts

Chief Scientist at BioMedware Inc.
3526 W Liberty, Suite 100
Ann Arbor, MI  48103
Voice: (734) 913-1098 (ext. 202)
Fax: (734) 913-2201

Courtesy Associate Professor, University of Florida
Associate Editor, Mathematical Geosciences
Geostatistician, Computer Sciences Corporation
President, PGeostat LLC
710 Ridgemont Lane
Ann Arbor, MI 48103
Voice: (734) 668-9900
Fax: (734) 668-7788

http://goovaerts.pierre.googlepages.com/



  

AI-GEOSTATS: kriging variance and resources classification

2008-09-19 Thread M. Nur Heriawan
Dear list,

I am searching any references which can address the relationship between 
kriging variance and mineral resources classification (measured, indicated, and 
inferred). Is there rule of thumb for that? As I know, kriging variance only 
takes into account drilling spacing and variogram model, while grade value is 
not related to it.

I hope anybody in the list could give me the hint.

Thank you.
---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan



  
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AI-GEOSTATS: DDH vs BH

2008-07-31 Thread M. Nur Heriawan
Dear list,

I am doing the structural analysis for Pb-Zn grade in 3D. In the first step, I 
have used the diamond drill hole (DDH exploration) data. Then I work separately 
using blast hole (BH) data with number of data is much larger than DDH, but BH 
data cover the area much less wider in 3D space compare to DDH data. I would 
like to check the spatial consistency of Pb-Zn grade by statistics and 
variography analysis between DDH and BH. In this case is interesting also to 
discuss about change of support as the BH data have much closer spacing compare 
to DDH data, and BH result  sludges/cuttings compare to DDH which result cores 
for assay data. I am performing the analysis for each rocktypes group (domain). 

I will be happy if anyone here in the list could share or suggest me any 
references related to this subject.

Thank you for kind help and attention.

Regards,
---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan



  
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AI-GEOSTATS: public domain software for reserve modeling and mine planning

2007-12-12 Thread M. Nur Heriawan
Dear list,

How are you doing? Hopefully everything is doing well.

I would like to ask anybody if you could share some
knowledges...are there any kind of public domain (open
source) softwares for reserve modeling as well as for
mine planning (design)? 

I know something like SGeMS perhaps can be used for
reserve modeling (block model in 3D), but not for mine
planning.

Thank you for any comments.

Best regards,

---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan


  

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AI-GEOSTATS: Global estimation on a domain of unknown geometry

2007-11-24 Thread M. Nur Heriawan
Dear list,

I would like to discuss with you about the case study
given in Journel`s book of Mining Geostatistics,
related to the Chapter V.C.4.: Global estimation on a
domain of unknown geometry. The case study is
regarding Ity deposit (p. 439 to 443) where the
estimated block has different size: b1 (N-S direction)
is 20 m and b2 (W-E direction) is 30 m.

When we calculate the variance of global estimation,
in p. 441 mentioned that in this case, the global
estimation variance is calculated as the sum of a line
term and section term. The line term (corresponding to
the N-S lines which have the greatest data density,
b1b2) measures the extension error of the 58 central
accumulations to their segments (b1=20 m) of
influence.

My question is: what to do if we have the same data
density, for example b1=b2...? which lines direction
we should use to calculate the extension variance of
points in lines term?

The second case is still related to p. 441, mentioned
that when we measure the extension variance of lines
in rectangles term...the nugget effect has no
influence, this is due to the fact that the nugget
constant, regularized over the length L1 (for
example), can be considered as zero because L1 is much
greater than the diameter of the sampling pit, which
is the support on which the constant C0 was defined.

My question is: for which case (the rasio or
comparison of the length of line and diameter of
sampling pit) we should consider that the nugget is
not zero? is there a rule of thumb for this case?

I am waiting for any comments. Thank you.

