Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite

We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Geochimica et cosmochimica acta 2016-06, Vol.183, p.176-197
Hauptverfasser: Han, Jangmi, Brearley, Adrian J.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 197
container_issue
container_start_page 176
container_title Geochimica et cosmochimica acta
container_volume 183
creator Han, Jangmi
Brearley, Adrian J.
description We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core consists of polycrystalline aggregates of spinel and ±minor melilite showing equilibrated grain boundary textures. The intergrowth layer contains fine-grained diopside and spinel with minor anorthite with highly curved and embayed grain boundaries. The diopside rim consists of polycrystalline aggregates of diopside. The compositions of pyroxene change significantly outward from Al-Ti-rich diopside in contact with the spinel-rich core to Al-Ti-poor diopside next to the surrounding olivine of the AOA. Overall microstructural and chemical characteristics suggest that the spinel-rich core formed under equilibrium conditions whereas the intergrowth layer is the result of reactions that occurred under conditions that departed significantly from equilibrium. The remarkable changes in formation conditions of the CAI-like objects may have been achieved by transport and injection of refractory objects into a region of a partially-condensed, Ca,Ti-saturated gas which reacted with spinel and melilite to form Al-Ti-rich diopside. Crystallographically-oriented TiO2 nanoparticles decorate the grain boundaries between spinel grains and between spinel and Al-Ti-rich diopside grains. During the disequilibrium back-reaction of spinel with a partially-condensed, Ca,Ti-saturated gas, metastable TiO2 nanoparticles may have condensed by an epitaxial nucleation mechanism and grown on the surface of spinel. These TiO2 nanoparticles are disordered intergrowths of the two TiO2 polymorphs, anatase and rutile. These nanoparticles are inferred to have nucleated as anatase that underwent partial transformation into rutile. The local presence of the TiO2 nanoparticles and intergrowth of anatase and rutile imply that the disequilibrium back-reaction of spinel with the gas occurred on a short timescale, i.e., minutes to hours at maximum.
doi_str_mv 10.1016/j.gca.2016.04.011
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1825492443</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0016703716301703</els_id><sourcerecordid>1808724680</sourcerecordid><originalsourceid>FETCH-LOGICAL-c472t-4d9fb7672d385052f21182bb32bf7cc3245f9e6557436deb32671608c7591e43</originalsourceid><addsrcrecordid>eNqNUU1r3DAUFKWFbJP8gNx07MWuPi2bnpalTQIbcsldyPLzrra2tZW0ofkt_bN5y_ZcCgJpNG8G3gwhd5zVnPHm66HeeVcLfNZM1YzzD2TFWyOqTkv5kawYMpVh0lyRzzkfGGNGa7Yif56CTzGXdPLllNxEfVwQubCUTOOCcD5O8JuWPaQZ6X3IJaYASI40wZicR_xGN-vHago_gcb-AB61YaEOzxyhj2GgcQqvYQHqdrsEO1eAjinOZ1u63j6sjZHM0M2zrBn1-7gMKRS4IZ9GN2W4_Xtfk5cf3182D9X2-f5xs95WXhlRKjV0Y28aIwbZaqbFKDhvRd9L0Y_GeymUHjtotDZKNgPgf2N4w1pvdMdByWvy5WJ7TPHXCXKxc8gepsktEE_ZoplWnVBK_scow8xV0zIc5ZfRc7wZk7LHFGaX3ixn9lyZPViszJ4rs0xZrAw13y4awG1fAySbfYDFwxAShmqHGP6hfgfd_J6B</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1808724680</pqid></control><display><type>article</type><title>Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite</title><source>Elsevier ScienceDirect Journals Complete</source><creator>Han, Jangmi ; Brearley, Adrian J.</creator><creatorcontrib>Han, Jangmi ; Brearley, Adrian J.</creatorcontrib><description>We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core consists of polycrystalline aggregates of spinel and ±minor melilite showing equilibrated grain boundary textures. The intergrowth layer contains fine-grained diopside and spinel with minor anorthite with highly curved and embayed grain boundaries. The diopside rim consists of polycrystalline aggregates of diopside. The compositions of pyroxene change significantly outward from Al-Ti-rich diopside in contact with the spinel-rich core to Al-Ti-poor diopside next to the surrounding olivine of the AOA. Overall microstructural and chemical characteristics suggest that the spinel-rich core formed under equilibrium conditions whereas the intergrowth layer is the result of reactions that occurred under conditions that departed significantly from equilibrium. The remarkable changes in formation conditions of the CAI-like objects may have been achieved by transport and injection of refractory objects into a region of a partially-condensed, Ca,Ti-saturated gas which reacted with spinel and melilite to form Al-Ti-rich diopside. Crystallographically-oriented TiO2 nanoparticles decorate the grain boundaries between spinel grains and between spinel and Al-Ti-rich diopside grains. During the disequilibrium back-reaction of spinel with a partially-condensed, Ca,Ti-saturated gas, metastable TiO2 nanoparticles may have condensed by an epitaxial nucleation mechanism and grown on the surface of spinel. These TiO2 nanoparticles are disordered intergrowths of the two TiO2 polymorphs, anatase and rutile. These nanoparticles are inferred to have nucleated as anatase that underwent partial transformation into rutile. The local presence of the TiO2 nanoparticles and intergrowth of anatase and rutile imply that the disequilibrium back-reaction of spinel with the gas occurred on a short timescale, i.e., minutes to hours at maximum.