Would not one expect tensile cracks to be radial and 'implosion' cracks
to be concentric around the inclusion?
All the best
Christian
Le 2022-07-02 06:17, Matt Kohn a écrit :
> Maybe I’m missing something, but I think some in situ
> quartz-to-coesite conversion is possible, albeit not an entire
> inclusion.
>
> For example, using either an almandine or pyrope host, at a final P-T
> condition of 700 °C, 3.5 GPa, quartz entrapped at 500 °C and 2 GPa
> would have a peak pressure of 2.83-2.85 GPa, which is within the
> coesite stability field. However, I agree if the entire quartz
> inclusion converted to coesite, the decrease in volume would drop the
> pressure back to quartz stability. So, the whole inclusion can’t
> convert to coesite. Rather, as pressure increases, enough quartz would
> convert to coesite to bring the (now composite inclusion) pressure to
> the quartz-coesite boundary. And it would stay there (increasing the
> amount of coesite as pressure increases and decreasing the amount as
> pressure decreases) until the host rock pressure decreased
> sufficiently that the coesite in the composite inclusion completely
> reverted to quartz.
>
> Many have commented on partial conversion of coesite inclusions to
> quartz during exhumation and buffering along the quartz-coesite
> boundary. But the same process must occur on the prograde path, too,
> if quartz is originally included at sufficiently high pressure.
>
> But that’s assuming only elastic behavior. Depending on the P-T
> condition of quartz entrapment, a garnet at coesite-stable pressures
> could experience high differential stress around a quartz inclusion
> (e.g., see Angel et al., 2015), potentially leading to failure of the
> garnet. This would immediately subject the quartz inclusion to
> coesite-stable conditions and convert it to coesite.
>
> So, getting back to original question, I agree that conversion of a
> quartz grain entirely to coesite would not happen. But couldn't some
> fracturing be prograde, and associated with high differential stresses
> around quartz inclusions? The quartz would then covert to coesite,
> leading to coesite inclusions surrounded by lots of fractures.
>
> A potential test might be if fracture patterns are different for
> garnet “implosion” vs. garnet “explosion”.
>
> Best,
>
> Matt
>
>
>> On Jul 1, 2022, at 2:42 PM, chopin <[log in to unmask]> wrote:
>>
>> The point was also clearly made earlier by, e.g., van der Molen and
>> van Roermund (Lithos 19, 317-324, 1986; The pressure path of solid
>> inclusions in minerals: the retention of coesite inclusions during
>> uplift), who conclude:
>> "Coesite included in garnet cannot have formed during progressive
>> metamorphism from quartz at lithostatic pressures below the coesite
>> stability field because of differential volume changes".
>> I hope this helps.
>> Christian
>>
>> ---
>> Christian Chopin [log in to unmask]
>> Laboratoire de Géologie
>> Ecole normale supérieure - CNRS UMR8538
>> 24 rue Lhomond
>> 75231 PARIS CEDEX 05
>> France
>>
>>
>>
>> Le 2022-07-01 11:00, Richard White a écrit :
>>> There are some more recent studies, but the work below nicely
>>> reinforces Christian's statement regarding coesite having to be
>>> included as coesite in general.
>>> P–V–T relationships and mineral equilibria in inclusions in minerals
>>> M Guiraud, R Powell 2006
>>> Earth and Planetary Science Letters 244 (3-4), 683-694
>>> Professor Richard White
>>> Head of School
>>> School of Earth & Environmental Sciences
>>> University of St Andrews
>>> Bute Building,
>>> Queen’s Terrace
>>> St Andrews, Fife KY16 9TS, UK
>>> Tel: +44 01334 464944
>>> On 30/06/2022, 20:26, "Metamorphic Studies Group on behalf of
>>> chopin"
>>> <[log in to unmask] on behalf of [log in to unmask]>
>>> wrote:
>>> Dear all,
>>> one point should be clear: considering thermal expansion and
>>> compressibility of quartz vs garnet, a quartz inclusion in garnet
>>> CANNOT
>>> convert to coesite upon increasing P and T. Trapped as quartz, it
>>> remains quartz, as examplified by UHP metapelitic garnets having
>>> quartz
>>> inclusions in their core and coesite inclusions in their rim.
