[meteorite-list] Anomalous and Ungrouped Ordinary Chondrites

2003-10-19 Thread j . divelbiss
Hello all,

I've always been intrigued but puzzled about the classification of a few 
ordinary chondrites into the black hole of assigned classification 
names...ungrouped and/or anomalous. Some are specified with petrologic 
assignments and others without. Ebay on occasion offers us Hah 180 that is 
classified as an anomalous 3.5 ordinary chondrite and Dhofar 535 that is 
classified as ungrouped, and without a petrologic designation in its' 
description. According to David's site below...Hah 180 is similar to Deakin 
001. And there maybe others I am not thinking of. Oxygen isotopes and 
weathering seem to be some of the key factors...and as stated on David's site 
they may come from a proximity close to where enstatite chondrites were 
formed, and in my opinion their appearance makes them at least look like some 
of the EL3's out there.

Does anyone know what the latest theory is for these and will they one day 
get an official LL3 to 3.5 anomalous label which would finally give them a 
home? Seems to me to call them anything else puts them/keeps them in 
classification limbo.

http://www.geocities.com/dgweir/HAH180.HTM

Just curious,

John


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AW: [meteorite-list] Anomalous and Ungrouped Ordinary Chondrites

2003-10-19 Thread Norbert Classen
Hi John, and list,

As to the ungrouped HaH 180, and Deakin 001, it has been suggested
that both represent samples of a new and previously unsampled parent
body. If that holds to be true, they will never get a LL or L
classification. Ungrouped just means that a sample can't be
assigned to any of the established groups, and that means also
that they do most probably represent a unique parent body. Now,
if we find three more meteorites like HaH 180, or Deakin 001,
scientists will most likely create a new group, and then these
samples won't be ungrouped, any longer.

The term anomalous is used for meteorites that actually can be
assigned to an existing group, but that differ in some aspects from
the other known members of that group. Thus, HaH 180 isn't anomalous,
it's simply ungrouped.

Short: an ungrouped chondrite most probably stems from an asteroid
that hasn't been sampled so far. An anomalous LL, for example, is
most probably from the LL parent body/asteroid, but it differs from
the other LL members in some respect. The petrologic grades have
nothing to do with that, and of course an ungrouped chondrite can
be a 3.5, or a plain 6.

Hope this helps ;-)

Best,
Norbert

A puzzled John wrote:

 Hello all,

 I've always been intrigued but puzzled about the classification of a few
 ordinary chondrites into the black hole of assigned classification
 names...ungrouped and/or anomalous. Some are specified with petrologic
 assignments and others without. Ebay on occasion offers us Hah
 180 that is  classified as an anomalous 3.5 ordinary chondrite and
 Dhofar 535 that is classified as ungrouped, and without a petrologic
 designation in its' description. According to David's site below...Hah
 180 is similar to Deakin 001. And there maybe others I am not thinking
 of. Oxygen isotopes and weathering seem to be some of the key factors...
 and as stated on David's site they may come from a proximity close to
 where enstatite chondrites were formed, and in my opinion their appearance
 makes them at least look like some  of the EL3's out there.

 Does anyone know what the latest theory is for these and will
 they one day
 get an official LL3 to 3.5 anomalous label which would finally
 give them a
 home? Seems to me to call them anything else puts them/keeps them in
 classification limbo.


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Re: AW: [meteorite-list] Anomalous and Ungrouped Ordinary Chondrites

2003-10-19 Thread j . divelbiss
Norbert,

Makes sense to me...it looks like some consistency is in order here. 

I wonder how many of these does Bernd have in an ungrouped  listing, or has 
he gone ahead and grouped them in the LL's, etc. Are you out there Bernd??? 
What say?

Do we have a good handle on which ones are ungrouped and related? 

How many samples does it take to create a new group? Is it when there is 
consistency in a few...if so, who would then come up with such a group?

I know we have been down similar paths with the olivine diogenite naming and 
the like, but this part of classifications and group naming still seems very 
loose to me.