Regards,
 

---
M. Nur Heriawan
Earth Resources Exploration Research Group
Faculty of Mining and Petroleum Engineering
Institut Teknologi Bandung (ITB)
Jl. Ganesha 10 Bandung 40132 INDONESIA
http://www.mining.itb.ac.id/heriawan


  

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AI-GEOSTATS: geostatistics for vector estimation

2007-09-11 Thread M. Nur Heriawan
Dear list,

I am wondering if estimating kind of vector, i.e.
fracture direction by using kriging or cokriging
method is a proper way in geostatistics. We need
opinion and references (if any) about this work.

Thank you for attention.

Regards,

---
M. Nur Heriawan
Laboratory of Applied Geoscience and Technology  
Graduate School of Science and Technology
Kumamoto University, JAPAN
http://www.civil.kumamoto-u.ac.jp/tansa


   

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AI-GEOSTATS: the importance of additiveness

2007-05-23 Thread M. Nur Heriawan
Dear list,

We know that additivity of the variables under study
is the basic requirement of any geostatistical study.
In practical term, geostatistic works on the variables
defined on constant support. 

Therefore if our variables (i.e. grade) were derived
from the different support (i.e. sample thickness or
size), we should use the accumulation (product of
thickness or size and the grade) before estimate it.
Then the estimated grade is obtained by dividing the
estimated accumulation by the estimated thickness or
size. 

May someone has experience regarding the effect of
ignoring additivity in any kind of geostatistical
estimation compare to the estimation which considering
additivity. In other word, how importance of this
additivity in geostatistical estimation. Any opinions
or references are very welcome.

Thank you for attention.

Kind regards,

---
M. Nur Heriawan
Laboratory of Applied Geoscience and Technology  
Graduate School of Science and Technology
Kumamoto University, JAPAN
http://www.civil.kumamoto-u.ac.jp/tansa


 

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AI-GEOSTATS: ore grade and reserve estimation

2007-04-25 Thread M. Nur Heriawan
Dear list,

I am looking for some books about integrated reserve
estimation and grade control (for mine planning).
These books are for teaching purpose.

From googling, I found two titles:
-
Ore Reserve Estimation and Strategic Mine Planning:
Stochastic Models and Optimizations with Case Studies
Dimitrakopoulos, Roussos 
Springer, 2006

Ore Reserve Estimation and Grade Control 
J.E. Gill
The Canadian Institute of Mining and Met, 1968
-

I did not find any reviews about these books.
Therefore, before I order them, may somebody give the
comment or suggestion.

Thank you for kind attention,

Regards,  

---
M. Nur Heriawan
Laboratory of Applied Geoscience and Technology  
Graduate School of Science and Technology
Kumamoto University, JAPAN
http://www.civil.kumamoto-u.ac.jp/tansa

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AI-GEOSTATS: how to incorporate drilling and wireline logging data

2007-01-28 Thread M. Nur Heriawan
Dear all,

I need a reference on how to incorporate the drilling
and wireline logging data. As we know that sometimes
the informations of layers depth resulted from
drilling and wireline logging are different, then for
this case we need to incorporate them by considering a
measurement error.

Actually a few years ago I found a paper discussed
about this, but I lost it, and I could not search it
again.

I appreciate any helps.

Thank you.
 

---
M. Nur Heriawan
Laboratory of Applied Geoscience and Technology  
Graduate School of Science and Technology
Kumamoto University, JAPAN
http://www.civil.kumamoto-u.ac.jp/tansa


 

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AI-GEOSTATS: software for image analysis

2006-10-10 Thread M. Nur Heriawan
Dear list,

I am going to analyze and interpret the digital image
obtained from X-Ray CT scanner. Hopefully someone
could suggest me regarding a free software for such
image analysis.

Thank you for attention.

Regards,


---
M. Nur Heriawan
Lab. of Applied Geosciences  Tech.  
Kumamoto Univ., Japan

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Re: AI-GEOSTATS: Coregionalization2

2006-08-24 Thread M. Nur Heriawan
Hello Gonzalo,

To fit your linear model of coregionalization, you
could use a fortan program named LCMFIT2.FOR. You have
to download it from IAMG official homepage. Please
read the following article for detail explanation:

Pardo-Iguzquiza, E. and P.A. Dowd.(2002), FACTOR2D: a
computer program for factorial kriging. Computer 
Geosciences, Vol. 28, pp.857-875.