>>> I do agree that garnet formation upon increasing P and T,
>>> especially at
>>> low T, may be more substantial than stated in the initial message.
>>> Yet,
>>> there is some truth in the concern expressed in that message:
>>> coesite
>>> inclusions in garnet are seldom abundant; actually they are
>>> profuse only
>>> in the Dora-Maira whiteschits, in pyrope crystals that formed,
>>> together
>>> with coesite, from talc+kyanite (in a coesite matrix), therefore a
>>> case
>>> where most of the garnet growth took place in the coesite field.
>>> Kind regards
>>> Christian
>>> ---
>>> Christian Chopin [log in to unmask]
>>> Laboratoire de Géologie
>>> Ecole normale supérieure - CNRS UMR8538
>>> 24 rue Lhomond
>>> 75231 PARIS CEDEX 05
>>> France
>>> Le 2022-06-30 20:19, Bruce Yardley a écrit :
>>> > Hi Martin, Pavel and all
>>> > This is a very interesting observation. Even if some garnet
>>> does grow
>>> > at ultra high-P it still would not account for coesite through
>>> the
>>> > bulk of the garnet. My suggestion, for what it's worth, is that
>>> garnet
>>> > may have recrystallised completely at ultra high-P so that the
>>> present
>>> > grains contain both old garnet material and any new material
>>> generated
>>> > at ultra high-P. We see this phenomenon in migmatite restites,
>>> where
>>> > garnets can be texturally quite different from those formed
>>> before the
>>> > onset of melting, still present at lower grade. I have also seen
>>> > examples where plagioclase in pelites completely recrystallised
>>> into
>>> > large porphyroblasts at the staurolite-out isograd, although the
>>> modal
>>> > abundance only increased very slightly. In these cases,
>>> > recrystallisation accompanies reactions that that involve a lot
>>> of the
>>> > rock and release fluid or melt. Can you say whether the
>>> > coesite-bearing garnet grains last formed while some other
>>> reaction
>>> > was going on, even if it did not generate much new garnet? At
>>> UHP
>>> > conditions alumiosilicates are much more soluble and this may
>>> make
>>> > recrystallisation easier.
>>> > Good wishes
>>> > Bruce
>>> >
>>> > Bruce Yardley
>>> > Emeritus Professor
>>> > School of Earth and Environment
>>> > University of Leeds
>>> > Leeds LS2 9JT
>>> > UK
>>> > Tel: +44(0)7745 132560
>>> >
>>> > https://www.lakedistrictgeology.co.uk/
>>> >
>>> > -------------------------
>>> >
>>> > FROM: Metamorphic Studies Group
>>> <[log in to unmask]> on
>>> > behalf of Pavel Pitra <[log in to unmask]>
>>> > SENT: 30 June 2022 17:48
>>> > TO: [log in to unmask]
>>> <[log in to unmask]>
>>> > SUBJECT: Re: [geo-metamorphism] how do coesite inclusions end up
>>> in
>>> > garnet?
>>> >
>>> > Hi Martin and all,
>>> >
>>> > I would tend to agree with Jarek that quartz inclusions may have
>>> > difficulties to convert to coesite, in particular if the
>>> excursion to
>>> > the coesite stability field is only of limited "extent" (both in
>>> time
>>> > and PT terms).
>>> >
>>> > On the other hand, I would at least partly disagree with the
>>> statement
>>> >
>>> > that "For a wide range of bulk compositions, mineral equilibria
>>> > modelling suggests garnet modes are generally quasi invariant
>>> above
>>> > about 2.4 GPa for a range of rocks types".
>>> >
>>> > This is true for eclogite-facies conditions (at least for
>>> metabasic
>>> > rocks). However, at lower temperatures garnet can definitely
>>> grow with
>>> >
>>> > increasing temperature, in particular in the lawsonite stability
>>> field
>>> >
>>> > (both in metapelitic and metabasic rocks), and even more so
>>> close to
>>> > the
>>> > upper T limit of lawsonite. This is nicely shown in Fig. 10 of
>>> Paola
>>> > Manzotti's recent paper on a new, cold, coesite-bearing unit in
>>> the
>>> > Dora-Maira massif
>>> >
>>> (https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fdoi.org%2F10.1007%2Fs00410-022-01923-8&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749071871%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=PUWEOs2qLqoVInSpgmct6X%2BQMbS7%2FLD0XmONv8FcvLk%3D&reserved=0).
