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Volumn 283, Issue 5408, 1999, Pages 1652-1653

A thermal balancing act

Author keywords

[No Author keywords available]

Indexed keywords

GEOLOGY; HEAT TRANSFER; PHYSICS; PRESSURE; PRIORITY JOURNAL; SHORT SURVEY; TEMPERATURE; THERMAL CONDUCTIVITY;

EID: 0033548707     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.283.5408.1652     Document Type: Short Survey
Times cited : (5)

References (33)
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    • note
    • D″, the deepest part of the mantle, about 200 km wide, constitutes the thermal boundary between the convecting core and the convecting mantle. The thermal gradient of D″ is high, as shown in the first figure. The composition of D″ is thought to be the same as that of the mantle; it is possible, however, that D‴ has a composition that departs slightly from that of the mantle rock. The boundary separating the core from D″ is called the CMB (core-mantle boundary).
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.