Good luck!

Nur H.

--- [EMAIL PROTECTED] wrote:

 I am interested in a program for fitting a linear
 model of corregionalization
 for soil physical and chemical properties data.
 
 If some of you can give me some advices i woul be
 very please


---
M. Nur Heriawan
Lab. of Applied Geosciences  Tech.  
Kumamoto Univ., Japan

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RE: AI-GEOSTATS: covert binary grid to ASCII grid

2006-08-21 Thread M. Nur Heriawan
Dear Bob,

Thanks for response my mail and sorry for not giving a
complete information. The format of binary grid file I
have is .bgr

In fact, I have tried to use the grid translator in
GEODAS, but it failed.


Regards,

Nur H.


--- bob sandefur [EMAIL PROTECTED] wrote:

 There are thousands of binary grid formats-Which one
 do you have?
 


---
M. Nur Heriawan
Lab. of Applied Geosciences  Tech.  
Kumamoto Univ., Japan

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[ai-geostats] about cross-validation

2006-04-26 Thread M. Nur Heriawan
Dear everyone,

One of my colleague asked me about the mathematical
equation of cross-validation method (leave-one-out
method), and I said that it depends on the estimation
method he used. He wants to know the general
mathematical equation to define a cross-validation
process. 

So far, in my experience, such method is performed
just to check...which variograms model we used in
(kriging) estimation are correct (valid). 

But cross-validation method should be used also to
check the validation of any kind of estimation methods
beyond kriging.

May someone address me to a reference or book
discussed in detail about cross-validation
(leave-one-out) method, especially in mathematical
point of view. Any kind of information related to this
method is also appreciated.

Many thanks for kind attention.


Regards,


Nur Heriawan

Earth Resources Exploration Research Group
Faculty of Earth Sciences and Mineral Technology
Institut Teknologi Bandung (ITB), Indonesia
http://www.isme-ix.org/
 
  

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[ai-geostats] software for 3D visualization

2006-03-12 Thread M. Nur Heriawan
Hello everybody,

I have 3D categorical output data in X, Y, and Z
resulted from interpolation. I need a program or
software for visualizing those data in 3D block model.
I have used PIXELPLT (from GSLIB) to make any slices
in XY, XZ, and YZ directions, but it could not be used
for 3D block visualization. 

So, could anybody suggest me which free or comercial
program (or software) I should use in this purpose? 

Thanks for your helps.


Best regards,

Nur Heriawan

Earth Resources Exploration Research Group
Institut Teknologi Bandung (ITB)
Indonesia
  

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Re: [ai-geostats] spherical model

2006-02-20 Thread M. Nur Heriawan
Dear Isobel,

Thanks for your reply. It is the first reply regarding
this subject. Beforehand, I got one information
mentioned that spherical model corresponds to a Random
Function resulting of the summation of 3D spheres
random in space, each sphere being given a value.
 
Moreover, it is mentioned that there is no particular
reason why this model should be used rather than
another (positive definite) equation. But historically
people have given preference to this model, and most
(but not all) experimental semivariograms can be
modeled by a combination of spherical.

The information I got above is exactly matching with
yours. Again thank you.

Cheers,

Nur H.

--- Isobel Clark [EMAIL PROTECTED] wrote:

   Hi, I do not know whether you received any answers
 off-list, so here goes.

   The spherical model of geostatistics was
 so-named by Matheron and is sometimes also known as
 the Matheron model. His idea was that a sample has a
 'sphere of influence' around it. Potential (or
 actual) samples within this sphere have values which
 are 'related' to the value at the central point.
 Imagine, now, a second such point with its own
 sphere of influence. If the spheres do not touch,
 there is no relationship between the values at the
 two central points. If the spheres overlap, there
 will be a relationship. The more the spheres
 overlap, the stronger the relationship. 

   The spherical semi-variogram is the simple
 geometric calculation for the volume of NON-overlap
 of the two spheres, given the distance between their
 centres. 

