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An hexahedrite meteorite from the Campo del Cielo Fall
Aimed to clarify the shower of Campo del Cielo with respect to the presence of a large number of hexahedrites in the shower of Campo del Cielo, we have studied a piece that belongs to the Campo del Cielo meteorite Fall by X-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive...
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Published in: | Planetary and space science 2006-03, Vol.54 (3), p.303-309 |
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creator | Cabanillas, E.D. Palacios, T.A. |
description | Aimed to clarify the shower of Campo del Cielo with respect to the presence of a large number of hexahedrites in the shower of Campo del Cielo, we have studied a piece that belongs to the Campo del Cielo meteorite Fall by X-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDS), chemical analysis, Mössbauer spectroscopy (MS), and optical metallography. The studies showed that it is an
HIIA iron hexahedrite meteorite of 94.6
wt% Fe, 5.4
wt% Ni and 370
ppm of C, consisting of a kamacite matrix with small inclusions of iron–nickel phosphides. We have found Neumann bands differentiated from scarce taenite streaks and found that taenite is a path walk for corrosion. We also mention the approximate present localization of some of the principal pieces of the fall. |
doi_str_mv | 10.1016/j.pss.2005.11.002 |
format | article |
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HIIA iron hexahedrite meteorite of 94.6
wt% Fe, 5.4
wt% Ni and 370
ppm of C, consisting of a kamacite matrix with small inclusions of iron–nickel phosphides. We have found Neumann bands differentiated from scarce taenite streaks and found that taenite is a path walk for corrosion. We also mention the approximate present localization of some of the principal pieces of the fall.</description><identifier>ISSN: 0032-0633</identifier><identifier>EISSN: 1873-5088</identifier><identifier>DOI: 10.1016/j.pss.2005.11.002</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Campo del Cielo ; Hexaedrites ; Iron meteorite</subject><ispartof>Planetary and space science, 2006-03, Vol.54 (3), p.303-309</ispartof><rights>2005 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c390t-c952fbbb4a9ff1b24570cadc0593b406d93c142f05034aefccc88c6ae0159d3b3</citedby><cites>FETCH-LOGICAL-c390t-c952fbbb4a9ff1b24570cadc0593b406d93c142f05034aefccc88c6ae0159d3b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Cabanillas, E.D.</creatorcontrib><creatorcontrib>Palacios, T.A.</creatorcontrib><title>An hexahedrite meteorite from the Campo del Cielo Fall</title><title>Planetary and space science</title><description>Aimed to clarify the shower of Campo del Cielo with respect to the presence of a large number of hexahedrites in the shower of Campo del Cielo, we have studied a piece that belongs to the Campo del Cielo meteorite Fall by X-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDS), chemical analysis, Mössbauer spectroscopy (MS), and optical metallography. The studies showed that it is an
HIIA iron hexahedrite meteorite of 94.6
wt% Fe, 5.4
wt% Ni and 370
ppm of C, consisting of a kamacite matrix with small inclusions of iron–nickel phosphides. We have found Neumann bands differentiated from scarce taenite streaks and found that taenite is a path walk for corrosion. We also mention the approximate present localization of some of the principal pieces of the fall.</description><subject>Campo del Cielo</subject><subject>Hexaedrites</subject><subject>Iron meteorite</subject><issn>0032-0633</issn><issn>1873-5088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqNkD1PwzAQQC0EEqXwA9gysSWcP-LYYqoiCkiVWGC2HOesukqaYqcI_j0pZQamu-G9O-kRck2hoEDl7abYpVQwgLKgtABgJ2RGVcXzEpQ6JTMAznKQnJ-Ti5Q2ACAlq2ZELrbZGj_sGtsYRsx6HHH43nwc-mxcY1bbfjdkLXZZHbAbsqXtukty5m2X8Opnzsnr8v6lfsxXzw9P9WKVO65hzJ0umW-aRljtPW2YKCtwtnVQat4IkK3mjgrmoQQuLHrnnFJOWgRa6pY3fE5ujnd3cXjbYxpNH5LDrrNbHPbJMKUlVVz8A5x-Cq3-BGklFJdSTyA9gi4OKUX0ZhdDb-OnoWAOzc3GTM3Nobmh1EzNJ-fu6ODU5D1gNMkF3DpsQ0Q3mnYIv9hfzAaIhA</recordid><startdate>20060301</startdate><enddate>20060301</enddate><creator>Cabanillas, E.D.</creator><creator>Palacios, T.A.</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>7U5</scope><scope>8FD</scope><scope>L7M</scope><scope>H8D</scope></search><sort><creationdate>20060301</creationdate><title>An hexahedrite meteorite from the Campo del Cielo Fall</title><author>Cabanillas, E.D. ; Palacios, T.A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c390t-c952fbbb4a9ff1b24570cadc0593b406d93c142f05034aefccc88c6ae0159d3b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Campo del Cielo</topic><topic>Hexaedrites</topic><topic>Iron meteorite</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cabanillas, E.D.</creatorcontrib><creatorcontrib>Palacios, T.A.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Aerospace Database</collection><jtitle>Planetary and space science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cabanillas, E.D.</au><au>Palacios, T.A.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>An hexahedrite meteorite from the Campo del Cielo Fall</atitle><jtitle>Planetary and space science</jtitle><date>2006-03-01</date><risdate>2006</risdate><volume>54</volume><issue>3</issue><spage>303</spage><epage>309</epage><pages>303-309</pages><issn>0032-0633</issn><eissn>1873-5088</eissn><abstract>Aimed to clarify the shower of Campo del Cielo with respect to the presence of a large number of hexahedrites in the shower of Campo del Cielo, we have studied a piece that belongs to the Campo del Cielo meteorite Fall by X-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDS), chemical analysis, Mössbauer spectroscopy (MS), and optical metallography. The studies showed that it is an
HIIA iron hexahedrite meteorite of 94.6
wt% Fe, 5.4
wt% Ni and 370
ppm of C, consisting of a kamacite matrix with small inclusions of iron–nickel phosphides. We have found Neumann bands differentiated from scarce taenite streaks and found that taenite is a path walk for corrosion. We also mention the approximate present localization of some of the principal pieces of the fall.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.pss.2005.11.002</doi><tpages>7</tpages></addata></record> |
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subjects | Campo del Cielo Hexaedrites Iron meteorite |
title | An hexahedrite meteorite from the Campo del Cielo Fall |
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