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Volumn 8, Issue 3, 1989, Pages 497-516

The evolution of forearc structures along an oblique convergent margin, central Aleutian Arc

(2)  Ryan, Holly F a   Scholl, David W a  

a NONE

Author keywords

[No Author keywords available]

Indexed keywords

FOREARC; OBLIQUE CONVERGE; SHEAR ZONE; STRUCTURAL EVOLUTION; TERTIARY; UNDERTHRUSTING;

EID: 0024483604     PISSN: 02787407     EISSN: 19449194     Source Type: Journal    
DOI: 10.1029/TC008i003p00497     Document Type: Article
Times cited : (67)

References (56)
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    • Terrane motion by strike‐slip faulting of forearc slivers
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    • (1983) Can. Mineral. , vol.21 , pp. 665-681
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    • (1984)
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    • (1984) J. Geophys. Res. , vol.89 , pp. 5849-5857
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    • Leg 112 Shipboard Scientists, Ocean Drilling Program Leg 112, Peru continental margin; 1, Tectonic history
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.