   There is no real reason why it should work in so
 many cases -- any more than there is for the Normal
 (Gaussian) distribution being found so often in
 nature. In fact, there is often a possibility to fit
 several of the semi-variogram models in practice.
 You could decide which is most appropriate using
 something like Cressie's goodness of fit test
 (analagous to a sort of chi-squared statistic).


M. Nur Heriawan
http://www.mining.itb.ac.id/heriawan

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[ai-geostats] spherical model

2006-02-13 Thread M. Nur Heriawan
Dear list,

I have small query. Why almost all kind of spatial
data set (ore grade data, sea surface temperature
data, soil thickness, etc.) is fitted to the spherical
(variogram) model? May anyone explain the origin of
this spherical model?

Thank you for your help.

Regards,

M. Nur Heriawan
---
Graduate School of Science and Technology
Kumamoto University 
Kurokami 2-39-1, Kumamoto 860-8555, JAPAN 


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[ai-geostats] fitting an ellipsoid model

2005-09-07 Thread M. Nur Heriawan
Dear list,

I am going to fit an ellipsoid model of anisotropy.
The input are 4 ranges (scale parameters) and 4 main
directions (0, 45, 90, 135 degree) from directional
semivariogram model.

Is there anybody have experience or a reference
related to the algorithm for doing that? It is looked
simple but make me confusing. I could do it by manual,
but I want to obtain the precise ellipsoid anisotropy
by writing a small routine. 

Many thanks for your attention.

Regards,

M. Nur Heriawan
http://www.mining.itb.ac.id/heriawan

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Re: [ai-geostats] autofitting variogram

2005-06-23 Thread M. Nur Heriawan
Hello,

The GSLIB itself gives the routine to draw a variogram
model (vmodel), but unfortunately not by autofit.
First, you have to define the fitting model, then set
it into the parameter file in vmodel.

Good luck

Cheers,

Nur Heriawan
http://www.mining.itb.ac.id/heriawan
 

--- samuel verstraete [EMAIL PROTECTED]
wrote:

 Hello dear list,
 
 Is there anybody aware of software that can autofit
 a variogram to
 gslib output (gamv)
 
 gr,
 
 Samuel
 
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Re: [ai-geostats] Joint of two layer.

2005-06-19 Thread M. Nur Heriawan
I did the same project 2 years ago using the same
software. But on that time I worked with 2D variogram
(of coal thickness). I think there is no direct
relationship between the range of vertical variogram
with the clay thickness, if the variogram you used was
related to the coal thickness. 

OK made the smoothing in estimation result, that's
why some parts of your intercalations were calculated
as coal. This problem will be more clearly appeared if
you have a nugget component in your variogram (of coal
thickness).  

I think you can try to use other methods such as
indicator kriging or conditional simulation.  


Cheers,

Nur Heriawan
http://www.mining.itb.ac.id/heriawan


--- Tayfun Yusuf Yunsel [EMAIL PROTECTED] wrote:

 Dear list members,
  
 I am studying on a coal reserve calculation using OK
 procedure. I applied a 
 3D grid design to the composited data. So I have a
 horizontal and vertical 
 variogram (two range). The grid size in the vertical
 direction is 4m and 
 vertical variogram range is 16m. There are
 intercalations whose thickness 
 varies between 0.50-6m in the coal layer. In the
 estimation process (OK), 
 the clay layers (intercalations) were calculated as
 coal (due to clay 
 thickness  vertical variogram range). 
  
 My question is that How can I seperate a thin
 intercalation layer (according 
 to the coal layer (30-60m)) from the coal layer?
  
 Currently I am using the Isatis software.
  
 Thank you very much for your attention and time.
  
  
  
 Res. Assist. Tayfun Yusuf YNSEL
  
 Mining Engineering Department
 Engineering Faculty
 Cukurova University
 01330, Balcali, Adana
 TURKEY
  
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[ai-geostats] a linear coregionalization model

2005-05-16 Thread M. Nur Heriawan
Dear All,

I am working with a multivariate geostatistics. In
determining whether the semivariogram or
cross-semivariogram follows a linear coregionalization
model or not...must the spatial range be the same?

