Breccias from the Lunar Highlands: Preliminary Petrographic Report on Apollo 16 Samples 60017 and 63335
Lunar samples 60017,4 and 63335,14 are composed of microbreccias and devitrified glass. These components are predominantly anorthositic, with the exception of a cryptocrystalline clast found in the microbreccia portion of 63335,14 which contains 2.7 percent potassium oxide and 66.7 percent silicon d...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 1973-01, Vol.179 (4068), p.71-74 |
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creator | Kridelbaugh, S. J. McKay, G. A. Weill, D. F. |
description | Lunar samples 60017,4 and 63335,14 are composed of microbreccias and devitrified glass. These components are predominantly anorthositic, with the exception of a cryptocrystalline clast found in the microbreccia portion of 63335,14 which contains 2.7 percent potassium oxide and 66.7 percent silicon dioxide. The samples have been subjected to extreme shock and thermal metamorphism. The parent materials of the microbreccias include both a coarsegrained anorthosite and a fine-grained subophitic anorthositic gabbro. |
doi_str_mv | 10.1126/science.179.4068.71 |
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J. ; McKay, G. A. ; Weill, D. F.</creator><creatorcontrib>Kridelbaugh, S. J. ; McKay, G. A. ; Weill, D. F.</creatorcontrib><description>Lunar samples 60017,4 and 63335,14 are composed of microbreccias and devitrified glass. These components are predominantly anorthositic, with the exception of a cryptocrystalline clast found in the microbreccia portion of 63335,14 which contains 2.7 percent potassium oxide and 66.7 percent silicon dioxide. The samples have been subjected to extreme shock and thermal metamorphism. The parent materials of the microbreccias include both a coarsegrained anorthosite and a fine-grained subophitic anorthositic gabbro.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.179.4068.71</identifier><identifier>PMID: 17731632</identifier><language>eng</language><publisher>United States: American Association for the Advancement of Science</publisher><subject>Anorthosite ; Basalt ; Breccia ; Gabbro ; Highlands ; Impact craters ; Olivine ; Plagioclase ; Rocks ; Spinel</subject><ispartof>Science (American Association for the Advancement of Science), 1973-01, Vol.179 (4068), p.71-74</ispartof><rights>Copyright 1973 American Association for the Advancement of Science</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c385t-766f1771498505a77ee06c268d22518e99aab7e3e567d9e58350881b195774a53</citedby><cites>FETCH-LOGICAL-c385t-766f1771498505a77ee06c268d22518e99aab7e3e567d9e58350881b195774a53</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1734951$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1734951$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,2871,2872,27903,27904,57995,58228</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/17731632$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Kridelbaugh, S. 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The parent materials of the microbreccias include both a coarsegrained anorthosite and a fine-grained subophitic anorthositic gabbro.</description><subject>Anorthosite</subject><subject>Basalt</subject><subject>Breccia</subject><subject>Gabbro</subject><subject>Highlands</subject><subject>Impact craters</subject><subject>Olivine</subject><subject>Plagioclase</subject><subject>Rocks</subject><subject>Spinel</subject><issn>0036-8075</issn><issn>1095-9203</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1973</creationdate><recordtype>article</recordtype><recordid>eNp9kUFvEzEQhS1ERUPhF4CQT3Da1LMTe2xupQJaKRJVgbPlOJNkq914sTcH_j2OEglOnEaa-eZp3jwh3oCaA7TmusSO95HnQG6-UMbOCZ6JGSinG9cqfC5mSqFprCJ9KV6W8qRUnTl8IS6BCMFgOxPbT5lj7EKRm5wGOe1YLg_7kOVdt931Yb8uH-VD5r4butr9LR94ymmbw7jronzkMeVJpr28GVPfJwlGfg_D2HORRikgWQWkQUT9SlxsQl_49bleiZ9fPv-4vWuW377e394sm4hWTw0Zs6nHwcJZrXQgYlYmtsau21aDZedCWBEja0Nrx9qiVtbCCpwmWgSNV-LDSXfM6deBy-SHrkTuqxVOh-IJq3FjHFXy_X_JFqxFpKMknsCYUymZN37M3VCf4UH5YxL-nISvSfhjEp6gbr07yx9WA6__7pxfX4G3J-CpTCn_M8eF04B_AD8bjBI</recordid><startdate>19730105</startdate><enddate>19730105</enddate><creator>Kridelbaugh, S. J.</creator><creator>McKay, G. A.</creator><creator>Weill, D. F.</creator><general>American Association for the Advancement of Science</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope><scope>7X8</scope></search><sort><creationdate>19730105</creationdate><title>Breccias from the Lunar Highlands: Preliminary Petrographic Report on Apollo 16 Samples 60017 and 63335</title><author>Kridelbaugh, S. J. ; McKay, G. A. ; Weill, D. F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c385t-766f1771498505a77ee06c268d22518e99aab7e3e567d9e58350881b195774a53</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1973</creationdate><topic>Anorthosite</topic><topic>Basalt</topic><topic>Breccia</topic><topic>Gabbro</topic><topic>Highlands</topic><topic>Impact craters</topic><topic>Olivine</topic><topic>Plagioclase</topic><topic>Rocks</topic><topic>Spinel</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kridelbaugh, S. J.</creatorcontrib><creatorcontrib>McKay, G. A.</creatorcontrib><creatorcontrib>Weill, D. 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F.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Breccias from the Lunar Highlands: Preliminary Petrographic Report on Apollo 16 Samples 60017 and 63335</atitle><jtitle>Science (American Association for the Advancement of Science)</jtitle><addtitle>Science</addtitle><date>1973-01-05</date><risdate>1973</risdate><volume>179</volume><issue>4068</issue><spage>71</spage><epage>74</epage><pages>71-74</pages><issn>0036-8075</issn><eissn>1095-9203</eissn><abstract>Lunar samples 60017,4 and 63335,14 are composed of microbreccias and devitrified glass. These components are predominantly anorthositic, with the exception of a cryptocrystalline clast found in the microbreccia portion of 63335,14 which contains 2.7 percent potassium oxide and 66.7 percent silicon dioxide. The samples have been subjected to extreme shock and thermal metamorphism. The parent materials of the microbreccias include both a coarsegrained anorthosite and a fine-grained subophitic anorthositic gabbro.</abstract><cop>United States</cop><pub>American Association for the Advancement of Science</pub><pmid>17731632</pmid><doi>10.1126/science.179.4068.71</doi><tpages>4</tpages></addata></record> |
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source | American Association for the Advancement of Science; Jstor Complete Legacy |
subjects | Anorthosite Basalt Breccia Gabbro Highlands Impact craters Olivine Plagioclase Rocks Spinel |
title | Breccias from the Lunar Highlands: Preliminary Petrographic Report on Apollo 16 Samples 60017 and 63335 |
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