>>> >
>>> > So I believe the PT path of the rocks can play an important
>>> role, and
>>> > perhaps at least some of the coesite-bearing rocks went through
>>> the
>>> > HP-LT conditions before the eclogite-facies peak. (That's why
>>> looking
>>> > at
>>> > the prograde PT paths is so important)
>>> >
>>> > Cheers,
>>> >
>>> > Pavel
>>> >
>>> > On 30/06/2022 18:02, Jaroslaw Majka wrote:
>>> >> Hi Martin,
>>> >>
>>> >> To follow up, I would ask even more straightforward
>>> (provocative?)
>>> >> question, namely whether quartz actually ever converts into
>>> coesite
>>> > if
>>> >> captured at low P or no?
>>> >>
>>> >> My observations from various UHP rocks and some reading I have
>>> done
>>> >> suggest that coesite should/would be a newly formed phase
>>> rather
>>> > than a
>>> >> pseudopmorph.
>>> >>
>>> >> Best,
>>> >> Jarek
>>> >>
>>> >> Sent from my iPhone
>>> >>
>>> >>> On 30 Jun 2022, at 17:46, Martin Hand
>>> <[log in to unmask]>
>>> > wrote:
>>> >>>
>>> >>>
>>> >>>
>>> >>> Hi folks,
>>> >>>
>>> >>> I’d be interested in your collective thoughts about coesite
>>> > inclusions
>>> >>> in garnet.
>>> >>>
>>> >>> For a wide range of bulk compositions, mineral equilibria
>>> modelling
>>> >
>>> >>> suggests garnet modes are generally quasi invariant above
>>> about 2.4
>>> >
>>> >>> GPa for a range of rocks types. Therefore in general, garnet
>>> >>> shouldn’t be able to capture coesite in an equilibrium
>>> system..
>>> >>>
>>> >>> So unless garnet nuceation is radically overstepped, the
>>> presence
>>> > of
>>> >>> coesite in garnet means captured quartz had to convert to
>>> coesite
>>> >>> after inclusion in garnet (?).
>>> >>>
>>> >>> If quartz inclusions in garnet convert to coesite, presumably
>>> > garnet
>>> >>> needs to deform (contract) to accommodate the c. 10% quartz to
>>> > coesite
>>> >>> volume change. So maybe(?) some of the ubiquitous fractures
>>> in
>>> > high-P
>>> >>> garnets are prograde strains.
>>> >>>
>>> >>> However looking in places like the Western Gneiss Complex, it
>>> seems
>>> >
>>> >>> that only an extremely small fraction of quartz inclusions in
>>> > garnet
>>> >>> converted to coesite (based on the prevalence of quartz
>>> inclusions
>>> >>> that show no microstructural evidence they were ever coesite).
>>> >>>
>>> >>> I guess a caveat to the bracketed statement is that coesite to
>>> > quartz
>>> >>> microstructures and their garnet host may have annealed,
>>> obscuring
>>> > the
>>> >>> former presence of abundant coesite. However the apparent
>>> paucity
>>> > of
>>> >>> evidence for coesite in the WGC (for example) seems logical,
>>> > because
>>> >>> the garnet load forms well down-P of coesite-in.
>>> >>>
>>> >>> Some papers demonstrate quartz in garnet can metastably
>>> persist
>>> > above
>>> >>> coesite-in. Perhaps this is generally the case and conversion
>>> of
>>> >>> quartz inclusions in garnet to coesite is the exception rather
>>> than
>>> >
>>> >>> the rule.
>>> >>>
>>> >>> I’m interested in what people think.