For instance, I have semivariogram and
cross-semivariogram from 2 different variables as
follow:
gamma1(h) = 11 nug(h) + 39 sph(h/60)
gamma1(h) =  9 nug(h) + 15 sph(h/100)
gamma12(h)= 14.5 sph(h/80)

If I consider only the variance-covariance components,
such models follow the positive-semi definite
condition. But how about the different spatial range I
have in each semivariogram-cross semivariogram? Is it
essential in a linear coregionalization model?

Thank you for your attention.

Regards,

Nur Heriawan




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Re: [ai-geostats] Who is J. W. Merks???

2005-04-30 Thread M. Nur Heriawan
Dear Perry,

Please visit this website:
http://www.geostatscam.com/index.htm

You might know him better... :-)  

Regards,

Nur Heriawan

Dept. of Mining Eng.
Institut Teknologi Bandung
Jl. Ganesha 10 Bandung 40132
INDONESIA

--- [EMAIL PROTECTED] wrote:

 Hi List
  
 I was searching for geostats books on www.amazon.com
 http://www.amazon.com
 and came across a reviewer by the name of J. W.
 Merks who has trashed every
 single geostatistical publication available.  This
 is what he had to say
 about Geostatistics : Modeling Spatial Uncertainty
 (Wiley Series in
 Probability and Statistics) by

http://www.amazon.com/exec/obidos/search-handle-url/index=booksfield-autho
 r=Jean-Paul%20%20Chil%E8s/103-9170296-4642251
 Jean-Paul Chilès,

http://www.amazon.com/exec/obidos/search-handle-url/index=booksfield-autho
 r=Pierre%20%20Delfiner/103-9170296-4642251 Pierre
 Delfiner :
  
 Geostatistics is a fatally flawed variant of
 mathematical statistics
 because it violates the requirement of functional
 independence and ignores
 the concept of degrees of freedom. Google bre-x
 bogus barren and look
 under Geostatistical Fiction to find out what the
 author and similarly
 challenged scholars know about degrees of freedom.
 Ironically, unbiased
 statistical inferences are impossible to obtain
 without taking degrees of
 freedom into account. The author has been asked to
 explain why the variance
 of a SINGLE distance-weighted average is replaced
 with the variance of a SET
 of distance-weighted averages. His reply will be
 posted ASAP.
  
 He said this about the GSLIB2 manual:
  
 Geostatistics is a fundamentally flawed variant of
 mathematical statistics
 because it violates the requirement of functional
 independence and ignores
 the concept of degrees of freedom. Each weighted
 average had its on variance
 wen Sir Ronald A Fisher was knighted in 1952 but
 when the distance-weighted
 average mutated into an honorific kriged estimate,
 it became the first and
 only weighted average to be reborn without its
 variance. Incredibly, kriging
 variances and kriging covariances of sets of kriged
 estimates are the
 cornerstones of geostatistics. Incredible indeed
 because the variance of a
 set of distance-weighted averages is as inane a
 measure for variability,
 precision and risk as its covariance is for spatial
 dependence. 
 
 Hailed by pundits as a new science but dismissed by
 skeptics as a sham,
 geostatistics is applied to small data sets in large
 sample spaces by
 assuming spatial dependence, interpolation by
 kriging, perfect smoothing and
 rigging the rules of mathematical statistics.
 Statistics 101 ought to be
 compulsory for those who assume the requirement of
 functional independence
 can be violated a little but not a lot.
 
  
 Can anyone tell me what this guy is talking about? 
 Is he a nutter?  Does he
 need to get a life?  Who is he anyway?
  
  
 Cheers
 Perry
  
 
 Perry Collier 
 
 Senior Mine Geologist 
 Ernest Henry Mine   
 Xstrata Copper Australia 
 * (07) 4769 4527 
 *  (07) 4769 4555 
 * [EMAIL PROTECTED] 
  http://www.xstrata.com http://www.xstrata.com/  
   
 PO Box 527 
 Cloncurry QLD 4824 
 Australia 
   
 I like rich people. I like the way they live. I
 like the way I live when
 I'm with them... 
 
 From Roger  Hammerstein's Sound of Music 


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