John

 Hi John, and list,
 
 As to the ungrouped HaH 180, and Deakin 001, it has been suggested
 that both represent samples of a new and previously unsampled parent
 body. If that holds to be true, they will never get a LL or L
 classification. Ungrouped just means that a sample can't be
 assigned to any of the established groups, and that means also
 that they do most probably represent a unique parent body. Now,
 if we find three more meteorites like HaH 180, or Deakin 001,
 scientists will most likely create a new group, and then these
 samples won't be ungrouped, any longer.
 
 The term anomalous is used for meteorites that actually can be
 assigned to an existing group, but that differ in some aspects from
 the other known members of that group. Thus, HaH 180 isn't anomalous,
 it's simply ungrouped.
 
 Short: an ungrouped chondrite most probably stems from an asteroid
 that hasn't been sampled so far. An anomalous LL, for example, is
 most probably from the LL parent body/asteroid, but it differs from
 the other LL members in some respect. The petrologic grades have
 nothing to do with that, and of course an ungrouped chondrite can
 be a 3.5, or a plain 6.
 
 Hope this helps ;-)
 
 Best,
 Norbert
 
 A puzzled John wrote:
 
  Hello all,
 
  I've always been intrigued but puzzled about the classification of a few
  ordinary chondrites into the black hole of assigned classification
  names...ungrouped and/or anomalous. Some are specified with petrologic
  assignments and others without. Ebay on occasion offers us Hah
  180 that is  classified as an anomalous 3.5 ordinary chondrite and
  Dhofar 535 that is classified as ungrouped, and without a petrologic
  designation in its' description. According to David's site below...Hah
  180 is similar to Deakin 001. And there maybe others I am not thinking
  of. Oxygen isotopes and weathering seem to be some of the key factors...
  and as stated on David's site they may come from a proximity close to
  where enstatite chondrites were formed, and in my opinion their appearance
  makes them at least look like some  of the EL3's out there.
 
  Does anyone know what the latest theory is for these and will
  they one day
  get an official LL3 to 3.5 anomalous label which would finally
  give them a
  home? Seems to me to call them anything else puts them/keeps them in
  classification limbo.
 
 
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Re: AW: [meteorite-list] Anomalous and Ungrouped Ordinary Chondrites

2003-10-19 Thread j . divelbiss
Norbert,

I didn't read your comment very closely. It looks like you are saying it 
takes 5 samples to make a group. Where does that criteria come from? I know 
you are involved with the Society...so maybe there are known guidelines after 
all. thanx in advance.

John

 Hi John, and list,
 
 As to the ungrouped HaH 180, and Deakin 001, it has been suggested
 that both represent samples of a new and previously unsampled parent
 body. If that holds to be true, they will never get a LL or L
 classification. Ungrouped just means that a sample can't be
 assigned to any of the established groups, and that means also
 that they do most probably represent a unique parent body. Now,
 if we find three more meteorites like HaH 180, or Deakin 001,
 scientists will most likely create a new group, and then these
 samples won't be ungrouped, any longer.
 
 The term anomalous is used for meteorites that actually can be
 assigned to an existing group, but that differ in some aspects from
 the other known members of that group. Thus, HaH 180 isn't anomalous,
 it's simply ungrouped.
 
 Short: an ungrouped chondrite most probably stems from an asteroid
 that hasn't been sampled so far. An anomalous LL, for example, is
 most probably from the LL parent body/asteroid, but it differs from

 the other LL members in some respect. The petrologic grades have
 nothing to do with that, and of course an ungrouped chondrite can
 be a 3.5, or a plain 6.
 
 Hope this helps ;-)
 
 Best,
 Norbert
 
 A puzzled John wrote:
 
  Hello all,
 
  I've always been intrigued but puzzled about the classification of a few
  ordinary chondrites into the black hole of assigned classification
  names...ungrouped and/or anomalous. Some are specified with petrologic
  assignments and others without. Ebay on occasion offers us Hah
  180 that is  classified as an anomalous 3.5 ordinary chondrite and
  Dhofar 535 that is classified as ungrouped, and without a petrologic
  designation in its' description. According to David's site below...Hah
  180 is similar to Deakin 001. And there maybe others I am not thinking
  of. Oxygen isotopes and weathering seem to be some of the key factors...
  and as stated on David's site they may come from a proximity close to
  where enstatite chondrites were formed, and in my opinion their appearance
  makes them at least look like some  of the EL3's out there.
 