>>> >>>
>>> >>> martin
>>> >>>
>>> >>> Martin Hand
>>> >>>
>>> >>> Department of Earth Sciences
>>> >>>
>>> >>> University of Adelaide
>>> >>>
>>> >>> Phone: +61 (0)419 314 306
>>> >>>
>>> >>>
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.adelaide.edu.au%2Fdirectory%2Fmartin.hand&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749071871%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=6Yg2j2ro3n0B60q2spHyA6C098RROv1itebUPzaeH38%3D&reserved=0
>>> > [1]
>>> >>>
>>> >
>>> <https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.adelaide.edu.au%2Fdirectory%2Fmartin.hand&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749071871%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=6Yg2j2ro3n0B60q2spHyA6C098RROv1itebUPzaeH38%3D&reserved=0>
>>> >>>
>>> >>> CRICOS Provider Number 00123M
>>> >>>
>>> >>> -----------------------------------------------------------
>>> >>>
>>> >>> IMPORTANT: This message may contain confidential or legally
>>> > privileged
>>> >>> information. If you think it was sent to you by mistake,
>>> please
>>> > delete
>>> >>> all copies and advise the sender. For the purposes of the SPAM
>>> Act
>>> >>> 2003, this email is authorised by The University
>>> >>>
>>> >>> image001.jpg
>>> >>>
>>> >>>
>>> >>>
>>> >
>>> ------------------------------------------------------------------------
>>> >>>
>>> >>> To unsubscribe from the GEO-METAMORPHISM list, click the
>>> following
>>> > link:
>>> >>>
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&reserved=0
>>> > [2]
>>> >>>
>>> >
>>> <https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&reserved=0>
>>> >
>>> >>>
>>> >>>
>>> >> Page Title
>>> >>
>>> >>
>>> >>
>>> >>
>>> >>
>>> >>
>>> >>
>>> >> När du har kontakt med oss på Uppsala universitet med e-post så
>>> > innebär
>>> >> det att vi behandlar dina personuppgifter. För att läsa mer om
>>> hur
>>> > vi
>>> >> gör det kan du läsa här:
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.uu.se%2Fom-uu%2Fdataskydd-personuppgifter%2F&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=A90f2bC1GB68zPqGpNlzgXi7T6vmOpLqv7FDtQ%2FzJGA%3D&reserved=0
>>> > [3]
>>> >>
>>> >> E-mailing Uppsala University means that we will process your
>>> > personal
>>> >> data. For more information on how this is performed, please
>>> read
>>> > here:
>>> >>
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.uu.se%2Fen%2Fabout-uu%2Fdata-protection-policy&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=KcyQLGoDLnwjkRcVEfEJjpNxZwyxSUQl3fZwKaRNYgk%3D&reserved=0
>>> > [4]
>>> >>
>>> >
>>> ------------------------------------------------------------------------
>>> >>
>>> >> To unsubscribe from the GEO-METAMORPHISM list, click the
>>> following
>>> > link:
>>> >>
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&reserved=0
>>> > [2]
>>> >>
>>> >
>>> <https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&reserved=0>
>>> >
>>> >>
>>> >>
>>> >
>>> >
>>> ########################################################################
>>> >
>>> > To unsubscribe from the GEO-METAMORPHISM list, click the
>>> following
>>> > link:
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&reserved=0
>>> >
>>> > This message was issued to members of
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.jiscmail.ac.uk%2FGEO-METAMORPHISM&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=nP7HVAESjAFDVcqDEmzDYonAuu6jRLGMrkqpb%2B710wQ%3D&reserved=0
>>> > [5], a mailing list hosted by
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.jiscmail.ac.uk%2F&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=jEUAeIx8gK6me7deOeT4O47jcALoFoLSqebj6bXNjis%3D&reserved=0
>>> > [6], terms & conditions are available at
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fpolicyandsecurity%2F&data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&sdata=CspRFyVvwKvjMqg1SGioRljwwOJrIYGWLok%2Fv3HrdlI%3D&reserved=0
>>> > [7]
>>> >
>>> > -------------------------
>>> >
>>> > To unsubscribe from the GEO-METAMORPHISM list, click the
>>> following
>>> > link:
>>> >
>>> https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
