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Volumn 332, Issue 6035, 2011, Pages 1304-1307

Origin and evolution of prebiotic organic matter as inferred from the Tagish Lake meteorite

(20)  Herd, Christopher D K a   Blinova, Alexandra a   Simkus, Danielle N a   Huang, Yongsong b   Tarozo, Rafael b   Alexander, Conel M O'D c   Gyngard, Frank c   Nittler, Larry R c   Cody, George D c   Fogel, Marilyn L c   Kebukawa, Yoko c   Kilcoyne, A L David d   Hilts, Robert W e   Slater, Greg F f   Glavin, Daniel P g   Dworkin, Jason P g   Callahan, Michael P g   Elsila, Jamie E g   De Gregorio, Bradley T h,i   Stroud, Rhonda M i  


Author keywords

[No Author keywords available]

Indexed keywords

ORGANIC MATTER;

EID: 79958746238     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1203290     Document Type: Article
Times cited : (202)

References (41)
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    • note
    • Information on materials and methods is available as supporting material on Science Online.
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    • note
    • Hydrothermal alteration occurred early in the history of the carbonaceous chondrite parent bodies owing to accumulation of the heat of radioactive decay, so that liquid water was transiently present and percolated through the mineral matrix. The evidence for this process is preserved in mineral alterations. Furthermore, in the interior of the parent body, the temperature and pressure can rise high enough to produce hydropyrolysis of organic material.
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    • Where given, the errors are half the difference (standard error of the mean) between the compositions of two residues prepared from two separate aliquots of each specimen. Typically, the differences in elemental ratios and isotopic compositions are larger than the intrinsic measurement precisions. Where only one measurement was made, the uncertainties of the other samples are a guide to the likely uncertainties.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.