  Does anyone know what the latest theory is for these and will
  they one day
  get an official LL3 to 3.5 anomalous label which would finally
  give them a
  home? Seems to me to call them anything else puts them/keeps them in
  classification limbo.
 

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Re: AW: [meteorite-list] Anomalous and Ungrouped Ordinary Chondrites

2003-10-19 Thread Jeff Grossman
Norbert stated the facts well about ungrouped and anomalous chondrites.

There are no rules or guidelines for grouping meteorites.  However, a lot 
of researchers subscribe to the idea, which I think originated with John 
Wasson, that it takes 5 to sufficiently define the properties of a bunch of 
related meteorites that a name could be proposed.  The Editors of the 
Meteoritical Bulletin and the Catalogue of Meteorites probably wouldn't 
endorse a group-name if there were less than 5.  Of course, there are 
researchers who really want to be the ones to coin new names, and they 
sometimes get a bit hasty.  Anyway, for smaller sets of meteorites, the 
term grouplet is preferred by many, as is the suffix -like, each 
modifying the name of the best-known member.

jeff

At 11:19 PM 10/19/2003 +, [EMAIL PROTECTED] wrote:
Norbert,

I didn't read your comment very closely. It looks like you are saying it
takes 5 samples to make a group. Where does that criteria come from? I know
you are involved with the Society...so maybe there are known guidelines after
all. thanx in advance.
John

 Hi John, and list,

 As to the ungrouped HaH 180, and Deakin 001, it has been suggested
 that both represent samples of a new and previously unsampled parent
 body. If that holds to be true, they will never get a LL or L
 classification. Ungrouped just means that a sample can't be
 assigned to any of the established groups, and that means also
 that they do most probably represent a unique parent body. Now,
 if we find three more meteorites like HaH 180, or Deakin 001,
 scientists will most likely create a new group, and then these
 samples won't be ungrouped, any longer.

 The term anomalous is used for meteorites that actually can be
 assigned to an existing group, but that differ in some aspects from
 the other known members of that group. Thus, HaH 180 isn't anomalous,
 it's simply ungrouped.

 Short: an ungrouped chondrite most probably stems from an asteroid
 that hasn't been sampled so far. An anomalous LL, for example, is
 most probably from the LL parent body/asteroid, but it differs from
 the other LL members in some respect. The petrologic grades have
 nothing to do with that, and of course an ungrouped chondrite can
 be a 3.5, or a plain 6.

 Hope this helps ;-)

 Best,
 Norbert

 A puzzled John wrote:

  Hello all,
 
  I've always been intrigued but puzzled about the classification of a few
  ordinary chondrites into the black hole of assigned classification
  names...ungrouped and/or anomalous. Some are specified with petrologic
  assignments and others without. Ebay on occasion offers us Hah
  180 that is  classified as an anomalous 3.5 ordinary chondrite and
  Dhofar 535 that is classified as ungrouped, and without a petrologic
  designation in its' description. According to David's site below...Hah
  180 is similar to Deakin 001. And there maybe others I am not thinking
  of. Oxygen isotopes and weathering seem to be some of the key factors...
  and as stated on David's site they may come from a proximity close to
  where enstatite chondrites were formed, and in my opinion their 
appearance
  makes them at least look like some  of the EL3's out there.
 
  Does anyone know what the latest theory is for these and will
  they one day
  get an official LL3 to 3.5 anomalous label which would finally
  give them a
  home? Seems to me to call them anything else puts them/keeps them in
  classification limbo.


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Dr. Jeffrey N. Grossman   phone: (703) 648-6184
US Geological Survey  fax:   (703) 648-6383
954 National Center
Reston, VA 20192, USA


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