</description><identifier>ISSN: 0016-7037</identifier><identifier>EISSN: 1872-9533</identifier><identifier>DOI: 10.1016/j.gca.2016.04.011</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Amoeboid olivine aggregates (AOAs) ; Calcium magnesium silicates ; Condensation ; Diopside ; Grain boundaries ; Nanoparticles ; Refractory phases ; Rutile ; Solar nebula ; Spinel ; Texture ; TiO2 nanoparticles ; Titanium dioxide ; Transport</subject><ispartof>Geochimica et cosmochimica acta, 2016-06, Vol.183, p.176-197</ispartof><rights>2016 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c472t-4d9fb7672d385052f21182bb32bf7cc3245f9e6557436deb32671608c7591e43</citedby><cites>FETCH-LOGICAL-c472t-4d9fb7672d385052f21182bb32bf7cc3245f9e6557436deb32671608c7591e43</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0016703716301703$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65534</link.rule.ids></links><search><creatorcontrib>Han, Jangmi</creatorcontrib><creatorcontrib>Brearley, Adrian J.</creatorcontrib><title>Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite</title><title>Geochimica et cosmochimica acta</title><description>We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core consists of polycrystalline aggregates of spinel and ±minor melilite showing equilibrated grain boundary textures. The intergrowth layer contains fine-grained diopside and spinel with minor anorthite with highly curved and embayed grain boundaries. The diopside rim consists of polycrystalline aggregates of diopside. The compositions of pyroxene change significantly outward from Al-Ti-rich diopside in contact with the spinel-rich core to Al-Ti-poor diopside next to the surrounding olivine of the AOA. Overall microstructural and chemical characteristics suggest that the spinel-rich core formed under equilibrium conditions whereas the intergrowth layer is the result of reactions that occurred under conditions that departed significantly from equilibrium. The remarkable changes in formation conditions of the CAI-like objects may have been achieved by transport and injection of refractory objects into a region of a partially-condensed, Ca,Ti-saturated gas which reacted with spinel and melilite to form Al-Ti-rich diopside. Crystallographically-oriented TiO2 nanoparticles decorate the grain boundaries between spinel grains and between spinel and Al-Ti-rich diopside grains. During the disequilibrium back-reaction of spinel with a partially-condensed, Ca,Ti-saturated gas, metastable TiO2 nanoparticles may have condensed by an epitaxial nucleation mechanism and grown on the surface of spinel. These TiO2 nanoparticles are disordered intergrowths of the two TiO2 polymorphs, anatase and rutile. These nanoparticles are inferred to have nucleated as anatase that underwent partial transformation into rutile. The local presence of the TiO2 nanoparticles and intergrowth of anatase and rutile imply that the disequilibrium back-reaction of spinel with the gas occurred on a short timescale, i.e., minutes to hours at maximum.</description><subject>Amoeboid olivine aggregates (AOAs)</subject><subject>Calcium magnesium silicates</subject><subject>Condensation</subject><subject>Diopside</subject><subject>Grain boundaries</subject><subject>Nanoparticles</subject><subject>Refractory phases</subject><subject>Rutile</subject><subject>Solar nebula</subject><subject>Spinel</subject><subject>Texture</subject><subject>TiO2 nanoparticles</subject><subject>Titanium dioxide</subject><subject>Transport</subject><issn>0016-7037</issn><issn>1872-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqNUU1r3DAUFKWFbJP8gNx07MWuPi2bnpalTQIbcsldyPLzrra2tZW0ofkt_bN5y_ZcCgJpNG8G3gwhd5zVnPHm66HeeVcLfNZM1YzzD2TFWyOqTkv5kawYMpVh0lyRzzkfGGNGa7Yif56CTzGXdPLllNxEfVwQubCUTOOCcD5O8JuWPaQZ6X3IJaYASI40wZicR_xGN-vHago_gcb-AB61YaEOzxyhj2GgcQqvYQHqdrsEO1eAjinOZ1u63j6sjZHM0M2zrBn1-7gMKRS4IZ9GN2W4_Xtfk5cf3182D9X2-f5xs95WXhlRKjV0Y28aIwbZaqbFKDhvRd9L0Y_GeymUHjtotDZKNgPgf2N4w1pvdMdByWvy5WJ7TPHXCXKxc8gepsktEE_ZoplWnVBK_scow8xV0zIc5ZfRc7wZk7LHFGaX3ixn9lyZPViszJ4rs0xZrAw13y4awG1fAySbfYDFwxAShmqHGP6hfgfd_J6B</recordid><startdate>20160615</startdate><enddate>20160615</enddate><creator>Han, Jangmi</creator><creator>Brearley, Adrian J.