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Volumn 327, Issue , 2009, Pages 317-341

From Rodinia to Pangaea: Ophiolites from NW Iberia as witness for a long-lived continental margin

Author keywords

[No Author keywords available]

Indexed keywords

BACKARC BASIN; CONTINENTAL MARGIN; GEOCHEMISTRY; GEOCHRONOLOGY; GONDWANA; HERCYNIAN OROGENY; IAPETUS OCEAN; ISLAND ARC; LITHOLOGY; MID-OCEAN RIDGE BASALT; OCEANIC CRUST; OPHIOLITE; PALEOGEOGRAPHY; PLATE TECTONICS; RODINIA; SUBDUCTION ZONE; SUTURE ZONE; ULTRAHIGH TEMPERATURE METAMORPHISM;

EID: 75249098533     PISSN: 03058719     EISSN: None     Source Type: Book Series    
DOI: 10.1144/SP327.14     Document Type: Article
Times cited : (28)

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    • The application of a Th-Hf-Ta diagram to problems of tectomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province
    • Wood, D. A. 1980. The application of a Th-Hf-Ta diagram to problems of tectomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province. Earth and Planetary Science Letters, 50, 11-30.
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    • Wood, D.A.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.