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Volumn 79, Issue 3, 1984, Pages 779-798

Anomalous seismic crustal structure of oceanic fracture zones

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Indexed keywords


EID: 84986409014     PISSN: 00168009     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.1984.tb02868.x     Document Type: Article
Times cited : (105)

References (50)
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  • 15
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  • 24
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    • Multichannel seismic evidence for anomalously thin crust of the Blake Spur Fracture Zone, J. geophys. Res.
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    • The geology of the oceanographer transform: the ridge‐transform intersection
    • (1984) Mar. geophys. Res. , vol.6 , pp. 109-141
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    • Three‐dimensional flow beneath a slow‐spreading ridge axis: a dynamic origin for the deepening of the median valley towards fracture zones, J. geophys. Res.
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    • Parmentier, E.M.1    Forsyth, D.W.2
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    • The crustal rocks
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    • Geologic investigations in the Cayman Trough: evidence for thin crust along the mid‐Cayman Rise
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  • 43
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    • Sutton, G. H., Maynard, G. L., Hussong, D. M.,. Widespread occurrence of a high velocity basal layer in the Pacific crust found with repetitive sources and sonobuoya, The Structure and Physical Properties of the Earth's Crust, Heacock, J. G., Geophys. Monogr. Am. geophys. Un., 14,. Washington DC
    • (1971) , pp. 193-209
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    • Atlantic oceanic crust: seismic structure of a slow spreading ridge
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    • (1984) Ophiolites and Oceanic Lithosphere , pp. 101-111
    • White, R.S.1
  • 50
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    • Three dimensional temperature structure of a ridge‐transform‐ridge system (abstract)
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.