KREEP Rocks
KREEP rocks with high contents of K, REE and P were first recognized in Apollo-12 samples, and it was confirmed later that there were KREEP rock fragments in all of the Apollo samples, particularly in Apollo-12 and -14 samples. The KREEP rocks distributed on the lunar surface are the very important...
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| Veröffentlicht in: | Acta geochimica 2004, Vol.23 (1), p.65-70 |
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| container_title | Acta geochimica |
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| creator | 邹永廖 徐琳 欧阳自远 |
| description | KREEP rocks with high contents of K, REE and P were first recognized in Apollo-12 samples, and it was confirmed later that there were KREEP rock fragments in all of the Apollo samples, particularly in Apollo-12 and -14 samples. The KREEP rocks distributed on the lunar surface are the very important objects of study on the evolution of the moon, as well as to evaluate the utilization prospect of REE in KREEP rocks. Based on previous studies and lunar exploration data, the authors analyzed the chemical and mineral characteristics of KREEP rocks, the abundance of Th on the lunar surface materials, the correlation between Th and REE of KREEP rocks in abundance, studied the distribution regions of KREEP rocks on the lunar surface, and further evaluated the utilization prospect of REE in KREEP rocks. |
| doi_str_mv | 10.1007/bf02841138 |
| format | Article |
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The KREEP rocks distributed on the lunar surface are the very important objects of study on the evolution of the moon, as well as to evaluate the utilization prospect of REE in KREEP rocks. Based on previous studies and lunar exploration data, the authors analyzed the chemical and mineral characteristics of KREEP rocks, the abundance of Th on the lunar surface materials, the correlation between Th and REE of KREEP rocks in abundance, studied the distribution regions of KREEP rocks on the lunar surface, and further evaluated the utilization prospect of REE in KREEP rocks.</description><identifier>ISSN: 1000-9426</identifier><identifier>ISSN: 2096-0956</identifier><identifier>EISSN: 1993-0364</identifier><identifier>EISSN: 2365-7499</identifier><identifier>DOI: 10.1007/bf02841138</identifier><language>eng</language><publisher>Dordrecht: Springer Nature B.V</publisher><subject>Abundance ; Evolution ; Geochemistry ; Kreep ; Lunar exploration ; Lunar rocks ; Lunar surface ; Moon ; Rock ; Rocks ; Utilization ; 克里普岩石 ; 月球勘探</subject><ispartof>Acta geochimica, 2004, Vol.23 (1), p.65-70</ispartof><rights>Institute of Geochemistry, Chinese Academy of Sciences 2004</rights><rights>Institute of Geochemistry, Chinese Academy of Sciences 2004.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3148-a3c582b878e59e1f316bd1428f9c4981cc6bc601e50b00c6936a27b8697feb273</citedby><cites>FETCH-LOGICAL-a3148-a3c582b878e59e1f316bd1428f9c4981cc6bc601e50b00c6936a27b8697feb273</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/85079X/85079X.jpg</thumbnail><link.rule.ids>314,780,784,4024,27923,27924,27925</link.rule.ids></links><search><creatorcontrib>邹永廖 徐琳 欧阳自远</creatorcontrib><title>KREEP Rocks</title><title>Acta geochimica</title><addtitle>Chinese Journal of Geochemistry</addtitle><description>KREEP rocks with high contents of K, REE and P were first recognized in Apollo-12 samples, and it was confirmed later that there were KREEP rock fragments in all of the Apollo samples, particularly in Apollo-12 and -14 samples. 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| ispartof | Acta geochimica, 2004, Vol.23 (1), p.65-70 |
| issn | 1000-9426 2096-0956 1993-0364 2365-7499 |
| language | eng |
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| source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
| subjects | Abundance Evolution Geochemistry Kreep Lunar exploration Lunar rocks Lunar surface Moon Rock Rocks Utilization 克里普岩石 月球勘探 |
| title | KREEP Rocks |
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