>>> >
>>> >
>>> > Links:
>>> > ------
>>> > [1]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.adelaide.edu.au%2Fdirectory%2Fmartin.hand&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749071871%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=6Yg2j2ro3n0B60q2spHyA6C098RROv1itebUPzaeH38%3D&amp;reserved=0
>>> > [2]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fcgi-bin%2FWA-JISC.exe%3FSUBED1%3DGEO-METAMORPHISM%26A%3D1&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=BMCWY5e7Qa4Awss3NZxE6%2BTivJrNlEG1zlbduvgkO0c%3D&amp;reserved=0
>>> > [3]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.uu.se%2Fom-uu%2Fdataskydd-personuppgifter%2F&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=A90f2bC1GB68zPqGpNlzgXi7T6vmOpLqv7FDtQ%2FzJGA%3D&amp;reserved=0
>>> > [4]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.uu.se%2Fen%2Fabout-uu%2Fdata-protection-policy&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=KcyQLGoDLnwjkRcVEfEJjpNxZwyxSUQl3fZwKaRNYgk%3D&amp;reserved=0
>>> > [5]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.jiscmail.ac.uk%2FGEO-METAMORPHISM&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=nP7HVAESjAFDVcqDEmzDYonAuu6jRLGMrkqpb%2B710wQ%3D&amp;reserved=0
>>> > [6]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=http%3A%2F%2Fwww.jiscmail.ac.uk%2F&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=jEUAeIx8gK6me7deOeT4O47jcALoFoLSqebj6bXNjis%3D&amp;reserved=0
>>> > [7]
>>> >
>>> https://eur03.safelinks.protection.outlook.com/?url=https%3A%2F%2Fwww.jiscmail.ac.uk%2Fpolicyandsecurity%2F&amp;data=05%7C01%7CB.W.D.Yardley%40leeds.ac.uk%7Ce1d0b185a7a4466f146f08da5ab881f3%7Cbdeaeda8c81d45ce863e5232a535b7cb%7C1%7C0%7C637922045749228112%7CUnknown%7CTWFpbGZsb3d8eyJWIjoiMC4wLjAwMDAiLCJQIjoiV2luMzIiLCJBTiI6Ik1haWwiLCJXVCI6Mn0%3D%7C3000%7C%7C%7C&amp;sdata=CspRFyVvwKvjMqg1SGioRljwwOJrIYGWLok%2Fv3HrdlI%3D&amp;reserved=0
>>>
>>> ########################################################################
>>> To unsubscribe from the GEO-METAMORPHISM list, click the following
>>> link:
>>>
>>> https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
>>> This message was issued to members of
>>> www.jiscmail.ac.uk/GEO-METAMORPHISM, a mailing list hosted by
>>> www.jiscmail.ac.uk, terms & conditions are available at
>>> https://www.jiscmail.ac.uk/policyandsecurity/
>>> ########################################################################
>>> To unsubscribe from the GEO-METAMORPHISM list, click the following
>>> link:
>>> https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
>>> This message was issued to members of
>>> www.jiscmail.ac.uk/GEO-METAMORPHISM, a mailing list hosted by
>>> www.jiscmail.ac.uk, terms & conditions are available at
>>> https://www.jiscmail.ac.uk/policyandsecurity/
>>
>> ########################################################################
>>
>> To unsubscribe from the GEO-METAMORPHISM list, click the following
>> link:
>> https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
>>
>> This message was issued to members of
>> www.jiscmail.ac.uk/GEO-METAMORPHISM, a mailing list hosted by
>> www.jiscmail.ac.uk, terms & conditions are available at
>> https://www.jiscmail.ac.uk/policyandsecurity/
>
> ########################################################################
>
> To unsubscribe from the GEO-METAMORPHISM list, click the following
> link:
> https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
>
> This message was issued to members of
> www.jiscmail.ac.uk/GEO-METAMORPHISM, a mailing list hosted by
> www.jiscmail.ac.uk, terms & conditions are available at
> https://www.jiscmail.ac.uk/policyandsecurity/
########################################################################
To unsubscribe from the GEO-METAMORPHISM list, click the following link:
https://www.jiscmail.ac.uk/cgi-bin/WA-JISC.exe?SUBED1=GEO-METAMORPHISM&A=1
This message was issued to members of www.jiscmail.ac.uk/GEO-METAMORPHISM, a mailing list hosted by www.jiscmail.ac.uk, terms & conditions are available at https://www.jiscmail.ac.uk/policyandsecurity/
|