I meant "peer" as opposed to "pier".

Jim


On Wed, Mar 13, 2013 at 7:44 AM, Mendy Ouzillou <[email protected]> wrote:
> Peter,
>
> No one disputes science is messy, but Jim's point is valid. Drs. Rubin and 
> Grossman have forgotten more than I will likely know in regards to 
> meteoritics, but I also feel a bit frustrated. I expect papers in a journal 
> like "Meteoritics and Planetary Science" to be thoroughly reviewed before 
> being published. It's not an issue of a few esoteric differences, it's about 
> the paper as a whole being rejected by esteemed and respected meteoriticists.
>
> Again, Jim's question is valid. Was this paper peer reviewed? I'm sure it 
> was, which leads to the next question. How was it allowed to be published if 
> it is so far off?
>
> The answer is important to me because I do not have the time to read 
> everything. I have time to read selected books and articles and want to make 
> sure I am properly furthering my education.
>
> Best,
>
> Mendy Ouzillou
>
> On Mar 13, 2013, at 10:05 PM, "Peter Scherff" <[email protected]> wrote:
>
> Hi Jim,
>
>    I find this all delightful. Science is messy. Theories compete for
> acceptance. The one that best fits the facts and is able to predict future
> discoveries wins!
>    If I wanted absolute truths I would read books that the religions of
> the world are based on.
> Thanks,
>
> Peter
>
> -----Original Message-----
> From: [email protected]
> [mailto:[email protected]] On Behalf Of Jim
> Wooddell
> Sent: Wednesday, March 13, 2013 9:46 AM
> To: Meteorite List
> Subject: Re: [meteorite-list] Origin of chondrules
>
> Hello Alan, Jeff, Mendy,
>
> I find this response somewhat bothersome.
>
> I recently read a paper that little old me, not being anyone close to being
> a scientist, can shoot dozens of holes through because of the use of
> outdated obsolete information and now I read this from Alan and Jeff, who I
> look up to and consider piers in this field.
>
> The fact is, people read these papers, therefore they must be true!!!
> It's like the TV commericial where the girl read something on the interenet,
> so it must be true because no one can put stuff on the interent that isn't
> true!
>
> So, what is going on with these papers?  People are creating papers that are
> supposed to be pier reviewed and here we have two piers shooting them down
> in a public forum?  What happen to the process of pier review and if this
> particular paper is completely wrong! Who were the piers?
>
> I am not going to appologise for being a little critical about this but come
> on guys, has it just become a paper mill?  It sure beginning to seem that
> way.  I am completely missing the point of publishing papers with outdated
> and obsolete information (when the new data is in
> hand) and papers that we are reading completely wrong!
>
> I honestly do read these papers and try to ingest as much as I can, but here
> of late, it seems I am completely wasting my time reading them and then I
> read your responses!  Arrrrrgh.
>
> Jim Wooddell
>
>
> On Wed, Mar 13, 2013 at 3:28 AM, Jeff Grossman <[email protected]> wrote:
>> I second what Alan wrote, at the 90% level.  With my remaining finger,
>> I'll add that the worst problem may be that these molten planetesimals
>> must magically keep metallic and silicate melts mixed together in
>> order to make chondrules, many of which have abundant metal.  I think
>> this would be physically difficult, to say the least.
>>
>> I think the ideas in this paper are philosophically quite attractive,
>> joining modern research on cosmochronology with dynamical models of
>> the disk.  But despite this new way of thinking, the basic tenets are
>> quite retro.  Many people up through the 1960s hypothesized that
>> chondrules were fragments of igneous rock. Then modern research on
>> them began.  Study after study found problems with these models, many of
> which Alan outlined.
>> Although the new model is a twist on the old ones, it still is subject
>> to the same tests... and it cannot pass most of them.
>>
>> Jeff
>>
>>
>> On 3/13/2013 2:03 AM, Alan Rubin wrote:
>>>
>>> I'll be happy to give my opinion on the paper.  I think it is
>>> completely wrong.  Here is my reasoning:
>>> 1. Many chondrules are surrounded by secondary igneous shells, still
>>> others by igneous rims.  These shells and rims indicate that the
>>> chondrules haev experienced more than one melting event.
>>> 2.  Many FeO-rich (i.e., Type-II) porphyritic olivine chondrules
>>> contain relict grains of different FeO contents and different
>>> O-isotopic compositions, again indicating multiple melting.  This is
>>> very hard in a collision model.
>>> 3.  One might expect molten planetesimals to have well-mixed melts.
>>> If the chondrules are mainly from the larger planetesimal (the
>>> target) as one would expect, the O isotopic compositions of the
>>> chondrules would probably be mass-fractionated and lie on a slope-1/2
>>> line on the standard three-isotope diagram.  We don't see this.