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20160615</creationdate><title>Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite</title><author>Han, Jangmi ; Brearley, Adrian J.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c472t-4d9fb7672d385052f21182bb32bf7cc3245f9e6557436deb32671608c7591e43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Amoeboid olivine aggregates (AOAs)</topic><topic>Calcium magnesium silicates</topic><topic>Condensation</topic><topic>Diopside</topic><topic>Grain boundaries</topic><topic>Nanoparticles</topic><topic>Refractory phases</topic><topic>Rutile</topic><topic>Solar nebula</topic><topic>Spinel</topic><topic>Texture</topic><topic>TiO2 nanoparticles</topic><topic>Titanium dioxide</topic><topic>Transport</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Han, Jangmi</creatorcontrib><creatorcontrib>Brearley, Adrian J.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Geochimica et cosmochimica acta</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Han, Jangmi</au><au>Brearley, Adrian J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite</atitle><jtitle>Geochimica et cosmochimica acta</jtitle><date>2016-06-15</date><risdate>2016</risdate><volume>183</volume><spage>176</spage><epage>197</epage><pages>176-197</pages><issn>0016-7037</issn><eissn>1872-9533</eissn><abstract>We have carried out a FIB/TEM study of refractory CAI-like objects in one AOA from the ALHA77307 CO3.0 chondrite. The CAI-like objects in the AOA consist of a zoned sequence with a spinel-rich core through an intergrowth layer of spinel and Al-Ti-rich diopside to a diopside rim. The spinel-rich core consists of polycrystalline aggregates of spinel and ±minor melilite showing equilibrated grain boundary textures. The intergrowth layer contains fine-grained diopside and spinel with minor anorthite with highly curved and embayed grain boundaries. The diopside rim consists of polycrystalline aggregates of diopside. The compositions of pyroxene change significantly outward from Al-Ti-rich diopside in contact with the spinel-rich core to Al-Ti-poor diopside next to the surrounding olivine of the AOA. Overall microstructural and chemical characteristics suggest that the spinel-rich core formed under equilibrium conditions whereas the intergrowth layer is the result of reactions that occurred under conditions that departed significantly from equilibrium. The remarkable changes in formation conditions of the CAI-like objects may have been achieved by transport and injection of refractory objects into a region of a partially-condensed, Ca,Ti-saturated gas which reacted with spinel and melilite to form Al-Ti-rich diopside. Crystallographically-oriented TiO2 nanoparticles decorate the grain boundaries between spinel grains and between spinel and Al-Ti-rich diopside grains. During the disequilibrium back-reaction of spinel with a partially-condensed, Ca,Ti-saturated gas, metastable TiO2 nanoparticles may have condensed by an epitaxial nucleation mechanism and grown on the surface of spinel. These TiO2 nanoparticles are disordered intergrowths of the two TiO2 polymorphs, anatase and rutile. These nanoparticles are inferred to have nucleated as anatase that underwent partial transformation into rutile. The local presence of the TiO2 nanoparticles and intergrowth of anatase and rutile imply that the disequilibrium back-reaction of spinel with the gas occurred on a short timescale, i.e., minutes to hours at maximum.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.gca.2016.04.011</doi><tpages>22</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0016-7037
ispartof Geochimica et cosmochimica acta, 2016-06, Vol.183, p.176-197
issn 0016-7037
1872-9533
language eng
recordid cdi_proquest_miscellaneous_1825492443
source Elsevier ScienceDirect Journals Complete
subjects Amoeboid olivine aggregates (AOAs)
Calcium magnesium silicates
Condensation
Diopside
Grain boundaries
Nanoparticles
Refractory phases
Rutile
Solar nebula
Spinel
Texture
TiO2 nanoparticles
Titanium dioxide
Transport
title Microstructural constraints on complex thermal histories of refractory CAI-like objects in an amoeboid olivine aggregate from the ALHA77307 CO3.0 chondrite
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-21T20%3A45%3A44IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Microstructural%20constraints%20on%20complex%20thermal%20histories%20of%20refractory%20CAI-like%20objects%20in%20an%20amoeboid%20olivine%20aggregate%20from%20the%20ALHA77307%20CO3.0%20chondrite&rft.jtitle=Geochimica%20et%20cosmochimica%20acta&rft.au=Han,%20Jangmi&rft.date=2016-06-15&rft.volume=183&rft.spage=176&rft.epage=197&rft.pages=176-197&rft.issn=0016-7037&rft.eissn=1872-9533&rft_id=info:doi/10.1016/j.gca.2016.04.011&rft_dat=%3Cproquest_cross%3E1808724680%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1808724680&rft_id=info:pmid/&rft_els_id=S0016703716301703&rfr_iscdi=true