>>> 4.  One might also expect that as the planestimal melted and began to
>>> crystallize, it would become chemically fractionated, unlike the
>>> unfractionated, solar, compositions of chondrules in primitive
> chondrites.
>>> 5. The occurrence of microchondrules in the fine-grained rims around
>>> some normal-size chondrules and the apparent melting of pyroxene at
>>> the outer surface of the chondrule to form the microchondrules
>>> indicates chondrule melting by a mechanism capable of melting only
>>> the outer surface of the chondrule.  This is totally inconsistent
>>> with the formation by splashing by the collision of molten planetesimals.
>>> 6. There are correlations between chondrule size, the proportion of
>>> different chondrule types, the proportion of those with igneous rims
>>> and secondary shells that are difficult to explain by splashing but
>>> come naturally to a model invoking multiple melting in dusty nebular
> regions.
>>> 7. The non-spherical shapes of most CO chondrules indicates very
>>> rapid cooling or else they would have collapsed into spheres. This
>>> might be okay except for the fact that the large size of their
>>> phenocrysts require a growth period thousands of times longer than
>>> the time it would take a molten droplet to collapse into a sphere.
>>> This again indicates a flash heating mechanism.
>>> 8. The fairly rare occurrence of chondrule-CAI mixtures are difficult
>>> to explain by colliding molten planetesimals, but are sinple to
>>> explain by melting of a mafic dustball that had and old CAI fragment
> inside.
>>> 9. Each chondrite group has its own distinctive narrow range of
>>> chondrule sizes.  In fact, about 90% of the chondrules in any group
>>> have diameters within a factor of 2 of the mean size.  One would
>>> expect molten planetesimals to produce a similar size of chondrules range
> for each group.
>>> Furthermore, chondrule size is correlated with lots of other
>>> chondrule properties (proportions of textural types, numbers with
>>> rims and secondary shells, etc.) that are hard to explain by molten
> planetesimals.
>>> 10. And, I just don't see how we get the different chondrule textural
>>> types by that model.  Some chondrules lack olivine, others lack
>>> pyroxene, some are coarse grained, some are fine-grained, some have a
>>> mixture of different size grains, some include relict grains.  This
>>> seems impossible to produce by the molten planetesimal model.
>>> Since I only have 10 fingers, I'll stop there.
>>>
>>>
>>> Alan Rubin
>>> Institute of Geophysics and Planetary Physics University of
>>> California
>>> 3845 Slichter Hall
>>> 603 Charles Young Dr. E
>>> Los Angeles, CA  90095-1567
>>> phone: 310-825-3202
>>> e-mail: [email protected]
>>> website: http://cosmochemists.igpp.ucla.edu/Rubin.html
>>>
>>>
>>> ----- Original Message ----- From: "Mendy Ouzillou"
>>> <[email protected]>
>>> To: "met-list" <[email protected]>
>>> Sent: Tuesday, March 12, 2013 7:06 PM
>>> Subject: [meteorite-list] Origin of chondrules
>>>
>>>
>>> And now for something completely different ... Meteorite talk.
>>>
>>>
>>> I am in the process of reading through a fascinating article in
>>> latest issue of "Meteoritics and Planetary Science" called "The
>>> Origin of Chondrules and Chondrites: Debris from Low Velocity Impacts
>>> Between Molten Planetisimals."
>>>
>>> This paper is very well written and readable even by a novice such as
>>> myself. What I find interesting is the proposal for a (somewhat) new
>>> theory that chondrules did not instantly form from clumps of heated
>>> nebular dust but instead formed 1.5 to 2.5MY after the formation of
>>> CAIs. the paper states that chondrules formed from splashing when two
>>> differentiated planetisimals collided at a relatively slow speed of
> between 10 to 100m/s.
>>> Without being able to review the previous papers, I have to say that
>>> to me this makes a great deal of sense and appears to solve many of
>>> the inconsistencies that have been raised in some of the older books
>>> that I have read.
>>>
>>> Note: there is a typo in the paer on page 2177. Is states "A strength
>>> of the splashing model is that it can explain why chondrules are
>>> mostly between
>>> 1.5 and 2.5MYr younger than CAI ...". The sentence should read
>>> "older", no "younger".
>>>
>>> Dr. Jeff Grossman, would love to hear your thoughts on this paper.
>>>
>>> Mendy Ouzillou
>>> ______________________________________________
>>>
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>>
>>
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>
>
> --
> Jim Wooddell
> [email protected]
> 928-247-2675
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-- 
Jim Wooddell
[email protected]
928-247-2675
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